Consistent Ground Surface Temperature Climatology Over China: 1956-2022
文献类型：期刊论文
| 作者 | Wang, Shengdi4; Cao, Bin; Hao, Jiansheng3; Sun, Wen; Zhang, Kun2 |
| 刊名 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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| 出版日期 | 2024-05-28 |
| 卷号 | 129期号:10页码:e2024JD040916 |
| DOI | 10.1029/2024JD040916 |
| 产权排序 | 3 |
| 文献子类 | Article |
| 英文摘要 | The ground surface represents the land-atmosphere interface and plays a crucial role in exchanging energy, matter, and biochemical fluxes. The ground surface temperature (Ts) is hence widely investigated as an indicator to understand the thermal state of soil in a warming world. However, regular and continuous Ts measurements are rare worldwide, and the early Ts records were derived from snow surface measurements and are not comparable with the measurements of modern automatic systems. In this study, we reconstruct the Ts records of the China Meteorological Administration (CMA) for 1956-2022 by numerical simulation. The results show that the mean annual ground surface temperature (MAGST) during 1981-2010 ranged from 0.4 to 30.8 degrees C at 632 stations. The MAGST was mainly controlled by air temperature and refined by snow depth. The overall MAGST increased by 0.20 +/- 0.02 degrees C dec-1 across China during 1956-2022 and showed pronounced interdecadal variability corresponding to the surface air temperature (0.23 +/- 0.03 degrees C dec-1). At the snow-covered sites, the Ts warming was amplified by increased snow depth, leading to about 0.24 degrees C dec-1 (or 70.6%) faster warming for Ts in winter compared to that of surface air temperature. Many of the early reported ground surface temperature studies based on CMA measurements did not consider the measurement inconsistency and likely overestimated the warming trend of ground surface temperature over China. Ground surface temperature (Ts) affects a variety of temperature-related phenomena on the Earth's surface and is hence widely investigated as an indicator to understand the interaction of land-atmosphere in a warming climate. However, continuous Ts measurements are rare worldwide. Restricted by the early measurement conditions, the early Ts records were recorded manually from the snow surface, and are not comparable with the measurements of the modern automatic systems. Therefore, we reconstructed a Ts time series for the China Meteorological Administration (CMA) data for 1956-2022 by numerical simulation. Our results show that the mean annual ground surface temperature (MAGST) increased by 0.20 degrees C dec-1 across China during 1956-2022. The MAGST was mainly controlled by air temperature and refined by snow depth. Ts warming was amplified by about 0.24 degrees C dec-1 (or 70.6%) in winter by increased snow depth since 1970, compared to the surface air temperature. Many of the early reported Ts studies based on CMA measurements did not consider the measurement inconsistency and likely overestimated the warming trend of Ts over China. Continuous ground surface temperature data for China were estimated by filling the gaps arising from the inconsistent measurement systems The overall mean annual ground surface temperature increased by 0.20 +/- 0.02 degrees C dec-1 across China during 1956-2022 Ground surface temperature warming was amplified by about 0.24 degrees C dec-1 (or 70.6%) in winter since 1970 due to increased snow depth |
| WOS关键词 | AIR-TEMPERATURE ; SOIL-TEMPERATURE ; THERMAL REGIME ; LONG-TERM ; PERMAFROST ; MODEL ; EVAPORATION ; DATASET ; URBANIZATION ; REANALYSIS |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| WOS记录号 | WOS:001226340700001 |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/205157]  |
| 专题 | 陆地表层格局与模拟院重点实验室_外文论文 |
| 通讯作者 | Hao, Jiansheng |
| 作者单位 | 1.Sun Yat sen Univ, Sch Geospatial Engn & Sci, Zhuhai, Peoples R China 2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing, Peoples R China 3.Lanzhou Univ, Coll Earth & Environm Sci, Key Lab Western Chinas Environm Syst, Minist Educ, Lanzhou, Peoples R China 4.Chinese Acad Sci, Inst Tibetan Plateau Res, Natl Tibetan Plateau Data Ctr, Key Lab Tibetan Plateau Earth Syst Sci Environm &, Beijing, Peoples R China |
| 推荐引用方式 GB/T 7714 | Wang, Shengdi,Cao, Bin,Hao, Jiansheng,et al. Consistent Ground Surface Temperature Climatology Over China: 1956-2022[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2024,129(10):e2024JD040916. |
| APA | Wang, Shengdi,Cao, Bin,Hao, Jiansheng,Sun, Wen,&Zhang, Kun.(2024).Consistent Ground Surface Temperature Climatology Over China: 1956-2022.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,129(10),e2024JD040916. |
| MLA | Wang, Shengdi,et al."Consistent Ground Surface Temperature Climatology Over China: 1956-2022".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 129.10(2024):e2024JD040916. |
入库方式： OAI收割
来源：地理科学与资源研究所
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