Articles | Volume 17, issue 9
https://doi.org/10.5194/essd-17-4985-2025
https://doi.org/10.5194/essd-17-4985-2025
Data description article
 | 
29 Sep 2025
Data description article |  | 29 Sep 2025

Updates to C-LSAT 2.1 and the development of high-resolution land surface air temperature and diurnal temperature range datasets

Sihao Wei, Qingxiang Li, Qiya Xu, Zichen Li, Hanyu Zhang, and Jiaxue Lin

Related authors

An AI-Driven Reconstruction of Global Surface Temperature with Emphasis on Refining the Antarctic Record
Chenxi Ouyang, Qingxiang Li, Zichen Li, and Sihao Wei
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-717,https://doi.org/10.5194/essd-2025-717, 2026
Preprint under review for ESSD
Short summary

Cited articles

Beck, H. E., Zimmermann, N. E., McVicar, T. R., Vergopolan, N., Berg, A., and Wood, E. F.: Present and future Köppen-Geiger climate classification maps at 1 km resolution, Sci. Data, 5, 180214, https://doi.org/10.1038/sdata.2018.214, 2018. 
Caesar, J., Alexander, L., and Vose, R.: Large-scale changes in observed daily maximum and minimum temperatures: Creation and analysis of a new gridded data set, J. Geophys. Res.-Atmos., 111, https://doi.org/10.1029/2005JD006280, 2006. 
Cheng, J., Li, Q., Chao, L., Maity, S., Huang, B., and Jones, P.: Development of High Resolution and Homogenized Gridded Land Surface Air Temperature Data: A Case Study Over Pan-East Asia, Front. Environ. Sci., 8, https://doi.org/10.3389/fenvs.2020.588570, 2020. 
Cressie, N.: The origins of kriging, Math. Geol., 22, 239–252, https://doi.org/10.1007/BF00889887, 1990. 
Daly, C., Neilson, R. P., and Phillips, D. L.: A Statistical-Topographic Model for Mapping Climatological Precipitation over Mountainous Terrain, J. Appl. Meteorol. Clim., 33, 140–158, https://doi.org/10.1175/1520-0450(1994)033<0140:ASTMFM>2.0.CO;2, 1994. 
Download
Short summary
This study introduces the update to the C-LSAT 2.1 station data and its gridded dataset (5° × 5°) for 1850–2024, into which nearly 3000 additional stations were merged. Building on this, high‑resolution (0.5° × 0.5°) land surface air temperature (C‑LSAT HRv1) and diurnal temperature range (C‑LDTR HRv1) datasets for 1901–2023 were produced via thin-plate spline interpolation of the climatology fields and adjusted inverse distance weighted interpolation of the anomaly fields.
Share
Altmetrics
Final-revised paper
Preprint