2017
DOI: 10.1007/s00382-017-3622-0
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Assessment of the quality of NCEP-2 and CFSR reanalysis daily temperature in China based on long-range correlation

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Cited by 38 publications
(19 citation statements)
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“…The precipitation data (daily average) was collected from the CHIRPS (Climate Hazard Infrared Precipitation with Stations) database, which provides a high resolution (0.05°) dataset with integrated global climatology, satellite estimates, and rain gauge observations ( Funk et al., 2015 ). The daily temperature data for the study area was collected from National Centres for Environmental Prediction’s Climate Forecast System Realanalysis (CFSR), which provides 3 rd generation real analysis data at high resolution ( He and Zhao, 2018 ). The predominant wind direction in the study area was south and south-western and the average wind speed varied between 3 and 4 ms −1 .…”
Section: Methodsmentioning
confidence: 99%
“…The precipitation data (daily average) was collected from the CHIRPS (Climate Hazard Infrared Precipitation with Stations) database, which provides a high resolution (0.05°) dataset with integrated global climatology, satellite estimates, and rain gauge observations ( Funk et al., 2015 ). The daily temperature data for the study area was collected from National Centres for Environmental Prediction’s Climate Forecast System Realanalysis (CFSR), which provides 3 rd generation real analysis data at high resolution ( He and Zhao, 2018 ). The predominant wind direction in the study area was south and south-western and the average wind speed varied between 3 and 4 ms −1 .…”
Section: Methodsmentioning
confidence: 99%
“…The reliability of various reanalysis data is relatively low (e.g., [19,20]). Observational data recorded at meteorological stations are fundamental to the data processing and analysis that underpins climate research.…”
Section: Introductionmentioning
confidence: 99%
“…In recent years, state‐of‐the‐art dynamic models have been used for operational rainfall prediction (Kang et al, ; Liu et al, ; Gong et al, ). The performances of such models have shown significant progresses; however, limitations of dynamic rainfall prediction still exist (Li and Chou, ; He and Zhao, ). The reason may be that the summer rainfall in China involves several complex atmospheric processes, for example, the low‐latitude Indian summer monsoon (Huang et al, ), the East Asian summer monsoon (EASM; Ding and Chan, ), and the western North Pacific (WNP) subtropical high (Zhou et al, ), and the dynamic models have difficulties in reproducing the complex interactions among these processes.…”
Section: Introductionmentioning
confidence: 99%