WENHONG LI

Prof. WENHONG LI

Duke University, Durham, California, USA
orcid

Research Focus & Metrics

Academic Career Length

16Years (2011-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 March 2011 in Journal of Climate
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WENHONG LIWENHONG LI
WENHONG LI
LLLaifang Li
Laifang Li
RFRong Fu
Rong Fu
YDYi Deng
Yi Deng
HWHui Wang
Hui Wang
This study investigates the changes of the North Atlantic subtropical high (NASH) and its impact on summer precipitation over the southeastern (SE) United States using the 850-hPa geopotential height field in the National Centers for Environmental Prediction (NCEP) reanalysis, the 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40), long-term rainfall data, and Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4) model simulations during the past six decades (1948–2007). The results show that the NASH in the last 30 yr has become more intense, and its western ridge has displaced westward with an enhanced meridional movement compared to the previous 30 yr. When the NASH moved closer to the continental United States in the three most recent decades, the effect of the NASH on the interannual variation of SE U.S. precipitation is enhanced through the ridge’s north–south movement. The study’s attribution analysis suggested that the changes of the NASH are mainly due to anthropogenic warming. In the twenty-first century with an increase of the atmospheric CO2 concentration, the center of the NASH would be intensified and the western ridge of the NASH would shift farther westward. These changes would increase the likelihood of both strong anomalously wet and dry summers over the SE United States in the future, as suggested by the IPCC AR4 models.

5 December 2019 in WIREs Water
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GHGebremedhin Gebremeskel Gebremeskel Haile
Gebremedhin Gebremeskel Gebremeskel Haile
Qiuhong TangQiuhong Tang
Qiuhong Tang
WENHONG LIWENHONG LI
WENHONG LI
Xingcai LiuXingcai Liu
Xingcai Liu
XZXuejun Zhang
Xuejun Zhang

30 September 2012 in Nature Geoscience
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WENHONG LIWENHONG LI
WENHONG LI
LLLaifang Li
Laifang Li
MTMingfang Ting
Mingfang Ting
YLYimin Liu
Yimin Liu

15 October 2011 in Climate Dynamics
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LLLaifang Li
Laifang Li
WENHONG LIWENHONG LI
WENHONG LI
YKYochanan Kushnir
Yochanan Kushnir

22 September 2018 in Water Resources Research
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LHLu Hao
Lu Hao
XHXiaolin Huang
Xiaolin Huang
QMQin mengsheng
Qin mengsheng
YLYongqiang Liu
Yongqiang Liu
WENHONG LIWENHONG LI
WENHONG LI
Ge SunGe Sun
Ge Sun
Conversion of agricultural lands to urban uses affects regional and global climate not only through the release of greenhouse gases but also through altering land surface physical processes such as energy and water balances. Most existing studies on the meteorological impacts of urbanization focus on urban heat island effects with little attention on its impacts of atmospheric humidity, a key variable in hydrometeorology and climate science. We define the influences of urbanization on reducing atmospheric humidity and elevating vapor pressure deficit as urban dry island (UDI) effects. We conduct a case study in the Yangtze River Delta, a typical humid area in southern China that is under rapid urbanization. We examine spatiotemporal characteristics of UDI and identify potential drivers during 2001–2014. Relationships and interactions between variations of air temperature, atmospheric humidity, evapotranspiration, and leaf area index of different land cover were determined using correlation and attribution analyses at both station and regional levels. We show that atmospheric humidity decreased dramatically and vapor pressure deficit increased sharply in the urban core, resulting in enhanced UDI. In addition to global warming and localized urban heat island, UDI is closely related to the loss of vegetation cover (i.e., natural wetlands and paddies). Reduction of evapotranspiration or latent heat is another important factor contributing to UDI effects. We conclude that the role of vegetated land cover and associated ecohydrological processes in moderating UDI and maintaining a stable climate and environment should be considered in massive urban planning and global change impact assessment in southern China.

23 September 2023 in npj Climate and Atmospheric Science
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LHLu Hao
Lu Hao
Ge SunGe Sun
Ge Sun
XHXiaolin Huang
Xiaolin Huang
RTRun Tang
Run Tang
KJKailun Jin
Kailun Jin
WENHONG LIWENHONG LI
WENHONG LI
‘Urban Dry (Wet) Islands’ (UDI/UWI) represents microclimate change that impacts ecosystems and human well-being. However, causes of the UDI (UWI) phenomena are not fully understood due to the lack of empirical data. Here, we quantify UDI (UWI) using global observations of atmospheric humidity, evapotranspiration (ET), and land surface characteristics across 25 large urban agglomerations. We show that UDI (17) and UWI (8) are closely tied to local ET, global warming, and ‘Urban Heat Islands’ through intertwined linkages with water and energy balances. UDI is most pronounced in humid vegetated regions where mean urban-rural annual ET differences are as high as 215 mm, whereas UWI is found in arid regions or in climates with dry summers. We conclude that ET can be used as a single variable to explain emerging urban environmental changes. Our study supports a concerted strategy of restoring nature’s ET power as effective ‘Nature-based Solutions’ to mitigate the negative environmental effects of urbanization.