Articles | Volume 17, issue 12
https://doi.org/10.5194/tc-17-5007-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-17-5007-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evaluation of snow cover properties in ERA5 and ERA5-Land with several satellite-based datasets in the Northern Hemisphere in spring 1982–2018
Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland
Kari Luojus
Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland
Aku Riihelä
Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland
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16 citations as recorded by crossref.
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- Characteristics of the spatiotemporal differences in snowmelt phenology in the Northern Hemisphere X. Li & H. Fan 10.1016/j.ejrh.2025.102358
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- Modeling climate change effects on river ice thickness in the Northern Hemisphere Y. Lin et al. 10.1016/j.jhydrol.2025.133268
- Quality of Snow Cover Characteristics Derived from ERA5-Land Reanalysis for Perm Krai A. Kryuchkov et al. 10.1134/S0001433824701251
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13 citations as recorded by crossref.
- Structural Similarity-Guided Siamese U-Net Model for Detecting Changes in Snow Water Equivalent K. Malik & C. Robertson 10.3390/rs17091631
- Demystifying the drivers of the spring warming asymmetry between Eurasia and North America X. Ding et al. 10.1126/sciadv.adu2364
- Impact of climate change on spatiotemporal patterns of snow hydrology: Conceptual frameworks, machine learning versus nested model M. Besharatifar & M. Nasseri 10.1016/j.pce.2024.103691
- A New Method to Simulate the Microwave Effective Snow Grain Size in the Northern Hemisphere Without Using Snow Depth Priors J. Yang et al. 10.1109/JSTARS.2024.3441817
- Snow Cover Variability and Trends over Karakoram, Western Himalaya and Kunlun Mountains During the MODIS Era (2001–2024) C. Almagioni et al. 10.3390/rs17050914
- Streamflow abrupt change and the driving factors in glacierized basins of Tarim Basin, Northwest China C. Yang et al. 10.1016/j.accre.2024.01.009
- Characteristics of the spatiotemporal differences in snowmelt phenology in the Northern Hemisphere X. Li & H. Fan 10.1016/j.ejrh.2025.102358
- Uneven global retreat of persistent mountain snow cover alongside mountain warming from ERA5-land M. Blau et al. 10.1038/s41612-024-00829-5
- Snow depth in high-resolution regional climate model simulations over southern Germany – suitable for extremes and impact-related research? B. Poschlod & A. Daloz 10.5194/tc-18-1959-2024
- Cross-Examination of Reanalysis Datasets on Elevation-Dependent Climate Change in the Third Pole Region A. Rameshan et al. 10.3390/atmos16030327
- Cumulative Changes in Minimum Snow/Ice Extent over Canada and Northern USA for 2000–2023 A. Trishchenko & C. Ungureanu 10.1080/07038992.2024.2371359
- Prominent impacts of snow–hydrological processes on near-surface temperature variability over Western Siberia N. Ganeshi et al. 10.1016/j.jhydrol.2025.133187
- Terrestrial ecosystems enhanced root zone water storage capacity in response to climate change over the past four decades Q. Xi et al. 10.1016/j.scib.2025.06.027
3 citations as recorded by crossref.
- Modeling climate change effects on river ice thickness in the Northern Hemisphere Y. Lin et al. 10.1016/j.jhydrol.2025.133268
- Quality of Snow Cover Characteristics Derived from ERA5-Land Reanalysis for Perm Krai A. Kryuchkov et al. 10.1134/S0001433824701251
- Forces for recent snow cover variation on the Mount Everest region D. Kattel & T. Yao 10.1007/s12040-024-02472-3
Latest update: 26 Jun 2025
Short summary
We evaluated snow cover properties in state-of-the-art reanalyses (ERA5 and ERA5-Land) with satellite-based datasets. Both ERA5 and ERA5-Land overestimate snow mass, whereas albedo estimates are more consistent between the datasets. Snow cover extent (SCE) is accurately described in ERA5-Land, while ERA5 shows larger SCE than the satellite-based datasets. The trends in snow mass, SCE, and albedo are mostly negative in 1982–2018, and the negative trends become more apparent when spring advances.
We evaluated snow cover properties in state-of-the-art reanalyses (ERA5 and ERA5-Land) with...