首页|期刊导航|干旱区资源与环境|内蒙古高原多源雪深数据集适用性评估

内蒙古高原多源雪深数据集适用性评估OACHSSCD

Applicability evaluation on multi-source snow depth datasets in Inner Mongolia Plateau

中文摘要英文摘要

积雪是冬春季水循环过程的关键地球物理变量,当前格点雪深数据集在内蒙古高原存在较大不确定性,适用性研究亟须开展.基于2016~2025年内蒙古高原119个国家气象站观测逐日雪深资料,利用时间序列相关性、无偏均方根误差和克林-古普塔效率系数(KGE)等指标,评价了欧洲第五代再分析(ERA5)、欧洲第五代陆面再分析(ERA5Land)、全球陆面同化系统NOAH(GLDAS-NOAH)、全球陆面同化系统CLSM(GLDAS-CLSM)和全球同化系统(GDAS)雪深数据集在内蒙古高原的精度和适用性.结果表明:1)五套格点雪深数据集在内蒙古高原及其3个分区适用性各异,CLSM在内蒙古高原和东部区适用性最好,ERA5Land在中部区适用性最好,ERA5在西部区适用性最好.2)五套雪深数据集时空分布存在差异,但均能再现内蒙古高原雪深东高西低的空间分布,ERA5、ERA5Land和CLSM数据集均对内蒙古高原大部的雪深模拟能力相对较好,NOAH和GDAS在大多数时段高估了雪深.3)在内蒙古高原东部区适用性最优的CLSM在监测极端暴雪事件中表现不佳,同化了多源观测积雪资料的ERA5在监测40cm以上的积雪方面表现相对较好,其他数据集对大于40cm以上的积雪的监测能力不足.综上,各套数据集在内蒙古高原及其3个分区中表现各异,CLSM虽然在东部区的适用性最优,但在40cm以上的积雪监测中表现不如ERA5,各套雪深数据集在西部区的适用性差于其在其他区域的适用性.

Snow is a key geophysical variable in the water cycle in winter and spring.The current gridded snow depth datasets have great uncertainty in the Inner Mongolia Plateau,and its applicability needs to be studied urgently.Based on daily snow depth data observed from 119 national weather stations in the Inner Mongolian Plateau from 2016 to 2025,using indicators such as time series correlation,unbiased mean square root error,and Kling-Gupta efficiency coefficient(KGE),the accuracy and applicability of European Fifth Generation Reanalysis(ERA5),European Fifth Generation Land Reanalysis(ERA5 Land),Global Land Assimilation System NOAH(GLDAS-NOAH),Global Land Assimilation System CLSM(GLDAS-CLSM),and Global Assimilation System(GDAS)snow depth datasets were evaluated in the Inner Mongolian Plateau.The results reveal:1)The five snow depth datasets had different applicability in the Inner Mongolian Plateau and its three sub-regions.CLSM had the best applicability in the Inner Mongolian Plateau and the eastern region,ERA5Land had the best applicability in the central region,and ERA5 had the best applicability in the western region.2)The five snow depth datasets had different spatial and temporal distributions,but all could reproduce the spatial distribution of snow depth in the eastern and western regions of Inner Mongolian Plateau.ERA5,ERA5Land,and CLSM datasets were relatively good at simulating the snow depth in most parts of the Inner Mongolian Plateau.NOAH and GDAS overestimated the snow depth for most periods.3)The CLSM with the best applicability in the eastern region of the Inner Mongolian Plateau performed poorly in monitoring extreme snowstorm event with snow depth greater than 40cm,but the ERA5 dataset which assimilated multi-source snow observations performed relatively well,while the other four datasets had limited monitoring capacity for snow depth greater than 40 cm.In conclusion,none of the datasets performed the best in the Inner Mongolian Plateau and its three sub-regions.Although the CLSM had the best applicability in the eastern region,it performed less well than ERA5 in extreme snowstorm event with snow depth greater than 40cm,and the applicability of each snow depth dataset in the western region was worse than its applicability in other regions.

宋海清;皇彦;孙小龙

内蒙古自治区生态与农业气象中心,呼和浩特 010051||内蒙古自治区气象卫星遥感中心,呼和浩特 010051内蒙古自治区生态与农业气象中心,呼和浩特 010051||内蒙古自治区气象卫星遥感中心,呼和浩特 010051内蒙古自治区生态与农业气象中心,呼和浩特 010051||内蒙古自治区气象卫星遥感中心,呼和浩特 010051

天文与地球科学

雪深内蒙古高原适用性ERA5ERA5LandGLDAS

snow depthInner Mongolia PlateauapplicabilityERA5ERA5LandGLDAS

《干旱区资源与环境》 2026 (8)

109-122,14

内蒙古自治区自然科学基金(2023QN05021、2024ZD03)国家自然科学基金区域创新发展联合基金重点支持项目(U24A20573)内蒙古自治区重点研发和成果转化计划(2025YFHH0027)中国气象局气象能力提升联合研究专项(23NLTSQ008)松辽流域气象科技创新项目(SL202401)海河流域气象科技创新项目(HHXM202509)资助.

10.13448/j.cnki.jalre.2026.136

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