P. Suresh C. Rao’s research while affiliated with Purdue University and other places

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Publications (146)


Modeling the dynamics and spatial heterogeneity of city growth
  • Article
  • Full-text available

November 2022

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148 Reads

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10 Citations

npj Urban Sustainability

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P. Suresh C. Rao

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Satish V. Ukkusuri

We propose a systems model for urban population growth dynamics, disaggregated at the county scale, to explicitly acknowledge inter and intra-city movements. Spatial and temporal heterogeneity of cities are well captured by the model parameters estimated from empirical data for 2005–2019 domestic migration in the U.S. for 46 large cities. Model parameters are narrowly dispersed over time, and migration flows are well-reproduced using time-averaged values. The spatial distribution of population density within cities can be approximated by negative exponential functions, with exponents varying among cities, but invariant over the period considered. The analysis of the rank-shift dynamics for the 3100+ counties shows that the most and least dense counties have the lowest probability of shifting ranks, as expected for ‘closed’ systems. Using synthetic rank lists of different lengths, we find that counties shift ranks gradually via diffusive dynamics, similar to other complex systems.

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From wetlands to wetlandscapes: Remote sensing calibration of process‐based hydrological models in heterogeneous landscapes

October 2022

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33 Reads

Hydrological Processes

Wetlands are vital components of landscapes that sustain a range of important ecosystem services. Understanding how wetland-rich landscapes - or wetlandscapes - will evolve under a changing climate and increasing anthropogenic encroachment is urgent. Wetlandscapes are highly heterogeneous, and scaling local modelling insights from individual instrumented wetlands to characterize landscape-scale dynamics has been a pervasive challenge. We investigate the potential to use water extent information from satellite imagery to calibrate landscape-scale process-based hydrological models. Applications to wetlandscapes in the Prairie Pothole Region (PPR) in North Dakota and the Texas Playa Lakes (TPL) shed light on two important trade-offs. First, in-situ monitoring provides accurate water extent information on an arbitrary subset of wetlands, whereas satellite imagery captures landscape-scale hydrological dynamics but suffers persistent water-detection challenges. Satellite imagery is a superior source of data for model calibration in sparsely monitored and spatially heterogeneous landscapes like the PPR, where the sampling uncertainty of monitored wetlands exceeds the water detection uncertainty of remote sensing. The two data sources are equivalent for more homogeneous landscapes like the TPL. The second tradeoff concerns the spatial resolution and temporal coverage of satellite imagery. In that regard, the 20 years of bi-weekly images captured by Landsat 7 provides unprecedented insights into the dynamic nature of the ecohydrological characteristics of wetlandscapes, such as seasonal and inter-annual changes of their metapopulation capacity. In the PPR, the amplitude of these dynamics far exceeds the bias introduced by Landsat's inability to capture ecologically important connectivity details due to its coarse spatial resolution compared to more recent imagery.


Schematic representation of the dominant migratory trends that contribute to the heterogeneous population growth of cities
Core counties are more likely to receive inflows from core counties of other cities than from external counties (blue arrows). Flows to and from micro and non-statistical areas are more likely to be found at the external counties of a city (green arrows). Intra-city flows (red arrows) indicate vectors of redistribution of people within the city, and have an outwards radial direction: people move from central counties with larger population density to external counties with lower densities. International inflows (dashed arrows), which scale superlinearly with city population, are more likely to be directed to the core counties of large cities. The resulting spatial heterogeneity is depicted by the background color, in which the red intensity is proportional to the population density. The width of the arrows is proportional to the intensity of the flows.
Heterogeneity of inter- and intra-city netflows
The map (A) suggests that the domestic redistribution of people between different U.S. metro areas are non-uniform: the black arrows, indicating the direction of the most intense inter-city netflows (higher than 2000 people per year), reveal migration trends from northern and eastern cities to western and southern regions. Cities (composed of one or more counties) are colored according to the relative growth (viz. population growth adjusted by population) of the whole MSA during the 2015–2019 period, and the black intensity and the thickness of the arrows are proportional to the netflows. Alaska and Hawaii are not shown. Panels (B–H), which are close-up of New York (B), Chicago (C), Dallas (D), Houston (E), Washington D.C. (F), Philadelphia (G), Atlanta (H), suggest that the most intense intra-city netflows are oriented radially outwards: people are moving from core to external counties. Here, counties are colored according to their relative growth in the 2015–2019 period and the width of the arrows is proportional to the netflows between origin and destination counties.
Roles of intra- and inter-city flows in driving the heterogeneous population growth of cities
We define the core county as the one with the highest population density, and we plot the percentage of inflows due to intra- (A) and inter-city flows (B) of each county within a city as a function of its distance to the core county. The percentage of outflows due to intra- and inter-city flows are shown in (C) and (D), respectively. The positive correlation of the relative growth with distance due to intra-city flows in (E), along with the lack of correlation due to inter-city flows in (F), indicates that intra-city flows are mainly responsible for increasing the population in the external regions of cities. The sizes of red circles and blue squares are proportional to the city population. The range of distances is split into equally spaced bins. The number of counties n within each bin, from left to right, is 46, 1, 4, 7, 7, 17, 21, 31, 36, 38, 34, 31, 31, 30, 20, 20, 21, 14, 17, 9, 9, 6, 4, 2, 5, 5, 2, 1. The black dots and the error bars indicate the mean and the 90% interval, respectively, of the counties within the corresponding bin. We also show the Pearson correlation coefficient R and the p-value associated with the two-sided test of the null hypothesis of non-correlation.
People are moving to counties with lower population density
A The population density of the origin (ρo) and destination (ρd) counties of intra-city netflows for New York, Chicago, Dallas, Houston, Washington D.C., Philadelphia, Atlanta, reveal that the majority of the flows occur from high to low-density counties. The size of the symbols are proportional to the intensity of the netflow, and the black line corresponds to y = x. B The fraction of netflows to lower density counties F\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${{{{{{{\mathcal{F}}}}}}}}$$\end{document} has a positive correlation with city population when we consider the 46 MSAs with more than 5 counties, suggesting that intra-city netflows to lower density counties are more frequent as the city size increases. We also show the Pearson correlation coefficient R and the p-value associated with the two-sided test of the null hypothesis of non-correlation. C The ranking of the cities according to F\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${{{{{{{\mathcal{F}}}}}}}}$$\end{document}.
Inter-city flow patterns depend on the population size of the origin and destination cities
Each point corresponds to a particular city. A Fraction F\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${{{{{{{\mathcal{F}}}}}}}}$$\end{document} of netflows going to lower density counties versus the population of the destination city. Inflows to counties of large cities (with population greater than 10⁶, dashed line) usually comes from counties with lower population densities. B Rank of cities according to the share of inflows from lower density counties. C Fraction F\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${{{{{{{\mathcal{F}}}}}}}}$$\end{document} versus the population of the origin city. Outflows from counties of large cities usually go to cities with lower density counties. D The rank of cities according to the share of inter-city netflows to lower density counties is presented. The dots are colored according to the city population density (darker red means higher density). We also show the Pearson correlation coefficient R and the p-value associated with the two-sided test of the null hypothesis of non-correlation.

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Spatial structure of city population growth

October 2022

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1,091 Reads

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25 Citations

We show here that population growth, resolved at the county level, is spatially heterogeneous both among and within the U.S. metropolitan statistical areas. Our analysis of data for over 3,100 U.S. counties reveals that annual population flows, resulting from domestic migration during the 2015–2019 period, are much larger than natural demographic growth, and are primarily responsible for this heterogeneous growth. More precisely, we show that intra-city flows are generally along a negative population density gradient, while inter-city flows are concentrated in high-density core areas. Intra-city flows are anisotropic and generally directed towards external counties of cities, driving asymmetrical urban sprawl. Such domestic migration dynamics are also responsible for tempering local population shocks by redistributing inflows within a given city. This spill-over effect leads to a smoother population dynamics at the county level, in contrast to that observed at the city level. Understanding the spatial structure of domestic migration flows is a key ingredient for analyzing their drivers and consequences, thus representing a crucial knowledge for urban policy makers and planners.


Fig. 4 People are moving to counties with lower population density. (A) The population density of the origin (ρo) and destination (ρ d ) counties of intra-city netflows for New York, Chicago, Dallas, Houston, Washington D.C., Philadelphia, Atlanta, reveal that the majority of the flows occur from high to low density counties. The size of the symbols are proportional to the intensity of the netflow, and the black line corresponds to y = x. (B) The fraction of netflows to lower density counties F has a positive correlation with city population when we consider the 46 MSAs with more than 5 counties, suggesting that intra-city netflows to lower density counties are more frequent as the city size increases. (C) The ranking of the cities according to F .
Fig. 5 Inter-city flow patterns depend on the population size of the origin and destination cities. Each point corresponds to a particular city. (A) Fraction F of netflows going to lower density counties versus the population of the destination city. Inflows to counties of large cities (with population greater than 10 6 , dashed line) usually comes from counties with lower population densities. (B) Rank of cities according to the share of inflows from lower density counties. (C) Fraction F versus the population of the origin city. Outflows from counties of large cities usually go to cities with lower density counties. (D) The rank of cities according to the share of inter-city netflows to lower density counties is presented. The dots are colored according to the city population density (darker red means higher density).
Spatial Structure of City Population Growth

August 2022

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382 Reads

We show here that population growth, resolved at the county level, is spatially heterogeneous both among and within the U.S. metropolitan statistical areas. Our analysis of data for over 3,100 U.S. counties reveals that annual population flows, resulting from domestic migration during the 2015 - 2019 period, are much larger than natural demographic growth, and are primarily responsible for this heterogeneous growth. More precisely, we show that intra-city flows are generally along a negative population density gradient, while inter-city flows are concentrated in high-density core areas. Intra-city flows are anisotropic and generally directed towards external counties of cities, driving asymmetrical urban sprawl. Such domestic migration dynamics are also responsible for tempering local population shocks by redistributing inflows within a given city. This "spill-over" effect leads to a smoother population dynamics at the county level, in contrast to that observed at the city level. Understanding the spatial structure of domestic migration flows is a key ingredient for analyzing their drivers and consequences, thus representing a crucial knowledge for urban policy makers and planners.


Mobile phone location data for disasters: A review from natural hazards and epidemics

June 2022

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439 Reads

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66 Citations

Computers Environment and Urban Systems

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Nicholas K.W. Jones

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P. Suresh C. Rao

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[...]

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Satish V. Ukkusuri

Rapid urbanization and climate change trends, intertwined with complex interactions of various social, economic, and political factors, have resulted in an increase in the frequency and intensity of disaster events. While regions around the world face urgent demands to prepare for, respond to, and to recover from such disasters, large-scale location data collected from mobile phone devices have opened up novel approaches to tackle these challenges. Mobile phone location data have enabled us to observe, estimate, and model human mobility dynamics at an unprecedented spatio-temporal granularity and scale. The COVID-19 pandemic, in particular, has spurred the use of mobile phone location data for pandemic and disaster management. However, there is a lack of a comprehensive review that synthesizes the last decade of work and case studies leveraging mobile phone location data for response to and recovery from natural hazards and epidemics. We address this gap by summarizing the existing work, and point to promising areas and future challenges for using mobile phone location data to support disaster response and recovery.


Toward data-driven, dynamical complex systems approaches to disaster resilience

February 2022

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643 Reads

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74 Citations

Proceedings of the National Academy of Sciences

With rapid urbanization and increasing climate risks, enhancing the resilience of urban systems has never been more important. Despite the availability of massive datasets of human behavior (e.g., mobile phone data, satellite imagery), studies on disaster resilience have been limited to using static measures as proxies for resilience. However, static metrics have significant drawbacks such as their inability to capture the effects of compounding and accumulating disaster shocks; dynamic interdependencies of social, economic, and infrastructure systems; and critical transitions and regime shifts, which are essential components of the complex disaster resilience process. In this article, we argue that the disaster resilience literature needs to take the opportunities of big data and move toward a different research direction, which is to develop data-driven, dynamical complex systems models of disaster resilience. Data-driven complex systems modeling approaches could overcome the drawbacks of static measures and allow us to quantitatively model the dynamic recovery trajectories and intrinsic resilience characteristics of communities in a generic manner by leveraging large-scale and granular observations. This approach brings a paradigm shift in modeling the disaster resilience process and its linkage with the recovery process, paving the way to answering important questions for policy applications via counterfactual analysis and simulations.


Scale-dependent response of the urban heat island to the European heatwave of 2018

October 2021

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251 Reads

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22 Citations

Extreme heat continues to be a pressing challenge of the changing climate. The impacts of extreme heat manifest on two different spatio-temporal scales: (1) episodic continent-wide heatwaves (HWs) and (2) the city-scale urban heat island (UHI). As HWs are becoming more frequent, longer, and severe, they pose serious implications of increased public health risks at a city scale, and have adverse impacts on agricultural and terrestrial/aquatic ecosystems on the regional scale. Here we offer a fresh perspective of the HW as a forcing that invokes dynamic, heterogeneous, scale-dependent responses evident in inter and intra-urban heat islets. A numerical simulation of the 2018 European HW including the surface and air temperature-based UHIs of six urban agglomerations, with a high-resolution focus on Paris, serves as our case study. We find that the mean nighttime UHI intensities are reduced for inland cities but increased for coastal cities. Our examination of the heat islets reveals two major findings: (i) the HW homogenizes the intra-urban surface temperatures during the daytime (reduces variance), (ii) the HW impacts are most significant on the scale of large, spatially discontiguous extreme heat islets during nighttime. These results underscore the need to move beyond the prevalent HW-mean UHI intensity characterization and toward intra-urban heat islet analyses that aid targeted mitigation.


FIGURE 1 | Maps of human-related attributes distributed over the Weser River Basin of which location within Germany is shown in the most left figure. (A) Distribution of ∼8.4 million people as the number of persons per grid with a range from 1 to 25. River network with the final 7th order is overlaid with black lines of which thickness and brightness are proportional to stream-orders. Dashed and solid triangles indicate the outlets of four sub-basins with 5th-order (F, W, L, and A for Fulda, Werra, Leine, and Aller) and two sub-basins with 6th-order (W and L for Weser and Leine), respectively. (B) Distribution of ∼845 WWTPs categorized as five class-sizes of which color-codes are given in the legend. (C) Distribution of five types of land-cover of which areas are visualized with different colors [(B,C) were adapted from Yang et al. Copyright (2021), with permission from Elsevier].
FIGURE 4 | Distributions of the removed P tot loads along the Weser River network under the mean river discharge. (A) Entire basin-scale distribution for the fraction f R of P tot loads removed in each reach (L r ) to input mass flux to the same reach (L in ). (B) Stream-order ω based distribution for f R . (C) Distribution of the fraction of total P tot loads removed by upstream catchment F R at a given drainage area A. (D) The ω-based distribution for L r . (E) Distribution of removed P tot loads per unit length in each reach, ζ r , over A. For visual efficiency, values of gray dots in (B,D) were extracted from the most downstream point of each stream for a given ω. Hortonian scaling equation and the corresponding scaling ratio are in (B,D). Blue dots in (C,E) indicated the model results for each stream reach of the Weser River network. Dashed black line in (C) and (E) was plotted by following the analytical scaling of Equations (12) and (10) derived in Bertuzzo et al. (2017), respectively. Following the original framework, the exponent α = 0.91 was fitted from scaling of input mass flux only from diffuse-sources over drainage areas. The other exponent α w = 0.5 came from the hydraulic geometry scaling between width and river discharge.
Hortonian scaling ratios for the Weser River Basin and six sub-basins.
Hortonian Scaling of Coupled Hydrological and Biogeochemical Responses Across an Intensively Managed River Basin

August 2021

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133 Reads

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7 Citations

Frontiers in Water

Structural and functional attributes across fractal river networks have been characterized by well-established and consistent hierarchical, Hortonian scaling patterns. In most of the global river basins, spatial patterns of human settlements also conform to similar hierarchical scaling. However, emergent spatial hierarchical patterns and scaling of heterogeneous anthropogenic nutrient loads over a river basin are less known. As a case study, we examined here a large intensely managed river basin in Germany (Weser River; 46K km2; 8M population). Archived data for point-/diffuse-sources of total Phosphorus (Ptot) input loads were combined with numerical and analytical model simulations of coupled hydrological and biogeochemical processes for in-stream Ptot removal at the network scale. We find that Ptot input loads scale exponentially over stream-orders, with the larger scaling constant for point-source loads from urban agglomerations compared to those for diffuse-source contributions from agricultural and forested areas. These differences in scaling patterns result from hierarchical self-organization of human settlements, and the associated clustering of large-scale, altered land-cover. Fraction of Ptot loads removed through in-stream biogeochemical processes also manifests Hortonian scaling, consistent with predictions of an analytical model. Our analyses show that while smaller streams are more efficient in Ptot removal, in larger streams the magnitude of Ptot loads removed is higher. These trends are consistent with inverse scaling of nutrient removal rate constant with mean discharge, and downstream clustering of larger cumulative input loads. Analyses of six nested sub-basins within the Weser River Basin also reveal similar scaling patterns. Our findings are useful for projecting likely water-quality spatial patterns in similar river basins in Germany, and Central Europe. Extensions and generalizations require further examination of diverse basins with archetype spatial heterogeneities in anthropogenic pressures and hydroclimatic settings.


Mobile Phone Location Data for Disasters: A Review from Natural Hazards and Epidemics

August 2021

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446 Reads

Rapid urbanization and climate change trends are intertwined with complex interactions of various social, economic, and political factors. The increased trends of disaster risks have recently caused numerous events, ranging from unprecedented category 5 hurricanes in the Atlantic Ocean to the COVID-19 pandemic. While regions around the world face urgent demands to prepare for, respond to, and to recover from such disasters, large-scale location data collected from mobile phone devices have opened up novel approaches to tackle these challenges. Mobile phone location data have enabled us to observe, estimate, and model human mobility dynamics at an unprecedented spatio-temporal granularity and scale. The COVID-19 pandemic has spurred the use of mobile phone location data for pandemic and disaster response. However, there is a lack of a comprehensive review that synthesizes the last decade of work leveraging mobile phone location data and case studies of natural hazards and epidemics. We address this gap by summarizing the existing work, and pointing promising areas and future challenges for using data to support disaster response and recovery.


Resilience of Interdependent Urban Socio-Physical Systems using Large-Scale Mobility Data: Modeling Recovery Dynamics

August 2021

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141 Reads

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38 Citations

Sustainable Cities and Society

Cities are complex systems comprised of socioeconomic systems relying on critical services delivered by multiple physical infrastructure networks. Due to interdependencies between social and physical systems, disruptions caused by natural hazards may cascade across systems, amplifying the impact of disasters. Despite the increasing threat posed by climate change and rapid urban growth, how to design interdependencies between social and physical systems to achieve resilient cities have been largely unexplored. Here, we study the socio-physical interdependencies in urban systems and their effects on disaster recovery and resilience, using large-scale mobility data collected from Puerto Rico during Hurricane Maria. We find that as cities grow in scale and expand their centralized infrastructure systems, the recovery efficiency of critical services improves, however, curtails the self-reliance of socio-economic systems during crises. Results show that maintaining self-reliance among social systems could be key in developing resilient urban socio-physical systems for cities facing rapid urban growth.


Citations (85)


... Transfer learning, a concept wherein knowledge gained in one domain is applied to another related domain (Pan and Yang 2010;Weiss, Khoshgoftaar, and Wang 2016), can potentially serve as a novel approach to assessing different aspects of cities' balance (Reia, Rao, and Ukkusuri 2022;Y. Ma et al. 2024). ...

Reference:

Transferred Bias Uncovers the Balance Between the Development of Physical and Socioeconomic Environments of Cities
Modeling the dynamics and spatial heterogeneity of city growth

npj Urban Sustainability

... These motivators may be internal or external, ranging from local policy decisions to global economic forces. By analyzing spatial growth, researchers can gain insights into the social, economic, and environmental implications of urban and regional development (Reia, Rao, Barthelemy, & Ukkusuri 2022). ...

Spatial structure of city population growth

... Many studies across different disciplines have used various types of data from physical and social spaces to support urban emergency management (Gong et al. 2023), such as geospatial data, census data, social media data, mobile phone data, and transportation data, with the goal of constructing a model that reflects the dynamic situation in an emergency (Jing et al. 2023;Luna and Pennock 2018;Mei et al. 2015;Yabe et al. 2022). However, most of the existing research is fragmented and lacks a common vision towards a converging paradigm. ...

Mobile phone location data for disasters: A review from natural hazards and epidemics
  • Citing Article
  • June 2022

Computers Environment and Urban Systems

... This study aims to assess and anticipate the resilience of EVCS using a forward-looking approach under scenarios of rapid-onset disturbances, which can be worsened by uncertain stressors, such as climate change. One powerful method is counterfactual thinking (Woo, 2019;Yabe et al., 2022). Downward counterfactual thinking is rooted in historical catalog events aimed at tracking "Black Swans" -lowpossibility, high-cost extreme events -using alternative outcomes worse than what actually occurs (Woo, 2019). ...

Toward data-driven, dynamical complex systems approaches to disaster resilience

Proceedings of the National Academy of Sciences

... The topological structure of the river network can be quantified using stream ordering and empirical scaling laws (Horton, 1945;Schumm, 1956;Strahler, 1957). Stream ordering and scaling laws can be useful to identify the archetypes of organization of various properties that tend to evolve along the river networks (Fig. 11), such as riparian vegetation (Dunn et al., 2011), human settlements (Fang et al., 2018), land use patterns (Kang et al., 2008;Miyamoto et al., 2011) or nutrient pollution sources (Yang et al., 2021b). The width function (Rinaldo et al., 1991;Marani et al., 1994) that represents the distribution of distances to outlet within catchments (Fig. 11), is another metric to capture the topological structure of river networks and to infer the characteristic hydrological response of differently shaped networks (Moussa, 2008). ...

Hortonian Scaling of Coupled Hydrological and Biogeochemical Responses Across an Intensively Managed River Basin

Frontiers in Water

... While many important gaps and questions still exist with respect to this infrastructure resilience modeling paradigm, recent research trends suggest that we will slowly chip away at some of these needs. For example, developing missing models for understudied hazards or infrastructures 10-13 ; representing infrastructure systems as the socio-technical systems that they truly are when modeling their performance over time [14][15][16][17][18] ; tightening model coupling across natural-built-socio-economic systems when evaluating broader system dynamics and metrics of resilience [19][20][21][22][23][24] ; or integrating alternative decision algorithms with these resilience models to support interventions at different stages of the disaster life-cycle 4,[25][26][27][28] . However, future cities demand more from our infrastructure resilience algorithms and models, posing heightened challenges and opportunities. ...

Resilience of Interdependent Urban Socio-Physical Systems using Large-Scale Mobility Data: Modeling Recovery Dynamics

Sustainable Cities and Society

... First, social media platforms can effectively supplement the lack of interactivity in traditional mainstream media, thus providing a platform for more independent, interactive, and participatory debate on public agendas such as election campaigns and the response to the COVID-19 epidemic [10,11]. Social media platforms can also help the government and citizens keep in touch [12], and even in the face of extreme situations such as sudden disasters, the state can effectively disseminate political information, emergency warnings, or other information serving a social function [13,14]. Social media users can supervise the mainstream media and effectively record and question false statements [15]. ...

Modeling the Influence of Online Social Media Information on Post-Disaster Mobility Decisions

Sustainability

... Eutrophication has been a global ecosystem problem since the 1970s (Jarvie et al., 2013) and continues to be a challenge nowadays (Bol et al., 2018). River basins continue presenting episodes of eutrophication (Yang et al., 2021) and under the current climatic change scenario of high temperatures and low flow it is predicted that the situation will worsen (Gilbert et al., 2020). Substantial management efforts have been put into reducing nutrient pollution and setting limits to external nutrient inputs, but many aquatic ecosystems have not recovered accordingly (Saia et al., 2017;Wentzky et al., 2018;Berthold and Schumann, 2020). ...

Emergent spatial patterns of competing benthic and pelagic algae in a river network: A parsimonious basin-scale modeling analysis

Water Research

... Climate change has made existing risks worse [11] by enhancing the level of potential destruction and the frequency of events. It is essential to think about climate change for informal settlements because climate change is occurring and it is already impacting vulnerable areas in severe ways; in disasters, one may expect the devastation experienced in these areas to grow [86]. ...

Regional differences in resilience of social and physical systems: Case study of Puerto Rico after Hurricane Maria

Environment and Planning B Urban Analytics and City Science