@ The University of Oklahoma

Author: Chenghao Wang Page 2 of 6

New paper on continental-scale urban hydroclimate modeling evaluation published in Urban Climate

Our new paper, “Assessment of convection-permitting hydroclimate modeling in urban areas across the contiguous United States“, is published in Urban Climate (IF: 6.0). This work was led by undergraduate student Liam Thompson. Congratulations, Liam!

The paper can be downloaded at https://www.sciencedirect.com/science/article/pii/S2212095525000914.

Authors: Liam Thompson, Chenghao Wang, Cenlin He, Tzu-Shun Lin, Changhai Liu, and Jimy Dudhia

Abstract: Accurate representation of urban areas in weather and climate models is crucial for simulating interactions between urban surfaces and the atmospheric boundary layer, especially in high-resolution regional models that resolve deep convection. However, many continental-scale simulations use simplified urban parameterizations, raising questions about their ability to reproduce urban hydroclimate. This study evaluates CONUS404—a recent USGS-NCAR 4-km convection-permitting hydroclimate modeling dataset—in urban areas across the contiguous United States (CONUS). We assessed hourly near-surface air temperature, dewpoint, and wind speed simulations at 208 urban and 342 non-urban station locations from 2011 to 2020 using observations. Results show that CONUS404 performs better for air temperature in urban areas, with a slight mean warm bias (0.08 °C) at urban stations and a mean cold bias (−0.52 °C) at non-urban stations. Dewpoint simulations exhibit stronger dry biases at urban stations, suggesting underrepresented evapotranspiration from urban vegetation. Wind speed is generally underestimated, with average biases of −0.74 m s−1 at urban and −0.35 m s−1 at non-urban stations. Seasonal analyses reveal larger model errors for wintertime temperature and dewpoint that strongly depend on urban fraction. These findings highlight the limitations of the bulk urban parameterization in CONUS404, underscoring the need for enhanced urban representations to improve continental-scale hydroclimate simulations.

DOI: https://doi.org/10.1016/j.uclim.2025.102375

Fig. 9. Dependence of (a–c) MAE and (d–f) MBE for modeled hourly near-surface air temperature (a, d), dewpoint (b, e), and wind speed (c, f) on urban fraction across 208 urban grids. A linear or multi-linear regression line is fitted to the mean MAE and MBE of each plot, using the higher R2 of the fitted model. Each boxplot contains 40–43 urban grids/station locations. An F-test was performed to determine the overall goodness of fit of the model. N.S. indicates not significant, while *, **, and *** denote statistically significant with p < 0.05, 0.01, and 0.001, respectively. The box denotes the interquartile range (IQR) that represents the distribution of CONUS404 errors between the upper and lower quartiles, the whiskers represent the distribution of errors ±1.5 × IQR, and points outside the core box and whiskers are outliers.

New review paper on CO2 exchanges of urban trees published in Journal of Environmental Management

Our new paper, “Impact of urban trees on carbon dioxide exchange: Mechanistic pathways, environmental controls, and feedback“, is published in Journal of Environmental Management (IF: 8.0).

The paper can be downloaded at https://www.sciencedirect.com/science/article/pii/S0301479725000040.

Authors: Zhi-Hua Wang, Peiyuan Li, Chenghao Wang, & Xueli Yang

Abstract: The increase of carbon dioxide (CO2) concentration in the atmosphere is held responsible for global climate changes. To meet the objective of achieving carbon neutrality and keeping global warming in check, many cities, as hotspots of CO2 emissions, have been promoting the use of urban greenery, urban trees in particular, to mitigate carbon emissions from the built environment. However, there remain large uncertainty and divergence of the potential of urban trees for carbon mitigation, with the underlying mechanisms poorly understood. In this study, we conducted a comprehensive survey of the biophysical functions, their environmental controls, and possible heat-carbon-water feedback that mechanistically govern the CO2 exchange processes of trees in the built environment. This review helps to clarify some disparities and enables us to gain clearer insights into the participatory role of urban trees in the dynamics of CO2 exchange. In addition, we proposed a few guidelines for urban planning and management strategies of using trees to promote the sustainability of urban ecosystems.

DOI: https://doi.org/10.1016/j.jenvman.2025.124028

Fig. 1. Schematics of (a) plant biogenic CO2 processes in an urban setting, (b) stomatal exchange of CO2 by photosynthesis and leaf respiration of trees, and (c) total net ecosystem exchange (NEE) as a result of gross primary productivity (GPP) and ecosystem respiration (R).

New paper on an urban weather database published in Scientific Data

Our new paper, “CHUWD-H v1.0: a comprehensive historical hourly weather database for U.S. urban energy system modeling“, is published in Scientific Data (IF: 5.8).

The paper can be downloaded at https://www.nature.com/articles/s41597-024-04238-4.

Authors: Chenghao Wang, Chengbin Deng, Henry Horsey, Janet L. Reyna, Di Liu, Sarah Feron, Raúl R. Cordero, Jiyun Song, & Robert B. Jackson

Abstract: Reliable and continuous meteorological data are crucial for modeling the responses of energy systems and their components to weather and climate conditions, particularly in densely populated urban areas. However, existing long-term datasets often suffer from spatial and temporal gaps and inconsistencies, posing great challenges for detailed urban energy system modeling and cross-city comparison under realistic weather conditions. Here we introduce the Historical Comprehensive Hourly Urban Weather Database (CHUWD-H) v1.0, a 23-year (1998–2020) gap-free and quality-controlled hourly weather dataset covering 550 weather station locations across all urban areas in the contiguous United States. CHUWD-H v1.0 synthesizes hourly weather observations from stations with outputs from a physics-based solar radiation model and a reanalysis dataset through a multi-step gap filling approach. A 10-fold Monte Carlo cross-validation suggests that the accuracy of this gap filling approach surpasses that of conventional gap filling methods. Designed primarily for urban energy system modeling, CHUWD-H v1.0 should also support historical urban meteorological and climate studies, including the validation and evaluation of urban climate modeling.

DOI: https://doi.org/10.1038/s41597-024-04238-4

Database DOI: https://doi.org/10.17605/OSF.IO/5DP8E

Interactive Data Platform: https://arcg.is/COWWe

Fig. 1. Spatial distribution of the 550 representative weather stations in CHUWD-H v1.0, color coded by classification according to the official TMY3 dataset. Class I stations have the lowest uncertainty, Class II stations have moderate uncertainty, and Class III stations have the most data gaps. Shaded areas in orange are urban areas with populations of at least 50,000.

New paper on the cooling effect of urban trees published in Communications Earth & Environment

Our new paper, “Cooling efficacy of trees across cities is determined by background climate, urban morphology, and tree trait“, is published in Communications Earth & Environment (IF: 8.1).

The paper can be downloaded at https://www.nature.com/articles/s43247-024-01908-4.

Authors: Haiwei Li, Yongling Zhao, Chenghao Wang, Diana Ürge-Vorsatz, Jan Carmeliet, & Ronita Bardhan

Abstract: Urban planners and other stakeholders often view trees as the ultimate panacea for mitigating urban heat stress; however, their cooling efficacy varies globally and is influenced by three primary factors: tree traits, urban morphology, and climate conditions. This study analyzes 182 studies on the cooling effects of urban trees across 17 climates in 110 global cities or regions. Tree implementation reduces peak monthly temperatures to below 26 °C in 83% of the cities. Trees can lower pedestrian-level temperatures by up to 12 °C through large radiation blockage and transpiration. In tropical, temperate, and continental climates, a mixed-use of deciduous and evergreen trees in open urban morphology provides approximately 0.5 °C more cooling than a single species approach. In arid climates, evergreen species predominate and demonstrate more effective cooling within compact urban morphology. Our study offers context-specific greening guidelines for urban planners to harness tree cooling in the face of global warming.

DOI: https://doi.org/10.1038/s43247-024-01908-4

Fig. 1. a Urban trees moderate urban warming caused by urban heat island (UHI) effects. b Interconnecting factors determine the cooling benefits of urban trees. Maximized cooling from urban trees is achieved by selecting the optimal trees and their placement, with an articulated understanding of the interconnecting elements: background climates, tree traits, and urban morphology. The cooling effect of urban trees is determined by a combination of mechanisms, such as shading (shortwave radiation blocking) and transpiration. On the leaf and its stomata scale, the leaf energy balance can be represented by qsen (sensible heat flux) +qlat (latent heat flux)=qrad,l (net longwave radiation) + qrad,s (net shortwave radiation).

Liam Thompson won the First Generation UReCA Fellowship

Liam Thompson recently won the First Generation Undergraduate Research and Creative Activity (UReCA) Fellowship. This fellowship offers financial support to OU students who would like to undertake a project over the course of a semester. Liam will work on a project titled “Investigating the Influence of Convective Severe Weather on Ozone Pollution in Oklahoma City”.

Congratulations, Liam!

Upcoming presentations at AGU24 Annual Meeting

We have multiple presentations at AGU24 Annual Meeting (https://www.agu.org/annual-meeting) in Washington, D.C., December 9-13, 2024:

B11I-1442 The Global Hydrogen Budget

Presenter: Zutao Ouyang. 08:30-12:20, Monday, Dec 9, 2024. Hall B-C (Poster Hall). https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1598982

A21K-1910 Examination of Meteorological Factors and Emissions Sources Leading to the Large Methane (CH4) Enhancements at the ARM Site in Oklahoma. [student-led presentation]

Presenter: Qingyu Wang. 08:30-12:20, Tuesday, Dec 10, 2024. Hall B-C (Poster Hall). https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1544297

A23E-2022 Investigating Compound Heat Wave and Fine Particulate Matter Pollution Events in Urban Areas. [student-led presentation]

Presenter: Jessica Leffel. 13:40-17:30, Tuesday, Dec 10, 2024. Hall B-C (Poster Hall). https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1545993

A23B-1969 Observation and Simulation of Methane (CH4) Plumes during the Morning Boundary Layer Transition.

Presenter: Xiao-Ming Hu. 13:40-17:30, Tuesday, Dec 10, 2024. Hall B-C (Poster Hall). https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1543991

A33L-06 Complex Interplay between Temperature and Air Pollution in U.S. Cities.

Presenter: Xueli Yang. 15:25-15:40, Wednesday, Dec 11, 2024. 152A. https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1610050

GC44A-03 Enhancing the Representation of Hydrological Processes in an Urban Canopy Model: A Multi-parameterization Approach. [student-led presentation]

Presenter: Yuqi Huang. 16:25-16:35, Thursday, Dec 12, 2024. Salon A. https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1591503

GC51F-02 Worldwide Scaling of Waste Generation in Urban Systems.

Presenter: Mingzhen Lu. 08:40-08:50, Friday, Dec 13, 2024. Salon A. https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1731134

GC51F-03 Characterizing Compound Heat and Ozone Pollution Episodes in U.S. Cities.

Presenter: Chenghao Wang. 08:50-09:00, Friday, Dec 13, 2024. Salon A. https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1602258

GC53N-01 Hydrometeorological Evaluation of a Continental-Scale Convection-Permitting Simulation Across Urban Environments. [student-led presentation]

Presenter: Liam Thompson. 14:10-14:20, Friday, Dec 13, 2024. Salon A. https://agu.confex.com/agu/agu24/meetingapp.cgi/Paper/1602473

Dr. Wang is also co-chairing the following sessions:

GC41I – Advancing Representation of Urban Processes and Dynamics in Models Across Scales I Poster. 08:30-12:20, Thursday, Dec 12, 2024. Hall B-C. https://agu.confex.com/agu/agu24/meetingapp.cgi/Session/225944

GC44A – Advancing Representation of Urban Processes and Dynamics in Models Across Scales II Oral. 16:00-17:30, Thursday, Dec 12, 2024. Salon A. https://agu.confex.com/agu/agu24/meetingapp.cgi/Session/233418

Liam Thompson won first place in the GIS Day Undergraduate Poster Competition

Liam Thompson recently won first place in the GIS Day Undergraduate Poster Competition. He presented his work on continental-scale evaluation of convection-permitting hydroclimate simulation in urban areas.

The annual GIS Day at the University of Oklahoma is hosted by Center for Spatial Analysis. This event celebrates students and professionals in the broad geospatial community. It also hosts the student poster and StoryMap competition, an exposition designed to help students foster their professional development by presenting their research to both faculty and GIS professionals.

Congratulations, Liam!

New paper on Andean snow cover published in Scientific Reports

Our new paper, “Rapid decline in extratropical Andean snow cover driven by the poleward migration of the Southern Hemisphere westerlies“, is published in Scientific Reports (IF: 3.8).

The paper can be downloaded at https://www.nature.com/articles/s41598-024-78014-0.

Authors: Raúl R. Cordero, Sarah Feron, Alessandro Damiani, Shelley MacDonell, Jorge Carrasco, Jaime Pizarro, Cyrus Karas, Jose Jorquera, Edgardo Sepulveda, Fernanda Cabello, Francisco Fernandoy, Chenghao Wang, Alia L. Khan, & Gino Casassa

Abstract: Seasonal snow in the extratropical Andes is a primary water source for major rivers supplying water for drinking, agriculture, and hydroelectric power in Central Chile. Here, we used estimates from the Moderate Resolution Imaging Spectroradiometer (MODIS) to analyze changes in snow cover extent over the period 2001–2022 in a total of 18 watersheds spanning approximately 1,100 km across the Chilean Andes (27–36°S). We found that the annual snow cover extent is receding in the watersheds analyzed at an average pace of approximately 19% per decade. These alarming trends have impacted meltwater runoff, resulting in historically low river streamflows during the dry season. We examined streamflow records dating back to the early 1980s for 10 major rivers within our study area. Further comparisons with large-scale climate modes suggest that the detected decreasing trends in snow cover extent are likely driven by the poleward migration of the westerly winds associated with a positive trend in the Southern Annular Mode (SAM).

DOI: https://doi.org/10.1038/s41598-024-78014-0

Fig. 1. The snow cover extent is rapidly declining in the extratropical Andes. (a) Trend in the annual snow cover extent of 18 watersheds in Central Chile (from latitude 27°S to 36°S), computed from MODIS-derived estimates over the period 2001–2022. (b) Changes in snow cover extent from 2001–2012 to 2013–2022 in 18 watersheds in Central Chile. (c) Annual snow cover extent relative to the 2001–2020 mean. The watersheds in (a) were grouped into three regions based on latitude: 27–31°S, 31–34°S, and 34–36°S.

New paper on urban land surface model intercomparison published in Journal of Advances in Modeling Earth Systems

Our new paper, “The water balance representation in Urban-PLUMBER land surface models“, is published in Journal of Advances in Modeling Earth Systems (IF: 4.4).

The paper can be downloaded at https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2024MS004231.

Authors: H. J. Jongen, M. Lipson, A. J. Teuling, S. Grimmond, J.-J. Baik, M. Best, M. Demuzere, K. Fortuniak, Y. Huang, M. G. De Kauwe, R. Li, J. McNorton, N. Meili, K. Oleson, S.-B. Park, T. Sun, A. Tsiringakis, M. Varentsov, C. Wang, Z.-H. Wang, G. J. Steeneveld

Abstract: Urban Land Surface Models (ULSMs) simulate energy and water exchanges between the urban surface and atmosphere. However, earlier systematic ULSM comparison projects assessed the energy balance but ignored the water balance, which is coupled to the energy balance. Here, we analyze the water balance representation in 19 ULSMs participating in the Urban-PLUMBER project using results for 20 sites spread across a range of climates and urban form characteristics. As observations for most water fluxes are unavailable, we examine the water balance closure, flux timing, and magnitude with a score derived from seven indicators expecting better scoring models to capture the latent heat flux more accurately. We find that the water budget is only closed in 57% of the model-site combinations assuming closure when annual total incoming fluxes (precipitation and irrigation) are within 3% of the outgoing (all other) fluxes. Results show the timing is better captured than magnitude. No ULSM has passed all water balance indicators for any site. Models passing more indicators do not capture the latent heat flux more accurately refuting our hypothesis. While output reporting inconsistencies may have negatively affected model performance, our results indicate models could be improved by explicitly verifying water balance closure and revising runoff parameterizations. By expanding ULSM evaluation to the water balance and related to latent heat flux performance, we demonstrate the benefits of evaluating processes with direct feedback mechanisms to the processes of interest.

DOI: https://doi.org/10.1029/2024MS004231

Figure 8. Coefficient of determination (R2)
between (half-)hourly explicit and implicit water storage change by model and site. Green indicates the 0.9 IS,t threshold. Missing results are shown as white (i.e., cannot calculate explicit or implicit water storage change).

New paper on climate change in South America published in Communications Earth & Environment

Our new paper, “South America is becoming warmer, drier, and more flammable“, is published in Communications Earth & Environment (IF: 8.1).

The paper can be downloaded at https://www.nature.com/articles/s43247-024-01654-7.

Authors: Sarah Feron, Raúl R. Cordero, Alessandro Damiani, Shelley MacDonell, Jaime Pizarro, Katerina Goubanova, Raúl Valenzuela, Chenghao Wang, Lena Rester, Anne Beaulieu

Abstract: South America is experiencing severe impacts from climate change. Although the warming of the subcontinent closely follows the global path, the rise of temperatures has been more pronounced in some regions, which have also seen a parallel increment in the occurrence of droughts and weather conditions associated with enhanced fire risk. Here, we use reanalysis datasets to analyze the progression of the concurring warm, dry, and high fire risk conditions (i.e., dry compounds) since 1971. We show that the frequency of these compound extremes has surged in key South American regions including the northern Amazon, which have seen a 3-fold increase in the number of days per year with extreme fire weather conditions (including high temperatures, dryness, and low humidity). Our results also suggest that the surface temperature of the tropical Pacific Ocean modulates the interannual variability of dry compounds in South America. While El Niño enhances the fire risk in the northern Amazon, dry extremes in the Gran Chaco region appear to be more responsive to La Niña.

DOI: https://doi.org/10.1038/s43247-024-01654-7

Fig. 3: Dry compound extremes exhibit different regional and seasonal trends. Changes from 1971–2000 to 2001–2022 in the number of days per season with concurring warm, dry, and flammable conditions (i.e., dry compound days). The following meteorological seasons were considered: (a) December-January-February (DJF), (b) March-April-May (MAM), (c) June-July-August (JJA), and (d) September-October- November (SON). The number of dry compound days per season was derived (see “Methods”) from daily estimates from the ERA5 dataset over the period 1971–2022.

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