Taihua Wang
Biographic Data
| ID | 7994350 |
|---|---|
| NAME | Taihua Wang |
| GIVEN NAMES | Taihua |
| FAMILY NAME | Wang |
| SIGNATURE | WANG T |
| AFFILIATIONS | Tsinghua University |
| ORCID | 0000-0002-1620-5495 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2021 |
| LATEST PUBLICATION YEAR | 2023 |
| H-INDEX | 0 |
Divergent responses of permafrost degradation to precipitation increases at different seasons on the eastern Qinghai–Tibet Plateau based on modeling approach
The Qinghai–Tibet Plateau (QTP) has responded to remarkable climate warming with dramatic permafrost degradation over the past few decades. Previous studies have mostly focused on permafrost responses to rising air temperature, while the effects of accompanying increases in precipitation remain contentious and largely unknown. In this study, a distributed process-based model was applied to quantify the impacts of increased precipitation on permaf…
Seasonal characteristics and spatio-temporal variations of the extreme precipitation-air temperature relationship across China
It is assumed that extreme precipitation (P) increases with air temperature (T) by a scaling rate close to 7%/°C without moisture limitation according to the Clausius-Clapeyron (C-C) relationship. However, the spatial distribution of the P-T relationship in China is subject to divergent conclusions including both sub-C-C ( 7%/°C) scaling with reasons yet to be examined. Based on the long-term observations, here we show that P-T relationships with…
Overestimated global dryland expansion with substantial increases in vegetation productivity under climate warming
Drylands are serviced as an essential component of the earth’s ecosystem. The potential changes in dryland areas are of great importance to the environment, but various debates remain as to whether and to what extent drylands are expected to expand. Here we employ a physically-based potential evapotranspiration ( E P ) model accounting for vegetation response to climate change to quantify potential changes in dryland areas, on the basis of a comm…
Linkage between anomalies of pre-summer thawing of frozen soil over the Tibetan Plateau and summer precipitation in East Asia
The Tibetan Plateau (TP) is sensitive to climate change in the land–atmosphere coupling mechanism due to its complex topographic features and unique geographic location. This study explored the teleconnection between pre-summer thawing of frozen soil over the TP and summer precipitation in East Asia in the Meiyu–Baiu rainy season (June, July) from 1981 to 2019 using maximum covariance analysis (MCA). The precipitation fields forced by thawing of …
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Linkage between anomalies of pre-summer thawing of frozen soil over the Tibetan Plateau and summer precipitation in East Asia
The Tibetan Plateau (TP) is sensitive to climate change in the land–atmosphere coupling mechanism due to its complex topographic features and unique geographic location. This study explored the teleconnection between pre-summer thawing of frozen soil over the TP and summer precipitation in East Asia in the Meiyu–Baiu rainy season (June, July) from 1981 to 2019 using maximum covariance analysis (MCA). The precipitation fields forced by thawing of …
Divergent responses of permafrost degradation to precipitation increases at different seasons on the eastern Qinghai–Tibet Plateau based on modeling approach
The Qinghai–Tibet Plateau (QTP) has responded to remarkable climate warming with dramatic permafrost degradation over the past few decades. Previous studies have mostly focused on permafrost responses to rising air temperature, while the effects of accompanying increases in precipitation remain contentious and largely unknown. In this study, a distributed process-based model was applied to quantify the impacts of increased precipitation on permaf…
Seasonal characteristics and spatio-temporal variations of the extreme precipitation-air temperature relationship across China
It is assumed that extreme precipitation (P) increases with air temperature (T) by a scaling rate close to 7%/°C without moisture limitation according to the Clausius-Clapeyron (C-C) relationship. However, the spatial distribution of the P-T relationship in China is subject to divergent conclusions including both sub-C-C ( 7%/°C) scaling with reasons yet to be examined. Based on the long-term observations, here we show that P-T relationships with…
Overestimated global dryland expansion with substantial increases in vegetation productivity under climate warming
Drylands are serviced as an essential component of the earth’s ecosystem. The potential changes in dryland areas are of great importance to the environment, but various debates remain as to whether and to what extent drylands are expected to expand. Here we employ a physically-based potential evapotranspiration ( E P ) model accounting for vegetation response to climate change to quantify potential changes in dryland areas, on the basis of a comm…
Atmospheric sciences (4 works) · Climatology (4 works) · Environmental Science (4 works) · Geography (4 works) · Geology (4 works) · Meteorology (4 works) · Precipitation (4 works) · Climate variability and models (3 works) · China (2 works) · Climate change (2 works)