New high-resolution estimates of the permafrost thermal state and hydrothermal conditions over the Northern Hemisphere
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Published:2022-02-24
Issue:2
Volume:14
Page:865-884
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ISSN:1866-3516
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Container-title:Earth System Science Data
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language:en
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Short-container-title:Earth Syst. Sci. Data
Author:
Ran YouhuaORCID, Li Xin, Cheng GuodongORCID, Che Jingxin, Aalto Juha, Karjalainen OlliORCID, Hjort JanORCID, Luoto MiskaORCID, Jin Huijun, Obu JaroslavORCID, Hori Masahiro, Yu QihaoORCID, Chang Xiaoli
Abstract
Abstract. Monitoring the thermal state of permafrost (TSP) is
important in many environmental science and engineering applications.
However, such data are generally unavailable, mainly due to the lack of
ground observations and the uncertainty of traditional physical models. This
study produces novel permafrost datasets for the Northern Hemisphere (NH),
including predictions of the mean annual ground temperature (MAGT) at the
depth of zero annual amplitude (DZAA) (approximately 3 to 25 m) and active
layer thickness (ALT) with 1 km resolution for the period of 2000–2016, as
well as estimates of the probability of permafrost occurrence and permafrost
zonation based on hydrothermal conditions. These datasets integrate
unprecedentedly large amounts of field data (1002 boreholes for MAGT and
452 sites for ALT) and multisource geospatial data, especially remote
sensing data, using statistical learning modeling with an ensemble
strategy. Thus, the resulting data are more accurate than those of previous
circumpolar maps (bias = 0.02±0.16 ∘C and RMSE = 1.32±0.13 ∘C for MAGT; bias = 2.71±16.46 cm and
RMSE = 86.93±19.61 cm for ALT). The datasets suggest that the areal
extent of permafrost (MAGT ≤0 ∘C) in the NH, excluding
glaciers and lakes, is approximately 14.77 (13.60–18.97) × 106 km2 and that the areal extent of permafrost regions (permafrost
probability >0) is approximately 19.82×106 km2. The areal fractions of humid, semiarid/subhumid, and arid permafrost regions are 51.56 %, 45.07 %, and 3.37 %, respectively. The
areal fractions of cold (≤-3.0 ∘C), cool (−3.0 ∘C
to −1.5 ∘C), and warm (>-1.5 ∘C)
permafrost regions are 37.80 %, 14.30 %, and 47.90 %, respectively.
These new datasets based on the most comprehensive field data to date
contribute to an updated understanding of the thermal state and zonation of
permafrost in the NH. The datasets are potentially useful for various
fields, such as climatology, hydrology, ecology, agriculture, public health,
and engineering planning. All of the datasets are published through the
National Tibetan Plateau Data Center (TPDC), and the link is https://doi.org/10.11888/Geocry.tpdc.271190 (Ran et al.,
2021a).
Funder
Chinese Academy of Sciences National Natural Science Foundation of China Academy of Finland
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences
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