2020
DOI: 10.1016/j.accre.2020.09.003
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Projected drought conditions in Northwest China with CMIP6 models under combined SSPs and RCPs for 2015–2099

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Cited by 134 publications
(47 citation statements)
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“…The precipitation of wettest quarter, which contributed 11.6%, was another important variable to explain the distribution of H. japonica, and subclass of soil, which contributed 9.7%, was another important variable. However, under the SSP 245 and SSP 585 climate change scenarios, total annual precipitation is expected to increase slightly at a rate of 6.4 and 8.0 mm per decade, according to studies conducted by Li et al [35]. Therefore, according to our experimental results, part of the reason why the suitable distribution area of H. japonica does not change significantly in the future under the two scenarios can be explained.…”
Section: Discussionsupporting
confidence: 61%
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“…The precipitation of wettest quarter, which contributed 11.6%, was another important variable to explain the distribution of H. japonica, and subclass of soil, which contributed 9.7%, was another important variable. However, under the SSP 245 and SSP 585 climate change scenarios, total annual precipitation is expected to increase slightly at a rate of 6.4 and 8.0 mm per decade, according to studies conducted by Li et al [35]. Therefore, according to our experimental results, part of the reason why the suitable distribution area of H. japonica does not change significantly in the future under the two scenarios can be explained.…”
Section: Discussionsupporting
confidence: 61%
“…In the climate prediction experiment, the shared socioeconomic paths (SSPs) and representative concentration paths (RCP) were considered, and two scenarios SSP 2-RCP 4.5 (SSP 245) and SSP 5-RCP 8.5 (SSP 585) were selected for simulation. SSP 245 is the updated scenario of RCP 4.5, which uses a moderate development path, represents an intermediate level of greenhouse gas emissions and a nominal 4.5 Wm −2 radioactive forcing level by 2100 [35]; while, SSP 585 is the updated scenario of RCP 8.5, which uses the development path dominated by fossil fuels, represents a high level of greenhouse gas emissions and a nominal 8.5 Wm −2 radioactive forcing level by 2100 [36]. Additionally, soil factors have also been shown to be important factors affecting species distribution [37].…”
Section: Variablesmentioning
confidence: 99%
“…The duration, severity, and intensity increase with the increasing greenhouse gas emission in the future period. The mean drought duration and severity are longer and severe under the high emission scenario SSP585, which is reported by (Li et al 2020). The frequency of drought occurrences under SSP245 (17.5%) is slightly higher than SSP126 (16.6%) and SSP585 (16.8%) scenarios.…”
Section: Discussionmentioning
confidence: 65%
“…Meanwhile, their potential influences on the social and economic development may be amplified (Chen and Sun, 2019). Following the launch of CMIP6 by the World Climate Research Programme (WCRP), Northwest China will become drier during 2015–2099 under SSP1‐2.6, SSP2‐4.5 and SSP5‐8.5 (Li et al ., 2020). However, limited studies have been conducted on the drought assessments and its impact over China (taking into consideration the whole territory and its distinct climatic zones) using the up‐to‐date simulation data.…”
Section: Introductionmentioning
confidence: 99%