模拟俄罗斯联邦境内积雪形成机制的动态特征。3.历史时期西伯利亚和远东地区的田野和林区

Pub Date : 2024-07-10 DOI:10.1134/s0097807824700842
E. M. Gusev, O. N. Nasonova, E. E. Kovalev, E. A. Shurkhno
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引用次数: 0

摘要

摘要 本文作者开发的SWAP地表模型被用于对俄罗斯亚洲主要地区的森林和田野地区的积雪覆盖特征进行多年计算:计算了历史时期(1967-2019 年)西西伯利亚、东西伯利亚和远东地区的森林和田野积雪特征。将模拟结果与俄罗斯亚洲地区气象站路线积雪调查的相关数据进行比较后发现,SWAP 能够充分再现所选地点空旷地区和林冠下的积雪水当量、积雪深度和密度的动态变化。对于所有位于积雪调查区的站点,均获得了两种地表类型(森林和田野)和两个气候时期(1967-1992 年和 1993-2019 年)的雪盖形成机制特征的气候值,并用于确定历史时期这些特征的变化趋势。结果表明,西西伯利亚、东西伯利亚和远东地区森林和田野积雪覆盖特征气候值的变化方向是一致的,并且与气候模型得出的二十一世纪预测值相一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Simulating the Dynamics of Characteristics of Snow Cover Formation Regime in Russian Federation Territory. 3. Field and Forest Areas in Siberia and Far East in the Historical Period

Abstract

SWAP land surface model, developed by the authors of this article, was used to carry out many-year calculations of snow cover characteristics for forest and field areas in the main regions of Asian Russia: West Siberia, East Siberia, and Far East for a historic period (1967−2019). The comparison of simulation results with the appropriate data of route snow surveys at meteorological stations in the Asian part of RF showed that SWAP adequately reproduces the dynamics of snow water equivalent, snow depth and density in open areas and under forest canopy at the chosen sites. For all sites located in snow survey areas, climatic values of the characteristics of snow cover formation regime were obtained for two types of the land surface (forest and field) and two climatic periods (1967−1992 and 1993−2019) and used to identify trends in changes in these characteristics in the historic period. It was shown that the direction of changes in the climatic values of snow cover characteristics in forest and field areas in West Siberia, East Siberia, and Far East is the same and corresponds to projections for the XXI century derived from climate models.

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