Local hourly trends in near-surface and land surface temperatures

Essential Climate Variables, such as near-surface (T2m) and land surface temperatures (LST), are typically reported in Coordinated Universal Time (UTC) for global consistency. However, their diurnal variability leads to temperature trends that differ by the local hour, a factor not analyzed on the global nor regional scale. Using ECMWF ERA5-Land reanalysis data (1981-2022), we assess temperature trends by local hour and month. Our results show that the trends can change significantly during the day. LST and T2m warming or cooling trends peak in the afternoon, while showing large spatial variability across both hemispheres. Using MODIS observations, we show how the nominal Equator crossing times of TERRA and AQUA influence LST trends. These findings highlight the necessity of accounting for local time in climate assessments to improve adaptation strategies.

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Publication Details

Journal
Scientific Reports
Published
2025-08-15
DOI
https://doi.org/10.1038/s41598-025-15731-0
Citations
2
Primary Topic
Urban Heat Island Mitigation
Type
article
Field-Weighted Citation Impact
1.60

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article

Local hourly trends in near-surface and land surface temperatures

Jean‐Noël Thépaut, Sarah Safieddine, Joaquı́n Muñoz-Sabater, Cathy Clerbaux
2 citations
Scientific Reports
Urban Heat Island Mitigation
1.60
article

Local hourly trends in near-surface and land surface temperatures

Jean‐Noël Thépaut, Sarah Safieddine, Joaquı́n Muñoz-Sabater, Cathy Clerbaux
article en
2 citations

Abstract

Essential Climate Variables, such as near-surface (T2m) and land surface temperatures (LST), are typically reported in Coordinated Universal Time (UTC) for global consistency. However, their diurnal variability leads to temperature trends that differ by the local hour, a factor not analyzed on the global nor regional scale. Using ECMWF ERA5-Land reanalysis data (1981-2022), we assess temperature trends by local hour and month. Our results show that the trends can change significantly during the day. LST and T2m warming or cooling trends peak in the afternoon, while showing large spatial variability across both hemispheres. Using MODIS observations, we show how the nominal Equator crossing times of TERRA and AQUA influence LST trends. These findings highlight the necessity of accounting for local time in climate assessments to improve adaptation strategies.

Scientific ReportsVol. 15(1)
Centre National de la Recherche Scientifique (FR), European Centre for Medium-Range Weather Forecasts (GB), Université de Versailles Saint-Quentin-en-Yvelines (FR), Sorbonne Université (FR), Institut Pierre-Simon Laplace (FR), Laboratoire atmosphères, milieux, observations spatiales (FR)
European Commission, European Organization for the Exploitation of Meteorological Satellites, Goddard Space Flight Center, HORIZON EUROPE European Research Council
Climate action
Openalex Percentile: Top 16%
Urban Heat Island Mitigation
1.60
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Local hourly trends in near-surface and land surface temperatures — Jean‐Noël Thépaut, Sarah Safieddine, et al. · Scientific Reports (2025) | TGRS Research Map | TGRS