Snow depth estimation and historical data reconstruction over China based on a random forest machine learning approach
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Published:2020-06-03
Issue:6
Volume:14
Page:1763-1778
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ISSN:1994-0424
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Container-title:The Cryosphere
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language:en
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Short-container-title:The Cryosphere
Author:
Yang JianweiORCID, Jiang LingmeiORCID, Luojus KariORCID, Pan Jinmei, Lemmetyinen JuhaORCID, Takala Matias, Wu ShengliORCID
Abstract
Abstract. We investigated the potential capability of the random forest (RF)
machine learning (ML) model to estimate snow depth in this work. Four
combinations composed of critical predictor variables were used to train the
RF model. Then, we utilized three validation datasets from out-of-bag (OOB)
samples, a temporal subset, and a spatiotemporal subset to verify the fitted
RF algorithms. The results indicated the following: (1) the accuracy of the
RF model is greatly influenced by geographic location, elevation, and land
cover fractions; (2) however, the redundant predictor variables (if highly
correlated) slightly affect the RF model; and (3) the fitted RF algorithms
perform better on temporal than spatial scales, with unbiased root-mean-square errors (RMSEs) of ∼4.4 and ∼7.3 cm,
respectively. Finally, we used the fitted RF2 algorithm to retrieve a
consistent 32-year daily snow depth dataset from 1987 to 2018. This product
was evaluated against the independent station observations during the period
1987–2018. The mean unbiased RMSE and bias were 7.1 and −0.05 cm,
respectively, indicating better performance than that of the former snow
depth dataset (8.4 and −1.20 cm) from the Environmental and Ecological
Science Data Center for West China (WESTDC). Although the RF product was
superior to the WESTDC dataset, it still underestimated deep snow cover
(>20 cm), with biases of −10.4, −8.9, and −34.1 cm for
northeast China (NEC), northern Xinjiang (XJ), and the Qinghai–Tibetan Plateau
(QTP), respectively. Additionally, the long-term snow depth datasets
(station observations, RF estimates, and WESTDC product) were analyzed in
terms of temporal and spatial variations over China. On a temporal scale,
the ground truth snow depth presented a significant increasing trend from
1987 to 2018, especially in NEC. However, the RF and WESTDC products
displayed no significant changing trends except on the QTP. The WESTDC
product presented a significant decreasing trend on the QTP, with a
correlation coefficient of −0.55, whereas there were no significant trends
for ground truth observations and the RF product. For the spatial
characteristics, similar trend patterns were observed for RF and WESTDC
products over China. These characteristics presented significant decreasing
trends in most areas and a significant increasing trend in central NEC.
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Water Science and Technology
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