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Climate Change and Outdoor Recreation Resources

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April 2009
Climate Change and
Outdoor Recreation
Daniel Morris and Margaret Walls
© 2009 Resources for the Future. All rights reserved. No portion of this paper may be reproduced without
permission of the authors.
Backgrounders are research materials circulated by their authors for purposes of information and discussion. They
have not necessarily undergone formal peer review.
I. Introduction ......................................................................................................................... 1
II. Freshwater Resources and Recreation ............................................................................ 2
Impacts on Snowpack ......................................................................................................... 2
Impacts on Streams and Reservoirs .................................................................................... 5
Impacts on Noncoastal Wetlands ........................................................................................ 6
III. Coastal Areas and Recreation ......................................................................................... 7
IV. Public Lands ................................................................................................................... 11
Impacts on National Forests .............................................................................................. 11
Impacts on National Parks ................................................................................................ 15
Impacts on National Wildlife Refuges .............................................................................. 17
V. Estimates of Recreational Benefits and Costs from Climate Change ........................ 17
VI. Conclusion ...................................................................................................................... 19
References .............................................................................................................................. 22
Resources for the Future Morris and Walls
Climate Change and Outdoor Recreation Resources
Daniel Morris and Margaret Walls
I. Introduction
It is now widely recognized that climate change is taking place, and in the absence of
serious policy to reduce greenhouse gas emissions—and in fact, even with it—the planet will
continue to grow warmer over the next century. In North America, mean temperatures are
expected to increase between 1°C and 3°C by 2039, according to the Fourth Assessment Report
of the Intergovernmental Panel on Climate Change (IPCC 2007). Beyond 2039, 2 to 3°C of
warming will likely occur on the continental edges, with more than 5°C of warming possible in
higher latitudes. Precipitation is predicted to increase across the continent with the exception of
the southwestern United States, which will experience decreased mean annual rainfall.
In this backgrounder, we look at the impacts these changes are likely to have on
recreation resources in the United States. We focus our attention on freshwater resources, coastal
areas, and public lands. Specifically, we assess the likely changes in snowmelt and the resulting
impact on winter recreation activities; the impacts on streams and reservoirs and how they may
affect recreational fishing and boating; and the impacts on noncoastal wetlands, which may
impact hunting and wildlife viewing opportunities. Rising sea levels will accompany climate
change, and we assess how this change will impact coastal recreation in various areas of the
United States. Finally, we look at impacts on forests, large wildlife, national parks, and national
wildlife refuges, and assess their likely influence on recreation opportunities and outcomes.
Wherever possible, the discussion highlights policies that can help recreation adapt to new
climate realities.
Many studies have been published, and many more are underway, of the impacts of
climate change on a variety of ecosystems and species. We are not comprehensive in covering
that literature in this backgrounder. Instead, we provide a selective overview of the most
significant findings for resources that are important for outdoor recreation. The penultimate
section of the paper includes a review of the limited number of economics studies on the
The authors are research assistant and senior fellow, respectively, at Resources for the Future. We appreciate the
helpful comments of Steve Williams of the Wildlife Management Institute.
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recreational benefits and costs of climate change. In the conclusion, we discuss the role played
by adaptation.
II. Freshwater Resources and Recreation
Because water often dictates the functionality of natural systems, it is one of the key
considerations in assessing the impacts of climate change and is pervasive in discussions about
the role played by adaptation. Water is critical for many recreation activities, from boating and
fishing to mountain biking and backpacking. Impacts on water resources from climate change
will vary by region of the country and by season. In this paper, we limit our discussion to
impacts on winter recreation from reduced snowpacks, impacts on fishing and boating from
lower streamflows and reservoir levels, and changes in hunting and wildlife viewing
opportunities from alterations in noncoastal wetlands.
Impacts on Snowpack
Climate models overwhelmingly predict that snowpack levels will decrease in the future
as a result of climate change. The snowpack in most locations is expected to accumulate later in
the winter months and melt away much more quickly in the spring. Increased precipitation is
expected in many regions under climate change, but will present few benefits to snowpacks
because higher temperatures during the events will cause much of it to fall as rain (Knowles et al.
2006). As a result, the number of areas where snow reliably falls is expected to shrink as the
climate warms. The Sierra Nevada Range in California may experience a 99 percent loss of its
April 1 baseline snowpack, and other western mountain ranges will suffer reduced late-season
snowpacks by the end of the century (USGCRP 2000). Ski areas with comparatively warmer
mean microclimates, such as those found in New Mexico, Arizona, Nevada, and California, will
experience more snowpack loss than areas that remain colder, such as those found in Colorado,
Montana, Utah, and Wyoming. A study of the impact on Washington state ski resorts found that
12.5 percent of the areas in the Cascade Mountains and 61 percent of the areas in the Olympics
are “at risk” from future climate change (Nolin and Daly 2006). The authors defined areas as “at
risk” if their snow currently accumulates at temperatures at or near freezing. Figure 1 shows a
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graph of estimated snowpack declines in the western United States under a likely future climate
change scenario.
Skiers and snowboarders tend to favor lower temperatures and more snow, and low-
quality snow can affect the demand for ski days (Englin and Moeltner 2004). Once again,
warmer ski areas in the Southwest are more at risk for significant reductions in snow quality than
colder areas in the central Rocky Mountains and are thus more likely to see reduced demand
(Butsic et al. 2008). Estimates for ski season day losses range from 7 percent with major
adaptation efforts to 100 percent with no adaptation efforts (Scott et al. 2003). The adaptation
options that are currently available are limited in scope and often constrained by financial
resources. The most obvious option is snowmaking, which many ski areas already use to some
degree. With warmer temperatures, advanced snow-making technology will be needed. A study
that simulated ski season operations under shifting climatic conditions in southern Ontario found
that the season will be reduced by 11 percent to 50 percent by 2080 with current snowmaking
capacity, but improved snowmaking technology leads to a reduction of the season by 4 percent to
39 percent (Scott et al. 2003). Other adaptation options include landscaping slopes to reduce the
need for deep snowpacks and moving ski operations to higher, more north-facing peaks to
maximize snowpack accumulation (OECD 2007). The extent to which such changes are feasible
or financially viable will vary by region.
In Europe, only 30 percent of ski resorts that currently receive reliable to marginal snow will continue to receive
snow with 4°C of warming (OECD 2007).
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Figure 1. Estimated Percentage Changes in Snowpack in the Western United States:
Results from Two General Circulation Models
Source: United States Global Change Research Program. 2000. Climate Change Impacts on the United States: The
Potential Consequences of Climate Variability and Change. Overview: Water.
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Impacts on Streams and Reservoirs
Seasonal changes in precipitation will not only affect winter recreation, but could have a
major influence on the quality and availability of activities that depend on reservoirs and
streams. More rain during the winter months is expected to combine with smaller snowpacks that
melt sooner to generate peak streamflows earlier in the spring and reduced summer streamflows
(USGCRP 2000). Moreover, reduced snowpack contributions to streams combined with warmer
air temperatures will likely result in warmer water temperatures. Both sportfishing and boating
will be affected by these changes, but in different ways. Sportfishing is dependent on water
quality, including water temperature, streamflow levels, and ecological conditions, whereas
recreational boating is more sensitive to lake, reservoir, and stream levels.
Water quality and temperature are major influences on the distribution of aquatic
species, and warmer streams are expected to reduce the current habitat of rainbow trout and other
coldwater fisheries that are valued by anglers. Pendleton and Mendelsohn (1998) combine
general circulation models, ecological models, and economic models to estimate the effects of a
doubling of atmospheric CO
on sportfishing in the northeastern United States. Their model
estimates that, on net, the annual economic benefits from climate change range from –$4.6
million to $20.4 million, depending on negative trends in rainbow trout populations and positive
trends in brook trout populations. In other words, there could be an economic cost related to
recreational fishing due to rainbow trout population declines resulting from increased water
temperatures. Conversely, rising water temperatures could make North Carolina streams more
hospitable for other trout species, like brook trout, leading to population increases and potential
benefits of up to $20 million per year. Other studies show brook trout have variable reactions to
global warming. Some scenarios predict that a 3.8°C overall increase in mean annual
temperatures could result in an 89 percent loss of brook trout from streams in Virginia and an 82
percent loss in North Carolina, whereas others project that the maximum loss of brook trout
habitat does not top 30 percent (Ahn et al. 2000). Drier, warmer summers are resulting in warmer
water and lower streamflow throughout the eastern and western United States (Covich 2009),
which could stress many trout and salmon species.
Fluctuating reservoir and stream levels will influence the quality and availability of
recreational boating in a changing climate, but these effects are likely to vary widely by region of
the country. The West will be hardest hit as mountain snowpacks feed streams throughout the
spring and into the summer, and snowpack levels will be lower. The Colorado River, for
example, gets 70 percent of its water from snowmelt (Christensen et al. 2004). Vanishing
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snowpacks and higher summertime temperatures will decrease streamflows and lower reservoir
levels, which can impede recreational boating and reduce waterfront property values (Covich
2009). Climate model runs with a 2.4°C warming show a 17 percent reduction in runoff in the
Colorado River Basin, which leads to a 40 percent reduction in basin storage (Christensen et al.
2004). Reservoirs in the basin include such popular recreation areas as Lake Powell, Lake Mead,
and Lake Havasu. Reductions in runoff may lead to more demand for water storage as an
adaptation measure, but large dams have major environmental costs and are very expensive.
In addition to impacts on boating and fishing, reductions in stream flows—particularly in
the hot and dry Southwest—could also have negative impacts on hiking, mountain biking, and
backpacking opportunities. Not only is water essential for engaging in these activities in the
outdoors, but it also enhances the appeal of the environment. Water is a draw for outdoor
recreation of all types.
Impacts on Noncoastal Wetlands
Wetlands in the northern plains states and the Canadian provinces of Alberta,
Saskatchewan, Manitoba, and northern British Columbia form the basis of what is known as the
Prairie Pothole Region. This system of wetlands, which covers over 216 million acres of land,
has been called the “duck factory” for its importance in providing breeding areas for a variety of
birds such as pintails, mallards, and blue-winged teal, and critical migratory habitat for lesser
scaup, Canada geese, and snow geese, among others. In most climate change scenarios, many of
the wetlands in the Prairie Pothole region are expected to dry up, and the portion of the region
that has optimum conditions for breeding is predicted to shift south and east (Johnson et al.
2005). Figure 2 shows a map of the region as it now exists, along with three alternatives for the
location of these key wetlands in a world of climate change. In some scenarios, 90 percent of the
region’s wetlands are predicted to disappear, which could lead to a 69 percent reduction in the
area’s breeding duck populations.
The Prairie Pothole Region is not the only waterfowl habitat under threat; lowering water
levels in the Upper Great Lakes area could lead to a 39 percent loss in regional duck populations
(Yaich and Wentz 2007). In addition to habitat loss, migrating game birds will face shifting
seasonal pressures that will alter migration patterns, including departure times and winter
locations. As the country warms, migrating flocks will not have to travel as far south to find open
water and suitable food sources, meaning once-productive hunting areas in the southern United
States could become bereft of game fowl. Moreover, warmer fall and winter temperatures will
muddle seasonal signals that initiate flock migration, leading to more erratic behavior among
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migrating species. Hunters and birdwatchers who plan their activities around the migration of
birds at certain times of the year will potentially have fewer and less reliable recreation
While climate change may have negative effects on water supplies, ranging from
reduced streamflows, warmer water temperatures, lower reservoir levels, and shifting patterns of
noncoastal wetlands, the demand for recreational boating, fishing, and swimming is expected to
soar in a warmer climate. A longer summer season and higher temperatures during the season
will increase demand for water-based outdoor activities. In addition, warmer temperatures affect
the demand for other recreational activities such as hunting and wildlife viewing. We discuss this
issue and the related calculations of recreational values in Section V below.
III. Coastal Areas and Recreation
Sea level rise is one of the most serious outcomes expected from climate change. The
IPCC estimates that for global temperature increases between 1.1°C and 6.4°C, which is the
range predicted by climate models under various conditions, global average sea levels should rise
between 0.18 and 0.59 meters over the next century. This forecast excludes any impact from
disintegration of the Greenland and Antarctica ice sheets, which could exacerbate the problem.
In the United States, sea levels could rise anywhere between 0.13 and 0.95 meters,
though 0.48 meters appears to be the best estimate for the average rise across all areas (USGCRP
2000). Impacts vary widely across the United States, however. Coastal areas with shallow slopes,
high tidal ranges, and high wave height are more vulnerable to widespread inundation (U.S.
Geological Survey 2002). In some regions—Louisiana, the Midatlantic, and the South Atlantic,
for example—land subsidence contributes to the net rise; in these areas, fairly significant
increases have already occurred. Current sea level rise in the midatlantic region is estimated to be
3mm to 4 mm per year, which is nearly two times the global average, and many scenarios see
this rate as increasing (U.S. CCSP 2009). Figure 3 shows the estimated land area in different
regions of the country that would be under water with a sea level rise of 20 inches (0.51 meters).
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Figure 2. Prairie Pothole Region and Coverage of Optimum Wetland Conditions under
Alternative Climate Scenarios
Source: Johnson et al. 2005.
Note: The figure shows historic conditions (a) and modeled future conditions (b, c, and d). The outlined area in each
map is the Prairie Pothole Region; the red area is the area with optimum wetland conditions for waterfowl breeding.
Several concerns arise in the south and midatlantic regions because of sea level increases.
Serious impacts on tidal wetlands, for example, are virtually certain. Moreover, many of these
wetlands have nowhere to migrate or reform because of extensive land development and
inadequate areas of dry land (U.S. CCSP 2009). Because much of the land is close to sea level, in
some scenarios spring high tides are expected to lead to large areas of land under water. Most of
the mid and south Atlantic states are bordered by barrier islands, which are expected to be
seriously impacted from climate change. There is a great deal of uncertainty in the predictions,
but in some scenarios, these islands are predicted to completely disappear. Studies of impacts
along the Pacific coast also suggest some areas of serious concern. In the Puget Sound region of
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Washington state, which includes the cities of Seattle and Tacoma, an area of about 56 square
miles could be under water within 50 years as a result of a 2-inch sea level rise, which is the
upper bound of projections (Bauman et al. 2006); this area would affect over 44,000 people.
Figure 3. Coastal Lands of the United States at Risk from a 20-Inch Sea Level Rise
Source: United States Global Change Research Program. 2000. Climate Change Impacts on the United States: The
Potential Consequences of Climate Variability and Change. Overview: Coastal Areas and Marine Resources.
Note: Graph shows square miles of both dry lands and wetlands expected to be under water in a 20-inch sea level–
rise scenario.
It is well-established that coastal recreation and tourism are immensely valuable. Studies
have shown that beaches are the leading tourist destination in the United States, followed by
national parks and historic sites (Houston 1996). A full 85 percent of tourism-related revenues in
the United States are generated by coastal states. And within those states, tourism and recreation
contribute significantly to the economy. Dwight et al. (2007) estimate that tourism and recreation
generate 59 percent of California’s ocean-related economy, which is the largest in the nation. In
addition, many of these states have coastal areas with unique ecological resources. There are ten
national seashores: seven along the Atlantic coast, from Cape Cod National Seashore in
Massachusetts south to Cape Canaveral in Florida; two in the Gulf of Mexico; and one in
California. In 2008, these sites had nearly 16 million visitors, accounting for 6 percent of visitors
to all National Park System sites while making up only 2 percent of the 391 units in the system
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(National Park Service 2009; National Park Conservation Association 2009). Gulf Islands
National Seashore in Mississippi and Florida has large areas of land that are extremely
vulnerable to climate change because the park is almost entirely a low-lying barrier island (U.S.
Geological Survey 2002).
In addition to the national seashores, there are several national wildlife refuges in coastal
areas that have high recreational values. Chincoteague National Wildlife Refuge in Virginia is
one of the most popular units with more than 1.5 million visitors per year. The refuge lies
entirely on Assateague Island, a 37-mile barrier island that runs along the coasts of Maryland and
Virginia. Scientists expect the island to migrate landward over time. Although many species of
birds and other animals that live in the refuge may continue to have habitat, albeit in a new
location, popular recreational sites such as the Wildlife Loop Road that circles Snow Goose
Pond, a major feeding and nesting spot for snow geese, will likely disappear (U.S. EPA 2009). In
a recreation demand model by Loomis and Crespi (1999) that we describe more fully in Section
V below, the authors estimate a net welfare loss from more limited bird viewing and waterfowl
hunting nationally as a result of a loss in coastal wetland acreage.
Given the popularity of coastal beaches, the importance of beach recreation and tourism
to local economies, and the highly developed nature of many coastal communities, it is likely
that inundation of some beaches will be replaced by comparable beaches in a slightly altered
location. Many beaches will simply move inland (Yohe et al. 1999). Moreover, the coastline can
be reinforced by beach nourishment, which consists of depositing sediment on beaches to replace
what is naturally eroded. Beach nourishment can protect shores from erosion and inundation as
well as maintain important recreation value (Hamilton 2007). This kind of adaptation activity is
likely to occur in many locations. And even though nourishment cannot protect all beaches,
people will not lose their desire to visit the coast. Loomis and Crespi (1999) found that, even
with a 15 percent net loss of beaches, user days will increase by 29.71 million by 2060 with
climate change, resulting in an additional $370 million in economic gains.
Unfortunately, although there are numerous studies of the impacts of sea level rise on
coastal lands, there have been few systematic attempts such as the Loomis and Crespi (1999)
study to link these changes to impacts on coastal recreation and recreational benefits. Wall
(1998) suggested that sea level rise could become a major cause for marine wetland loss,
especially if human structures like levees and seawalls impede the intrusion of sea water inland.
Hunting and fishing activities rely on the diversity that thrives within marine wetlands, and those
activities could be severely impacted if wetlands are converted into open water by rising seas.
Migrating waterfowl that rely on coastal wetlands and the hunters who pursue them on both sides
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of the country will suffer as well. The rising Atlantic may destroy up to 45 percent of coastal
wetland habitat for important game birds like canvasbacks, pintails, and redheads; the
encroaching Pacific will swallow habitat for migrating ducks and geese along the length of the
Pacific flyway that stretches from Alaska to California. Some estimates predict Louisiana’s
Chenier Plain marshes, which currently support over 1.3 million waterfowl, will be so inundated
that they will eventually only support 1 percent of current populations (Yaich and Wentz 2007).
The loss of beaches in some locations can be serious. Whitehead et al. (2008) investigate
the economic effects of sea level rise on recreational coastal fishing in North Carolina. Barrier
islands lie along the entire North Carolina coast. These authors find that narrower beaches are
less attractive to anglers because they are more difficult to access and make transporting
equipment more difficult. The study combines projected beach widths resulting from anticipated
erosion in 2030 and 2080 with revealed willingness-to-pay preferences based on spatial
differences observed on popular angling beaches. The study projects substantial aggregate
welfare losses from 2006 to 2080 due to reduced fishing access and quality, possibly as high as
$1.29 billion in net present value terms. In a related study, Bin et al. (2007) estimate that 34
percent of the recreational value of trips to North Carolina beaches will be lost by 2080 as a
result of reduced beach width and complete loss of some beaches. Moreover, the authors
emphasize that this is likely to be an underestimate because it fails to account for increased
congestion on remaining beach acreage.
IV. Public Lands
Impacts on National Forests
The national forests cover 188 million acres of land in the United States and provide the
settings for much of the nature-based recreation that takes place in the country. Several types of
damage are expected to be inflicted on forests as a result of climate change and in some cases,
some of that damage may already be manifesting. These damages are not the result of new
disturbance regimes in forest ecosystems but rather an exacerbation of current disturbances (Dale
et al. 2001). Drought, wildfire, insect infestation, and extreme weather are all significant impacts
that will grow more intense in a changing climate.
Drought is not as visually obvious as other disturbances, but it is perhaps the most
devastating because it can significantly weaken a forest’s defenses against fire and insect
invasion. Almost all forest ecosystems evolved with drought as a regular stressor; forests
throughout the intermountain West and Southwest experience seasonal summer droughts along
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with droughts that can sometimes last for years, while more humid forests in the northwestern
and eastern United States experience infrequent droughts (Dale et al. 2001). Climate models
suggest that the combination of higher overall temperatures and less frequent, more intense
rainstorms over long time periods will not only aggravate droughts in the forests of the interior
West, but is also likely to generate more frequent droughts in the forests of the Northwest and
East. Warmer summers will reduce both the amount of water available in soil and aquifers and
affect overall net primary productivity. Additionally, intensifying rainstorms that occur more
often in winter may impede ecosystems from storing water reserves that are critical to get
through hot summers. This will lead to higher mortality rates in young trees, which in turn leads
to more fuel generation for wildfires. In addition, all trees are likely to be weakened against
insect invasion and disease infection.
Similar to drought, insects are a natural and integral part of forest ecosystems. Bark
beetles are one of the most important mortality agents in western and southern forests (Dale et al.
2001; Fettig et al. 2007). The populations of the beetles, which are no bigger than a grain of rice,
are heavily affected by seasonal temperatures. Cold, harsh winters can knock back beetle
populations considerably, whereas warmer winter temperatures ensure that more beetle larvae
survive to become full-grown. Winter temperatures tempered by climate change can potentially
enhance bark beetle larvae’s chances of surviving and generate huge populations that can
overwhelm a forest. Concurrently, climate change–induced drought can deprive individual trees
of the ability to effectively defend themselves against the beetles, possibly leading to massive
infestation and tree mortality.
Some of these problems are already manifesting throughout the country, as states all over
the West, South, and as far north as Alaska have seen unprecedented levels of tree mortality
(Fettig et al. 2007). The telltale sign of infestation, forests smeared with wide strokes of red-
needled evergreens, can be seen throughout the country. Beetles killed 2.5 million acres of trees
in Colorado and Wyoming in 2006 and 2007, and they were expected to finish off another 2
million acres by the end of 2008 (Robbins 2008). Figure 4a shows a map of the extent of
infestations by three beetle species across western North America. Figure 4b shows the change in
the size of the area affected between 1980 and 2005.
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Figure 4. Area of Forests Damaged by Bark Beetle Infestations
Source: Raffa et al. 2008. Data are from the Canadian Forest Service, the British Columbia Ministry of Forests and
Range, and the U.S. Forest Service.
Deceased trees can pose a serious threat to the safety of recreationists. As a result of
massive tree dieoffs, officials in Colorado and Wyoming closed 38 campgrounds in the summer
of 2008 (Robbins 2008). The threat of falling trees is not limited to campgrounds; roads, trails,
picnic and other areas are all locations where forest users are vulnerable to deadfall. Most dead
trees will not injure people directly, but both standing and fallen trees present a different threat
because they are large fuel stocks for forest fires.
As drought and bark beetles work in concert to weaken forests and kill trees, they set the
stage for wildfire to scour the landscape. Although fire is an integral part of many forest
ecosystems, especially in the western United States, where it is too dry to encourage
decomposition of deadfall, government policies during the twentieth century to suppress all fires
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have led to a dangerous overload of fuel. Combined with dry conditions brought on by climate
change, this creates a volatile situation that has major implications for forest recreation. In 2007,
9.9 million acres of forest burned across the country, and the federal government is anticipating
having to deal with similarly destructive fire seasons over the next five years. Recognizing this
threat, the Obama Administration allotted $1.1 billion to the U.S. Forest Service to combat fires
in 2010, with an additional $282 million available in safety valve funds (Leber 2009).
Recreation is vulnerable to disruption from wildfire because people often recreate in
environments and seasons with high fire risks, although there is no clear link between
recreational user mortality and wildfire (Morehouse 2001). The effects of fires on recreation can
vary; prescribed fires that are closely monitored may not impede recreation activities, whereas
catastrophic stand-altering fires can close off popular areas for months or even years.
Additionally, even if burned areas are not closed to recreation, fire can degrade them to a point
where they are less attractive for users. A survey of outdoor recreationists found that 75 percent
said scenery quality was very or extremely important and between 73 and 85 percent of users
value safety while recreating (Morehouse 2001). The combination of inaccessibility due to forest
closures and the degradation of viewsheds and resources may drive visitors away. Fewer visitors
can, in turn, have a negative impact on local economies for which recreation is a valuable input.
Starbuck et al. (2006) use a combined travel cost/contingent valuation model to estimate the
consequences of catastrophic fires on recreation days and the concomitant economic effects.
Extrapolating from data gathered by mail surveys and on-site surveys in five national forests
throughout New Mexico, the model suggests a massive destructive fire would reduce forest visits
the following year in New Mexico by 7 percent, resulting in an $81 million loss in economic
output and more than 1,900 lost jobs. After the severe fires in Yellowstone National Park in
1988, visits to the park dropped 15 percent in one year (National Park Service 2009). However,
by the next year, visits had returned to almost the same level as the year prior to the fire.
Along with these easily identifiable disturbances, climate change may manifest in more
subtle and significant ways. A recent study by Van Mantgem et al. (2009) finds that background
(i.e., not attributable to a distinct disturbance) tree mortality rates in old-growth forests across the
western United States have doubled over the past few decades, and recruitment of new saplings
is not correspondingly increasing. After eliminating factors such as insect invasion, diseases, and
endogenous changes in forest structure as reasons for mortality increase, the study suggests that
regional warming is the culprit, as it is occurring consistently through different forest types from
Washington to Colorado to Arizona. While these mortality rate increases will not directly result
in large swaths of dead trees, the study points out that increasing mortality rates may be
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indicative of vulnerability to significant dieback events and can presage major alterations in
forest function, structure, and composition. These systematic stresses may eventually collude
with some of the large disturbances we described above to push forest ecosystems past their
tipping point, creating a scenario from which they cannot recover.
As these multiple disturbances manifest throughout public lands over time, animal
species that depend on the ecosystems found on those lands, especially big game animals like
deer, elk, and moose, will have to adjust to or migrate away from harsher conditions. Otherwise,
their populations will suffer significantly. Drought and wildfires represent obvious threats to big
game species’ habitats, and extreme events will force populations to migrate to more suitable
areas. More subtle effects of climate change will contribute to the movement of large animals as
well. For instance, milder winter temperatures may reduce moose populations, which are keenly
adapted to harsh, cold conditions, but could boost populations of animals that struggle in such
conditions, such as white-tailed deer and elk. Moose may be so stressed by milder winters that
they disappear completely from the upper Midwest (Wildlife Management Institute 2008).
Similarly, as alpine ecosystems retreat further up mountainsides in reaction to warmer
temperatures, they will continue to isolate populations of bighorn sheep and mountain goats. In
contrast, as increasing temperatures increase the survival odds of deer and elk, they will also
likely assist the survival of parasites and pests, which in turn may negatively affect herd
populations. As populations begin to expand, they will need more food sources, yet climate
change will present them with another challenge. Plants will absorb increasing amounts of CO
which will decrease the nutritional value of the leaves mule deer are particularly dependent on,
possibly leading to malnutrition. Elk are better evolved to survive on marginally nutritious plants
(Wildlife Management Institute 2008). Overall, hunters and wildlife watchers could have a more
difficult time finding healthy big game animals, especially in areas with marginal habitat
conditions. In a climate-altered world, areas with more robust ecosystems, such as those
protected by national parks, will become critical support areas for charismatic megafauna.
Impacts on National Parks
Some of the forest problems that we describe may occur in national parks, which could
have a serious impact on recreation given the high recreational value of these distinctive areas. In
addition, other problems have been identified that are unique to some individual parks. To
illustrate these impacts, it is useful to look at two very different parks: Glacier National Park,
situated next to the Canadian border in the Rocky Mountains of Montana, and Joshua Tree
National Park in the rugged Mojave Desert of southeastern California. These two parks could not
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have more different climates or ecosystems, but both may see their namesake resources
disappear from within their borders by the end of the century.
In a study now over 25 years old, Carrara and McGimsey (1981) found that more than
two-thirds of the 150 glaciers that had existed in the Glacier National Park area in 1857 had
already disappeared completely by 1980, and the remaining glaciers had shrunk in size. Hall and
Fagre (2003) estimate that under likely future climate scenarios, the glaciers remaining in the
park will all vanish by 2030. Such a dramatic change has many repercussions for the park’s
ecosystems. As the glaciers melt, streams will initially have greater summer flows but are likely
to transport more sediment, which has implications for aquatic life; eventually, as the glaciers
disappear, stream flow will decline. The distribution of plants and trees will change, as some
species will grow on land formerly covered by ice. From a recreation perspective, the glaciers
are, not surprisingly, a strong draw for visitation to the park—the park drew over 2 million
visitors in 2007. How that will change as the glaciers disappear is unclear.
Like Glacier, Joshua Tree National Park also faces threats from increasing temperatures.
The trees that are the park’s namesake covered a wide range of land during the last Ice Age,
when seeds were transported long distances by a now extinct animal, the Shasta ground sloth.
The extent of land covered by the tree is now much more limited, and without the sloth to carry
its seeds, the tree is expected to be unable to migrate in response to rising temperatures. Studies
have posited that the southern half of the tree’s range, which includes the national park, will
grow too warm to sustain them and that Joshua trees will vanish from Joshua Tree National Park
within the next 100 years (Shogren 2008). The tree, which has been described as the “canteen of
the desert” provides sustenance to many animal species, including the antelope ground squirrel
and the blacktail jack rabbit. It is unclear whether these species can migrate and survive without
the trees. How recreational values will be affected by loss of the trees is unclear, but is likely to
be negative. With warmer temperatures in a desert environment and with loss of the unique asset
of the park, some park rangers have speculated that there will be nothing there to attract visitors
(Shogren 2008).
The ranger’s comment may be overly pessimistic. The park attracts visitors for horseback riding, mountain biking,
off-road vehicles, and viewing other natural attractions besides the trees. Moreover, it is one of the most popular
rock climbing areas in the United States.
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Impacts on National Wildlife Refuges
There are 550 refuges in the National Wildlife Refuge System covering 97 million acres
of land. Scott et al. (2008) cite research findings in a recent doctoral dissertation showing 309 of
these refuges will lose waterfowl species as a result of range contraction due to climate change.
Concerns over an inadequate land base and worries about development and other activities on
contiguous properties have always been a concern of the National Wildlife Refuge System. With
climate change altering the land in many refuges or leading to the disappearance of land in
others, there is added concern about these issues. Scott et al. (2008) conclude that the most
vulnerable refuges are the 162 coastal refuges, along with those refuges in Alaska. We discussed
some of the impacts on key coastal areas above—Chincoteague National Wildlife Refuge, for
example, is expected to shift and move westward over time. Blackwater National Wildlife
Refuge, on the Chesapeake Bay in Maryland, is expected to be one of the most severely affected
refuges. The wetlands there, which are home to the largest concentration of nesting bald eagles
on the east coast north of Florida, are expected to completely disappear within 30 years (U.S.
EPA 2009). The J.N. Ding Darling National Wildlife Refuge on Sanibel Island near Ft. Myers,
Florida, is also expected to face serious impacts, losing 67 percent of its dry land, 99 percent of
its tidal flats, and 58 percent of its hardwood swamp (U.S. CCSP 2008). The refuge is a highly
popular tourist and recreation destination, with over 850,000 visitors per year (Wyman and Stein
Although the primary mission of the National Wildlife Refuge System is protection and
management of native fish and wildlife and their habitats, many of the refuges, such as the Ding
Darling Refuge, are highly desirable recreation destinations. In 2006, 35 million people visited
the refuges, generating an estimated $1.7 billion in total economic activity (Carver and Caudill
2007). Fully 82 percent of expenditures related to these visits were for “nonconsumptive” uses,
such as hiking, biking, and mostly, wildlife viewing; fishing accounted for 12 percent and
hunting, 8 percent. Wildlife viewing is one of the key recreational activities that takes place on
national wildlife refuge lands, and this activity has grown in popularity in recent years (Cordell
et al. 2008). How these values would be affected by climate change is uncertain. Much is likely
to depend on the adaptation measures taken by refuge managers and policymakers.
V. Estimates of Recreational Benefits and Costs from Climate Change
The studies we cite above present a sampling of the many research efforts that are
underway to model and predict the impact that climate change will have on natural resources and
ecosystems across the United States. We have tried to draw out the particular influence these
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changes are likely to have on recreational resources. In this section, we discuss some of the
economics studies that take the next step and estimate the full social benefits and costs from
changing recreation as a result of climate change. We discussed a few of these studies above—
Pendleton and Mendelsohn (1998), Whitehead et al. (2008), Bin et al. (2007), and Loomis and
Crespi (1999)—which we describe more fully below.
Using statewide aggregate demand models, Mendelsohn and Markowski (1999) extend
previous studies (Cline 1992) that focused solely on skiing to predict climate effects on
economic benefits from seven recreation activities: boating, camping, fishing, golfing, hunting,
skiing, and wildlife viewing. They use cross-sectional data for the lower 48 states (from 1991)
and estimate the aggregate number of days spent in these various activities as a function of
population, income, prices, and various temperature and precipitation variables. The authors use
their results to calculate welfare effects in 2060 from changes in temperature ranging from 1.5°C
to 5°C and increases in precipitation of 7 and 15 percent; they also look at welfare effects by
using region-specific changes in temperature and precipitation. They look only at the direct
effects on demand and do not incorporate any indirect effects due to changes in resource
availability or site characteristics.
The authors find that these climate change scenarios will result in major losses for snow
skiing, camping, and wildlife viewing, but that those losses will be swamped by substantial gains
for fishing and boating. Overall, there are welfare gains in the recreation sector from climate
change; for the central case of a 2.5°C temperature rise and 7 percent increase in precipitation,
the benefit ranges from $2.8 to $4 billion (in 2060) depending on the model used.
Loomis and Crespi (1999) use a similar approach. They estimate recreation demand
models by using aggregate visitation and other data, but they also, for some categories of
activities, use demand elasticities estimated from other studies. They include a wider set of
activities, 17 in all, and unlike Mendelsohn and Markowski (1999), Loomis and Crespi do
incorporate some changes in site characteristics due to climate change when predicting changes
in recreation in the future. For example, in their model of reservoir recreation, they include both
the direct positive effect of higher temperatures on the number of recreation visits and the
indirect negative effect on surface area of the reservoir (as higher temperatures reduce water
levels). They incorporate similar effects in their snow skiing model, including the reduced length
of the ski season as a result of climate change, and in their model of waterfowl hunting, with
reduced wetlands acreage. Even with these differences from the Mendelsohn and Markowski
approach, Loomis and Crespi find positive net recreational benefits overall from climate change,
and they are on the same order of magnitude as the Mendelsohn and Markowski results.
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Richardson and Loomis (2004) conduct a contingent valuation survey to estimate how
changes in climate factors will affect visitation in Rocky Mountain National Park in Colorado.
Using models to construct different scenarios of climate change effects on the park, the study
surveyed park visitors to gauge how they think changes in the park would affect their
recreational behavior. The results of the surveys indicate that climate change could positively
affect visitation rates and that temperature is a significant factor in determining visitation
behavior, implying that warmer temperatures could encourage more people to visit Rocky
Mountain National Park. The authors of the study suggest these findings may be applicable to
other high-altitude alpine parks. These results, though based on a different methodology, support
the findings in Loomis and Crespi (1999) and Mendelsohn and Markowski (1999).
All three of these studies highlight the importance of weather and climate in determining
the demand for outdoor recreation, and all forecast that demand will increase in a world with
climate change. Although the incorporation of changes in resource supply and recreation site
characteristics is rudimentary in the Loomis and Crespi (1999) study and nonexistent in the
Mendelsohn and Markowski (1999) and Richardson and Loomis (2004) studies, these findings
about the effect that a warmer climate might have on recreation demand are instructive. Warmer
temperatures, earlier springs, and longer-lasting summers are expected to increase the demand
for many kinds of outdoor recreation activities, making it all the more important for
policymakers to develop adequate adaptation policies directed at recreational resources.
In addition to these studies that predict overall increases in demand, other studies have
emphasized the effect on recreation in colder areas. Assuming recreation will increase with
economic growth, simulation models of international tourism demand show that climate change
is likely to shift tourism patterns toward higher latitudes and altitudes (Hamilton et al. 2005).
Domestic tourism will also move toward cold regions, resulting in a doubling of tourism for
colder countries and a 20 percent reduction of tourism in warmer countries (Bigano et al. 2005).
As tourism and recreation are closely related, these findings are presumably representative of
recreation patterns, meaning that more recreation is likely to shift to higher latitudes and
VI. Conclusion
Over the next century, climate change will be one of the most important and pervasive
influences on natural systems. Even if all emissions of CO
ended today, the atmosphere is still
guaranteed another 30 to 40 years of warming. Recent studies have also found global warming is
essentially irreversible over 1,000 years even after a complete halt to emissions (Solomon et al.
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2009). Regardless of mitigation efforts, the planet’s environment and inhabitants will have to
adapt to a new climate reality. Some plants and animals will naturally adjust to warmer
temperatures or less water availability, through processes known as autonomous or reactive
adaptation, but their natural adaptability will only go so far. In the best cases, plants and animals
will continue to survive under more adverse conditions. Many species will struggle more than
others and may have to migrate (or be transported) to new habitats as ecosystems shift and
natural cycles adjust to new climate realities. In the worst cases, some species will go extinct and
some of the country’s most treasured places will be altered for generations.
Anticipatory or planned adaptation, unlike autonomous adaptation, does not wait for
conditions to shift. Instead, natural resource managers can look ahead, anticipate some of the
negative consequences of climate change, and adjust management schemes in a way that gives
resources a better opportunity to weather those consequences. In one sense, climate change does
not present many new problems, just stronger versions of familiar problems. People and
ecosystems have always had to deal with droughts, wildfires, floods, and insect invasions.
Unfortunately, however, that does not mean people know how to deal well with those problems.
Fire suppression policies over the past 100 years led to the accumulation of huge fuel stockpiles
that have increased the ferocity of wildfires throughout the nation’s forests. Water policies,
especially in the western United States, have reduced once-mighty rivers to trickles and driven a
number of species to the brink of extinction. Levees that snake along the banks of powerful
rivers to protect against seasonal floods may not be able to withstand the onslaught of
increasingly stronger spring floods. If climate change is the ultimate challenge of the twenty-first
century, adapting to it will require serious overhauls of twentieth century policy.
Congress has not entirely ignored the issue of adaptation. In the 110th Congress, there
were 75 different bills that tried to address climate change adaption in some way. The
Lieberman–Warner Climate Security Act of 2008 (S. 3036) required the government to develop
a national adaptation strategy and contained a provision that could have funneled up to $5 billion
a year in the next decade toward adaptation projects. Similarly, the Climate Change Adaptation
Act (S. 2355), sponsored by Senator Maria Cantwell, would require the government to develop a
five-year strategic adaptation plan that would be updated continuously every five years. The first
major climate bill of the 111
Congress, the Waxman–Markey American Clean Energy and
Security Act, takes a comparable approach by requiring all federal agencies to design specific
adaptation plans and establishing a natural resource adaptation fund to support adaptation actions
taken by natural resource management agencies like the Department of Interior, the National
Oceanic and Atmospheric Administration, and the USDA Forest Service. While these bills show
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that there is some recognition by policymakers that adaptation must be addressed, the nation is
still far away from a comprehensive and effective policy to adapting to climate change.
A national adaptation policy is only a part of the adaptation puzzle. The federal
government must supply needed resources to maintain adaptation programs, whether that be
more money to fight wildfires or to build and maintain sea walls, but it alone cannot sculpt a
policy that is both comprehensive and flexible enough to address the myriad effects of climate
change. As we have highlighted, climate change impacts are heterogeneous across geography
and resource area. States and municipalities may require more autonomy to effectively and
responsibly adapt to different problems, and they will have to develop their own specific
adaptation plans. Adaptation policy that reforms existing institutions while allowing them to
prepare to manage extremes will be our best chance to properly adjust to the changing climate.
Climate impacts on natural resources are pervasive. In this Backgrounder, we have
highlighted the particular impacts on recreation resources. We have also shown that some
economics literature indicates that the value of these resources for recreation purposes may be
higher than ever. Recreation demand is highly dependent on climate, and several studies show
that longer and warmer summers are expected to increase the demand for outdoor recreation,
from hiking, fishing, and camping to simple beach visits. This makes it all the more important
that government policy at all levels—federal, state, and local—develop effective climate
adaptation programs and funding.
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... There are many reasons for changing recreation participation and the current exploration of climate has emerged as one of the most important considerations in planning and managing recreation experiences. Climate and tourism research has materialized as researchers discover the more global impact between our voluntary activities and the planet's health (Hamilton and Tol, 2004;Morris and Walls, 2009;Scott, Hall and Gössling, 2012;Bowker et al. 2014;Nicholls and Amelung, 2015). ...
... Several studies of climate change and recreation or tourism have been published recently (de Freitas, 2003;Morris and Walls, 2009;Scott et al., 2004;Martin, 2005;Becken, 2010;Nickerson et al., 2011;Scott, et al., 2012). Climate influences all aspects of tourism and can make it enjoyable or not (Martin 2005). ...
Full-text available
The World Tourism Organization, the United Nations Environment Programme and the World Meteorological Organization have identified one of the consequences of climate change is an interference of normal precipitation. This research investigates the changes in travel patterns by participants and spectators at an annual canoe race as influenced by variable stream flow. Given that stream flow varies seasonally, one might hypothesize that should a permanent reduction of water flow take place in the future, a decline or shift in water-based recreation might be expected. Using data collected over two years at the Annual Westfield River Wildwater Races, interviews were conducted at the staging area as participants waited in the queue. Observers of the race were also interviewed. The two sampling years represent a low flow season and a normal flow season and yield a sample of 142 parties. During the low flow season, one that is projected to become the norm under climate change models, expert paddlers travelled a greater distance characteristic of destination substitutability while spectators decreased travel distance and this suggests a reduction of interest in observing the race.
... Shifts in forest distribution and types, as well as changes in the composition and dynamics of pests and disease, also can affect rural com- munities that are dependent on forestry (Lal, Alavalapati, and Mercer 2011). Tourism can be another important part of rural econo- mies, and climate change impacts on this sec- tor can range from loss of coastal attractions that are affected by sea level rise, to reduced snowpack for winter recreation, to the effects of habitat changes on hunting and fishing activities ( Walls and Morris 2009;Hales et al. 2014). ...
... Spatial models have explored how land taxes and zoning restric- tions affect the efficient allocation of land uses (Rossi-Hansberg 2004), how environ- mental amenities can generate leapfrog de- velopment patterns (Wu 2006), how preferences for open space and open space policies affect spatial outcomes ( Wu and Plantinga 2003;Turner 2005), and more. Newer models in the Tiebout tradition have incorporated endogeneity in locational equi- librium models and analyzed how heteroge- neous households sort on the landscape (Epple and Sieg 1999;Walsh 2007). Once intertemporal issues become important-for example, in analyzing the timing of land con- version decisions-an integrated dynamic- spatial approach is preferred. ...
Research questions in resource economics increasingly have incorporated both the field’s traditional dynamic considerations and the spatial concerns that often are the focus of regional economics. Spatial heterogeneity in costs, benefits, or connectivity often interact with intertemporal change in contexts such as fisheries management, water allocation, invasive species control, and land use change, making spatially- or temporally-uniform polices less likely to be efficient. In this article, we examine how climate change is likely to enhance the need to incorporate spatial-dynamic approaches to address natural resource challenges. We focus our discussion on rural areas, which are typically highly dependent on natural resources and particularly vulnerable to climate change. Following a brief review of existing spatial-dynamic models in natural resource economics and the insights derived from them, we describe how climate change can bring new spatial or temporal aspects to resource management problems, or exacerbate existing resource challenges that are best characterized as spatial-dynamic processes. We conclude with three case studies that highlight how integrating resource and regional economics through spatial-dynamic modeling may improve the analysis of climate change impacts in rural areas, considering the effects on rangeland management, groundwater policy, and land use management in floodplains and coastal areas.
... Recreationists are more likely to seek respite from heat in natural areas as average temperatures rise (Morris and Walls 2009), increasing overall participation, especially in warm seasons, and extending the warm-weather recreation season. ...
... For example, in Canadian National Parks, warming trends were shown to have a positive effect on visitation in the summer as well as the 'shoulder season' spring and fall months (Jones & Scott, 2006). However, warming trends can cause ecological degradation, and intensify outbreaks of the mountain pine beetle (Morris & Walls, 2009), which visitors view as negative and unacceptable (McFarlane & Witson, 2008). Thus, temperature changes may have mixed effects on park tourists in cooler alpine settings. ...
... Thus, understanding more about climate change and recreation would help communities and land managers in formulating mitigation and adaptation strategies. Morris and Walls (2009) assert that managers should maintain future outlooks, especially with natural elements susceptible to climate change. Brice et al. (2017) emphasize that climate change dialogues include recreation, given the relationship among recreation, natural areas, and climate. ...
... Changing climatic conditions will alter the supply of and demand for outdoor recreation opportunities, affecting visitor use patterns and the ability of outdoor recreationists to obtain desired benefits derived from publicly managed lands in the future (Bark et al. 2010;Matzarakis and de Freitas 2001;Morris and Walls 2009). Benefits provided by outdoor recreation opportunities are expected to increase for some recreationists as the climate warms (Loomis and Crespi 2004;Mendelsohn and Markowski 2004), but will probably vary considerably by geographic region and activity. ...
... Lower snow cover will reduce the cost of snow removal from roads, and allow earlier access for snow removal and maintenance in low-mid elevation areas and a longer construction season at higher elevations (e.g., installation of temporary trail bridges). As noted above, less snow may increase access for warmweather recreation, but may reduce opportunities for winter recreation (Joyce et al., 2001;Morris and Walls, 2009). The highest elevations of the Blue Mountains are expected to retain a significant amount of snow, at least for the next few decades, which may focus snow-based activities in fewer areas as snow at lower elevations decreases. ...
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In the semi-arid environment of the Blue Mountains, Oregon (USA), water is a critical resource for both ecosystems and human uses and will be affected by climate change in both the near- and long-term. Warmer temperatures will reduce snowpack and snow-dominated watersheds will transition to mixed rain and snow, while mixed rain and snow dominated watersheds will shift towards rain dominated. This will result in high flows occurring more commonly in late autumn and winter rather than spring, and lower low flows in summer, phenomena that may already be occurring in the Pacific Northwest. Higher peak flows are expected to increase the frequency and magnitude of flooding, which may increase erosion and scouring of the streambed and concurrent risks to roads, culverts, and bridges. Mapping of projected peak flow changes near roads gives an opportunity to mitigate these potential risks. Diminished snowpack and low summer flows are expected to cause a reduction in water supply for aquatic ecosystems, agriculture, municipal consumption, and livestock grazing, although this effect will not be as prominent in areas with substantial amounts of groundwater. Advanced planning could help reduce conflict among water users. Responding pro-actively to climate risks by improving current management practices, like road design and water management as highlighted here, may be among the most efficient and effective methods for adaptation.
... For example, in Canadian National Parks, warming trends were shown to have a positive effect on visitation in the summer as well as the 'shoulder season' spring and fall months (Jones & Scott, 2006). However, warming trends can cause ecological degradation, and intensify outbreaks of the mountain pine beetle (Morris & Walls, 2009), which visitors view as negative and unacceptable (McFarlane & Witson, 2008). Thus, temperature changes may have mixed effects on park tourists in cooler alpine settings. ...
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Changes in temperature and precipitation can affect tourist experiences. This study examines how summer park visitation has changed in response to temperature and precipitation extremes. The study goals were two-fold. The first is to introduce a framework and the second is to test it in a pilot region with four mountainous National Parks. The framework is designed to compare the vulnerability of seasonal park visitation to shifts in a combined indicator of temperature and precipitation. It uniquely considers needed measurements, and the data required to conduct an analysis. The second goal is to test it in four destinations in the U.S. Northern Rockies, including Glacier, Yellowstone, Grand Teton, and Rocky Mountain National Parks. The preliminary test reveals outlier cases of visitation under wet and dry extremes. The analysis connects time series climate and visitation data for the peak summer season from 1991–2012. Outlier analysis illustrates more change in extremely dry conditions, with four out of the six dry-year outliers resulting in a visitation decline. Whether this decline in park tourism is attributable to climate features, economic factors, or conscious management decisions, these drops have significant economic impacts: estimates of changes in visitor spending during dry years are between roughly 9 and 90 million USD. These differences may be connected to the popular activities in each park, and the extent they are dependent on weather conditions. This framework can be used to test the relationship between climate and tourism visitation in other regions, in various seasons and time frames. The work may inform the tourist sector in adjusting and planning for a range of conditions. We discuss opportunities and conclude with additional needs for understanding the mechanisms behind risk in mountain park tourism under climate extremes.
Annual willingness-to-pay (WTP) for snowmobile recreation in Idaho is estimated using the travel cost method (TCM). On-site snow conditions are important and erratic, thus we collect two measures of the annual trip count, an in-season survey of the expected count, and a post-season survey of the actual count. Two variants of the TCM model are estimated. Using the post-season actual trip count data and the ‘traditional’ TCM model, WTP increases from $41 to $91 per person per trip as the fraction of the wage rate that is used to value the opportunity cost of travel time is increased from 1/4 to one. Using the preferred short-run decision TCM model, WTP increases from $53 to $194 as the snowmobiler ratings of off-trail snow conditions vary from worst to best. WTP estimates using the in-season expected trip count data and the traditional TCM model are much higher (triple) than those found using the post-season actual trip count data, and the confidence intervals are much larger.
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Urban parks are valued for their benefits to ecological and human systems, likely to increase in importance as climate change effects continue to unfold. However, the ability of parks to provide those myriad benefits hinges on equitable provision of and access to green spaces and their environmental quality. A social–ecological approach was adopted in a study of urban park use by recreationists in the City of Los Angeles, contrasting two affluent and two disadvantaged communities situated in coastal and inland zones. Twenty-four days of observations distributed across morning and afternoon time blocks were gathered, with observations in each day drawn from a pair of affluent and disadvantaged community parks. Observers noted location, gender, age, ethnicity/race, and level of physical activity of each visitor encountered during four scheduled observation sweeps on each day of field work. In addition, ozone dose exposure was measured through passive monitoring. Ozone dose exposure was calculated using average hourly ozone in ppb multiplied by METS (metabolic expenditures). Dose exposure was significantly higher in the disadvantaged community parks (with majority Latino use). Findings suggest that additional monitoring in disadvantaged communities, especially inland, may be prudent to facilitate community-based information as well as to assess the degree of potential impact over time. Additionally, mitigative strategies placed in urban parks, such as increased tree canopy may help to reduce the degree of risk and improve community resilience. Future research examining the positive outcomes from physically active use of urban parks may benefit from adopting a nuanced approach in light of the present findings.
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FOR-110, a 5-page illustrated fact sheet by Miriam S. Wyman and Taylor V. Stein, defines eco- and nature-based tourism, provides statistics, and discusses positive and negative aspects, community planning, and describes some successful examples. Includes references. Published by the UF School of Forest Resources and Conservation, April 2007. FOR 110/FR163: Introducing Ecotourism to Florida's Counties and Landowners: An Ecotourism/Nature Based Tourism Fact Sheet (
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21 tree-ring stations, totaling 116 trees, were sampled at varius localities within the forest trimlines fronting the Agassiz and Jackson glaciers. It was found that both glaciers began to retreat from their maximum late-Neoglacial positions c1860. Retreat rates, derived from the tree-ring data, appear to have been modest (under 7m yr-1) until c1910 when they increased, reaching more than 40m-1 for the Agassiz Glacier between 1917 and 1926. Since the mid-1940s the retreat rate of both glaciers has slowed markedly.-from Authors
The glaciers in the Blackfoot-Jackson Glacier Basin of Glacier National Park, Montana, decreased in area from 21.6 square kilometers (km2) in 1850 to 7.4 km2 in 1979. Over this same period global temperatures increased by 0.45°C (± 0. 15°C). We analyzed the climatic causes and ecological consequences of glacier retreat by creating spatially explicit models of the creation and ablation of glaciers and of the response of vegetation to climate change. We determined the melt rate and spatial distribution of glaciers under two possible future climate scenarios, one based on carbon dioxide-induced global warming and the other on a linear temperature extrapolation. Under the former scenario, all glaciers in the basin will disappear by the year 2030, despite predicted increases in precipitation; under the latter, melting is slower. Using a second model, we analyzed vegetation responses to variations in soil moisture and increasing temperature in a complex alpine landscape and predicted where plant communities are likely to be located as conditions change.
One of the most visible and widely felt impacts of climate warming is the change (mostly loss) of low-elevation snow cover in the midlatitudes. Snow cover that accumulates at temperatures close to the ice-water phase transition is at greater risk to climate warming than cold climate snowpacks because it affects both precipitation phase and ablation rates. This study maps areas in the Pacific Northwest region of the United States that are potentially at risk of converting from a snow-dominated to a rain-dominated winter precipitation regime, under a climate-warming scenario. A data-driven, climatological approach of snow cover classification is used to reveal these "at risk" snow zones and also to examine the relative frequency of warm winters for the region. For a rain versus snow temperature threshold of 0°C the at-risk snow class covers an area of about 9200 km2 in the Pacific Northwest region and represents approximately 6.5 km3 of water. Many areas of the Pacific Northwest would see an increase in the number of warm winters, but the impacts would likely be concentrated in the Cascade and Olympic Ranges. A number of lower- elevation ski areas could experience negative impacts because of the shift from winter snows to winter rains. The results of this study point to the potential for using existing datasets to better understand the potential impacts of climate warming.