Article

The calculation of climatic design conditions in the 2005 ASHRAE Handbook - Fundamentals

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Abstract

ASHRAE Research project 1273-RP recalculated and expanded the tables of climatic design conditions in the ASHRAE Handbook - Fundamentals. These tables provide values of dry-bulb, wet-bulb, and dew-point temperature, enthalpy, and wind speed at various frequencies of occurrence over annual and monthly periods and for some of these, mean coincident values of other variables of interest. Compared to the previous edition of the Handbook, the new tables include additional elements and are calculated for a much greater number of stations over a longer period of record. This paper explains the procedure used to compute the design conditions, the data sources used, the techniques employed to screen out erroneous data, and the completeness criteria required by the calculation. It also provides a summary of the stations included in the 2005 Handbook and a brief description of how the new values compare to those published in the 2001 edition. Finally, the paper provides an overview of the capability of the Weather Data Viewer, a companion CD-ROM that gives full access to the frequency information used to compile the tables of climatic design conditions.

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... Finally, the performance of buildings' cooling systems in Texas was evaluated based on climatic changes. Therefore, this study aims to answer the following research questions: After evaluating climatic outdoor design conditions in terms of both dry bulb temperature (DBT) and wet bulb temperature (WBT), based on the ASHRAE technical report [26], the first section of the study looks at the demographic trend impact on DBT and WBT in selected cities over thirty years (in each five-year interval). In the second part, the impact of climate change on variations in cooling degree hours (CDH), heating degree hours (HDH), and neutral mode (NM) parameters are evaluated under the influence of the DBT trend. ...
... To evaluate climatic outdoor design conditions, it is necessary to consider annual simple climate design values according to the 2005 ASHRAE Handbook-Fundamentals [26]: ...
... For example, the 0.4% dry-bulb design condition had been calculated by totaling rows in the (dry-bulb, dewpoint) joint frequency matrix, which resulted in indices such as DBT and dew point temperature not being considered. In the new edition [26], however, the frequency vectors were formed by the number of hours (Nbin) within each temperature interval (bin). The present study estimates the frequency vector for a total period of 30 years (from 1990 to 2020) at successive five-year interval periods (six different time frames : 1990-1995, 1995-2000, 2000-2005, 2005- ...
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... The reporting stations in the HOF'09 dataset are widely distributed and representative of major climatic zones [18]; hence, suitable for a global analysis of the relationship between annual mean temperature and degreedays. Further details on the dataset and underlying methodology are discussed in [2,19,20]. ...
... Given the regression coefficients for HDD 18.3 and CDD 10 in Tables 2 and 4, respectively, the relationship between degree-days and the independent variables in model #6 can be described as Eqs. (18) and (19). ...
... Errors in Eqs. (18) and (19) tend to occur at lower tail ends of HDD 18.3 and CDD 10 respectively. This is primarily because of points of inflection in 4th order curves in Fig. 2. Closer inspection of the original data reveals that degree-days around the inflection points are very low -either zero or very close to zero. ...
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Degree-days are a versatile climatic indicator and used for many applications in the design and operation of en- ergy efficient buildings – from the estimation of energy consumption and carbon emissions due to space heating and cooling to the energy and environmental monitoring of buildings. This research is aimed at developing an equation for calculating degree-days from low-resolution temperature data by exploring the relationship between degree-days and annual mean temperature of 5511 locations around the world, using multiple non-linear regres- sion. Results suggest a very strong relationship between annual mean temperature and degree-days. Incorporating standarddeviation(SD)ofmonthlymeantemperatureandlatitudeincreasestheaccuracyofprediction(R2 >.99), demonstrating the strength of the location-agnostic relationship in predicting degree-days from two temperature parameters: annual mean and SD of monthly mean. Research findings can be used to calculate degree-days of loca- tions, for which daily temperature data may not be available. The equation can also be used to calculate degree-days from low-resolution global circulation model (GCM) projections of increasing temperature, for investigating the im- pact of climate change on building heating and cooling energy demand at global scale without the need to create synthetic weather series through morphing or downscaling.
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... MATLAB code is developed for the solar intensity on tilted surfaces using equations reported in (Thevenard and Humphries, 2005) to determine the ideal yearly solar collector tilting angle that provides the maximum yearly solar radiation collected on the collector at a certain location (Tanta City), and it was found to be 25 • with the horizontal as shown in Fig. 10. The collector tilting angle of 25 • is taken into account in calculations for solar air and water heaters. ...
... Liquid condensed film heat transfer coefficient for plain tub. All properties of the liquid are to be evaluated at the film temperature:(Thevenard and Humphries, 2005) Dh d t,o,co * N t,co * ( T a,sat,Dh − T t,o,co )Coefficient of convective heat transfer in an air flow around tubes(Cengel and Heat, 2003)h a,Dh = C 2 C 1 Pr 0.31 (Re d,max ) m Where C 2 = 0.95 is the correction factor for N t,o,co < 20 Re d,max = ρ a,Dh u a,max d t,o,co μ a,Dh u a,max =ṁ Diffusivity coefficient of vapor in the air [41] h a,Dh = Km a,Dh C p,a,Dh Le 2/3 h a,Dh ≅ Km a,Dh C p,a,Dh Km a,Dh = h a,Dh C p,a,Dh Convective heat transfer coefficient through a water flowing inside the tubes (Cengel and Heat, 2003) For > >> Re d,sw < 2300 h sw,Dh = 1.86 For > >> 2300 ≤ Re d,sw ≤ 10 4For > >> Re d,sw > 10 4 ...
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... The four rules that are to be fulfilled for a day to be considered valid are: Rule A: Every climatic parameter has to be valid in at least 18 h during the day. This has to be satisfied in order to have consistent data to be used in the computation and avoid the presence of too many gaps to be filled with interpolation in the following steps [23]; ...
... This condition is necessary because, if interpolation of values is to be taken in the first/last day, a valid data may be required in the first/last hour to compute the interpolated values; Rule C: For every climatic parameter, a maximum of 6 consecutive hours of invalid data is acceptable across two contiguous days. This limitation aims to avoid the problem of interpolating data across too long time intervals as, for example, near stocks of 5 + 5 h of invalid values [23]; ...
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... Given the regression coefficients for HDD 18.3 and CDD 10 in Tables 2 and 4 respectively, the relationship between degree-days and the independent variables in model #6 can be described as Equations 18 and 19.19) where, HDD 18.3 is annual heating degree-days at 18.3°C (°C-day), CDD 10 is annual cooling degree-days at 10°C (°C-day), T is annual mean temperature (°C), S m is standard deviation of monthly mean temperatures (°C) and L is the latitude of the location in decimal degree (°) where north latitudes are positive and south latitudes are negative. Errors in Equations 18 and 19 tend to occur at lower tail ends of HDD 18.3 and CDD 10 respectively. ...
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... The conservation equations for heat and mass are written for each At the beginning, the input parameters were equal to the data taken from that measured by [166] on that day in 2020; spring 21/3, summer A MATLAB code is developed for the solar intensity on tilted surfaces using equations reported in [167] to determine the ideal yearly solar collector tilting angle that provides the maximum yearly solar radiation collected on the collector at a certain location (Tanta City), and it was found to be 25° from the horizontal that is taken into calculations for solar air and water heaters (see APPENDIX (A)). ...
Thesis
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... The evaluation of the annual dry-bulb design criteria is based on a comparison of the annual 99.6%, 99.0%, 2.0%, 1.0%, and 0.4% dry-bulb temperatures estimated from the MERRA-based cumulative distribution functions (CDFs) developed from the MERRA hourly temperatures and the corresponding annual 99.6%, 99.0%, 2.0%, 1.0%, and 0.4% dry-bulb temperatures taken from the WDV-4, where the site specific values from the WDV-4 are based upon surface station hourly observations. The methodology for determining the annual CDFs and subsequently the 99.6%, 99.0%, 2.0%, 1.0%, and 0.4% dry-bulb temperatures is described in Thevenard and Humphries (2005) and by Thevenard (2009). Evaluation of the MERRA-based annual design conditions focused on the CONUS study-region, and was accomplished by first acquiring the MERRA hourly temperature for the 6480 0.5°grid boxes contained within the CONUS study-region. ...
Conference Paper
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ASHRAE Technical Committee 4.2, Climatic Information, publishes a quadrennial update of climatic design information in Chapter 14 of the ASHRAE Handbook - Fundamentals(ASHRAE 2009a). The design information for 5564 locations around the world is based upon hourly values of dry-bulb temperature, wet-bulb temperature, dew-point temperature, wind speed and direction, surface pressure, and solar radiation. The 2009 design conditions provided a significant enhancement over the 2005 design conditions with respect to the global coverage - 5564 locations in 2009 versus 4422 locations in 2005. The ASHRAE design conditions, based on meteorological data, are calculated using hourly surface data from stations having a minimum of 8 years of observations, but more stations typically span 25 years of observations; although frequently the time series are discontinuous. The ASHRAE solar-related design conditions are based on model-derived solar radiation. A potential source for both global and time contiguous meteorological and solar data is NASA’s POWER(Prediction of Worldwide Energy Resource) web portal (NASA2013a). This includes the recently available meteorological data based on an improved reanalysis model - Modern Era Retrospective-analysis for Research and Applications(MERRA). MERRA yields global, hourly surface meteorological parameters for the years 1981 to present. An initial evaluation of the MERRA daily maximum, minimum, and averaged temperatures indicates accuracies sufficient to warrant their use to supplement existing surface observations. In this paper, we present an evaluation of the accuracy of the MERRA daily temperatures, followed by an assessment of the applicability of the MERRA hourly temperatures in the development of annual dry-bulb climate design criteria and annual heating and cooling degree-days over the continental United States.
... The 2005 edition increased the number of world sites to 4422, and introduced many improvements, particularly in the number of temperature-and humidity-related parameters, and their statistical interactions. These improvements reflected the results from an exhaustive study (Thevenard and Humphries, 2005). However, the SHG calculation method remained unchanged, despite the known problems and limitations of the ASHRAE radiation model, which are discussed in Section 2. Because of the need for a more accurate and universal radiation model, another study has recently been conducted to improve the incident radiation modeling and SHG calculation methodology, while further (i) expanding the number of world sites to over 5400 worldwide; (ii) providing still more climatological indices and monthly statistics. ...
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This paper establishes the formulation of a new clear-sky solar radiation model appropriate for algorithms calculating cooling loads in buildings. The aim is to replace the ASHRAE clear-sky model of 1967, whose limitations are well known and are reviewed. The new model is derived in two steps. The first step consists of obtaining a reference irradiance dataset from the REST2 model, which uses a high-performance, validated, two-band clear-sky algorithm. REST2 requires detailed inputs about atmospheric conditions such as aerosols, water vapor, ozone, and ground albedo. The development of global atmospheric datasets used as inputs to REST2 is reviewed. For the most part, these datasets are derived from space observations to guarantee universality and accuracy. In the case of aerosols, point-source terrestrial measurements were also used as ground truthing of the satellite data. The second step of the model consists of fits derived from a REST2-based reference irradiance dataset. These fits enable the derivation of compact, but relatively accurate expressions, for beam and diffuse clear-sky irradiance. The fitted expressions require the tabulation of only two pseudo-optical depths for each month of the year. The resulting model, and its tabulated data, are expected to be incorporated in the 2009 edition of the ASHRAE Handbook of Fundamentals.
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The active chilled beam system has been popularly used in office and meeting rooms. There are very few studies of their terminal configuration on the thermal comfort and ventilation performance of systems with different heat gains. A comparative experimental study was implemented in mock-up office and meeting rooms to provide a comprehensive evaluation of the airflow patterns, air distribution, ventilation effectiveness, and local thermal comfort of the 4-way system. Four different terminal layouts with two types of the chilled beams (600 unit and 1200 unit sized 0.6m × 0.6m and 1.2m × 0.6m, respectively) were tested at three heat gain levels: low (46W/m²) and medium (66W/m²) heat gains in the office room, and high (92W/m²) heat gain in the meeting room. The results revealed that the terminal layouts and heat gain levels had significant effects on air distribution and local thermal comfort. The increased heat gains generated lower heat removal effectiveness, worse indoor thermal uniformity, and increased risk of draught. Generally, the 1200-unit system performed better than that with 600 units for heat removal effectiveness and contaminant removal effectiveness. In terms of local thermal comfort, the 600-unit system generally provided higher performance than that with the 1200-unit system. The practical recommendations for the system design and operation stages are provided based on the operating range of the 4-way systems under variable terminal layouts and heat gain conditions.
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Understanding the climate and location aspects are usually the first step in energy applications - from buildings to renewable energy. With so many of the renewable energy sources being significantly dependent on weather, it is essential that the temporal and geospatial variability and distribution of climatic design parameters are investigated for effective planning and operation. ASHRAE-HOF is the most widely used climatic design conditions database for building energy and HVAC professionals, but gaps exist in the literature on the geospatial and temporal distributions of the HOF dataset. This research explored geospatial distributions of key HOF (2009) climatic parameters: temperature (dry-bulb, wet-bulb, dew-point and mean) and degree-days at various temporal scales. Identified spatial variability illustrate the effects of latitude, elevation, landuse and nearest coastline. Observed trends agree with conventional wisdom; however, sparse coverage in populated areas such as Africa and Asia diminish the versatility of the database. Variations in temperature exist, even between closely spaced sites -emphasizing the need to use location-specific data for enhancing the accuracy of the weather-related analysis. Moreover, latitudinal similarities in the distribution offer potential in identifying candidate locations for reciprocal transfer of knowledge on environmental design and operation.
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Calculation of climatic design conditions and cooling and heating degree days using data from different decades for 1274 stations worldwide reveals long-term trends. Over the last three decades, climatic design conditions have increased at an average rate of 0.76°C/decade (137°F/decade) for the 99.6% heating dry bulb temperature, 0.38°C/decade (0.68°F/decade) for the 0.4% cooling design temperature, and 0.28°C/decade (0.50°F/decade) for the 0.4% dehumidification dew point temperature. Annual heating degree-days have decreased on average by 118°C-day/decade (212°F-day/decade) while annual cooling degree days have increased by 68°C-day/decade (122°F-day/decade). These changes are indicative of a warming of the climate experienced by the monitoring stations. However, the magnitude of that warming indicates that it is probably less related to global warming than to the urban heat island effect; it is likely an indication of the built environment encroaching on locations where meteorological stations are situated, particularly airports. The paper also studies the appropriate period of record to use for the calculation of climatic design conditions and degree-days. The use of a 30-year period is recommended; the use of shorter periods of record encompassing only recent years, in order to better capture climatic trends, results in an added uncertainty that is greater than the observed climate trends themselves.
Conference Paper
ASHRAE Research Project RP-1613 prepared an update of the climatic design conditions for the "Climatic Design Information" chapter of ASHRAE Handbook - Fundamentals and for ANSI/ASHRAE Standard 169, Weather Data for Building Design Standards. This update resulted in an increase of the number of stations to 6443 (a 16% increase compared to 2009) and the inclusion of precipitation data used in particular to determine climate zones in energy standard ANSI/ASHRAE/IES Standard 90.1. A more recent period of record (1986-2010 for most stations) was used to incorporate changes in the climate. Compared to the previous edition, climatic design temperatures are generally slightly higher, cooling degree are slightly higher, and heating degree-days are lower, which is indicative of a general warming of the climate. In addition, RP-1613 prepared an update of the Weather Data Viewer, a stand-alone product used by engineers to access the full single- and joint-frequency distributions of all the climatic design parameters listed in ASHRAE Handbook Fundamentals, as well as additional parameters, such as temperature bin data and wind roses. Part two of the paper, "Revising ASHRAE Climatic Data for Design and Standards - Part II: Clear-Sky Solar Radiation Model," provides a detailed description of the changes made to the clear-sky solar radiation model.
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This paper summarizes the preparation of climatic design conditions for the 2009 ASHRAE Handbook - Fundamentals. The project (a) redefined new percentiles of monthly dry bulb and wet bulb temperatures to represent 'less extreme ' conditions than those used in the past, (b) added new monthly dry bulb and wet bulb coincident temperature ranges which can be used for the derivation of daily temperature profiles, (c) calculated heating and cooling degree-days base 50°F (10°C) and 65°F (18.3°C), in support of various standards including ASHRAE Std. 90.1-2004, and added parameters to accurately evaluate degree-days to any other base, and (d) developed a new clear sky solar irradiance model, to overcome the known limitations of the existing ASHRAE clear sky model and extend its applicability to the whole world. The most recent 25 years of climatic data (1982-2006 at the time of processing) were used to calculate the revised tables of climatic design conditions. This provides a balance between accounting for long-term trends and the sampling variation owing to year-to-year variation. Processing led to the calculation of climatic design conditions for a total of 5,564 locations worldwide.
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