Projections of Global Drought and Their Climate Drivers Using CMIP6 . . . In addition to considering the influence of evapotranspiration on drought, Based on three GCMs from CMIP6 forced with SSP585, we used the daily SPEI Z X Assessment of GCMs simulation performance for precipitation and temperature from CMIP5 to CMIP6 over the Tibetan Plateau Int J Climatol 2021, 41, 3994–4018 [Google Scholar
Frontiers | Impact of climate change on the long-term water balance in . . . On the Tibetan Plateau, the soil water content is reduced by 22%–34% at 0–80 cm depth, resulting in moderately and even severely degraded vegetation (Pan et al , 2017) Our predictions indicate that the soil water content in the upper reaches of the YZB will decrease by more than 20% under the high emission scenarios of CMIP5 and CMIP6
Evaluation and Correction of Climate Simulations for the Tibetan . . . - MDPI This study evaluates the abilities of fifteen High-resolution Coupled Model Intercomparison Project phase 6 (CMIP6) models to simulate temperature and precipitation over the Tibetan Plateau (TP) for the years 1980–2014 The impacts of terrain correction and Empirical Orthogonal Function (EOF) correction on simulations of temperature and precipitation are examined The results show that equal
Predicting Future Lake Water Storage Changes on the Tibetan Plateau . . . The variation of lake water storage is an important indicator for studying both climate change and ecological environment changes Previous studies have mainly focused on the lake storage changes in recent decades, and predicting future lake storage changes on the Tibetan Plateau under climate change scenarios remains a crucial gap We addressed this gap by establishing prediction models for
Assessment of CMIP6 Model Performance for Wind Speed in China The spatial bias between the historical and ssp585 simulations from CESM2-WACCM, NorESM2-MM, and HadGEM3-GC31-MM in China is shown in Figure 6 The wind speed projected by the three models shows an upward trend of wind speed in western China in the future, especially over the Tibetan Plateau and Xinjiang
CMIP6 Simulation-Based Daily Surface Air Temperature and . . . - MDPI The Qinghai-Tibetan Plateau (QTP), the source of many major Asian rivers, is sensitive to climate change, affecting billions of people’s livelihoods across Asia Here, we developed high-resolution projections of precipitation and daily maximum minimum temperatures at 0 1° spatial resolution over the QTP The projections are based on the output from seven global climate models (GCMs) from
Prediction of Future Spatial and Temporal Evolution Trends of Reference . . . Reference evapotranspiration (ET0) is an integral part of the regional hydrological cycle and energy balance and is extremely sensitive to climate change Based on temperature data from 24 global climate models (GCMs) in the Coupled Model Intercomparison Project Phase 6 (CMIP6), this study developed a multi-model ensemble based on delta statistical downscaling with multiple interpolation