首页|基于Crocus模型的雪深模拟研究

基于Crocus模型的雪深模拟研究

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雪深的准确模拟对于寒区的水文过程、气候变化、生态环境具有重要意义。积雪过程模型可以定量模拟物理环境对积雪参数的影响过程,从物理意义上定量模拟区域雪深。但是,目前积雪过程模型模拟存在参数设置复杂、不确定性大等问题。因此,有必要通过参数率定找到最适应区域的参数组合,从而完成模型参数的本地化。本文应用Crocus模型,在西藏自治区的聂拉木站、普兰站和帕里站进行3 a(2019—2021年)逐日雪深模拟,利用UQ-Pyl进行模型参数的敏感性分析及率定,构建以上站点的Crocus模型,并通过相关系数(R)、标准差比(SDC)、纳什效率系数(NSE)、平均差值(BIAS)和均方根误差(RMSE)综合评估Crocus模型在聂拉木站、普兰站和帕里站的适用性。结果表明:聂拉木站、普兰站、帕里站的Crocus模型主要敏感参数分别有20、15、13个;Crocus模型在聂拉木站的雪深模拟效果最佳(R=0。989、SDC=0。990、NSE=0。978、BIAS=0。276 cm、RMSE=4。280 cm),普兰站和帕里站次之;其中,聂拉木站的积雪沉降、积累和融化过程得到了很好的模拟,普兰站在积雪较厚时模拟效果更优,帕里站在每年3—4月时模型高估了雪深,但变化趋势基本一致,3个站点的日雪深模拟结果基本反映了雪深日变化过程。本文对Crocus模型的本地化是对积雪过程模拟研究的有益补充,为理解和揭示西藏自治区的积雪过程可提供科学依据和信息,同时,也为提高区域气候预测水平、水资源有效管理、灾害预防和应对提供有力支撑。
Research on snow depth simulation of Crocus model
In the context of global warming,the cryosphere is the second largest climate system in the world,and its changing characteristics and impacts are attracting more and more attention. In the past decade or more,the cryosphere has been shrinking all over the world. As a major part of the cryosphere,the change of snow cov-er will have a significant impact on climate change,ecological environment,agriculture and animal husbandry development and water resources balance. It will also affect the ecological environment,the development of ag-riculture and animal husbandry and the balance of water resources. The snow resources in the southern border ar-ea are extremely rich. Global warming accelerates the melting of snow and glaciers in Xizang,resulting in fre-quent snow and ice disasters such as avalanches,glacial lake outburst and glacial debris flow. It has a great im-pact on local production and residents' lives. Therefore,accurate simulation of snow depth is of great signifi-cance for hydrological processes,climate change,and ecological environment in cold regions. At present,the methods for simulating and monitoring snow depth mainly include ground snow depth observation,inversion of snow depth based on microwave remote sensing,measurement of snow depth based on satellite altimetry technol-ogy,and simulation of snow depth using snow accumulation process models. The snow accumulation process model is based on strict physical meaning and can quantitatively simulate the influence of physical environment on snow parameters,quantitatively simulating regional snow depth from a physical sense. The snow accumula-tion process model mainly includes single-layer snow accumulation model,medium complexity snow accumula-tion model,and detailed snow accumulation model. The model used in this paper is a detailed snow cover mod-el,which is based on the layering of snow physical properties and can describe the evolution of snow microstruc-ture over time. However,the current snow accumulation process model simulation has problems such as com-plex parameter settings and high uncertainty. Therefore,it is necessary to find the most suitable parameter com-bination for the region through parameter calibration,in order to complete the localization of model parameters. This paper innovatively applies the Crocus model for daily snow depth simulation over three years (2019—2021) at Nyalam Station,Purang Station,and Pagri Station in Xizang. Using UQ-Pyl software for model param-eter sensitivity analysis and calibration,the paper constructs localized Crocus models for the aforementioned sta-tions. The applicability of the Crocus model at Nyalam Station,Purang Station,and Pagri Station is comprehen-sively evaluated through correlation coefficients(R),ratios of standard deviation (SDC),Nash efficiency coeffi-cients (NSE),mean differences (BLAS) and root mean square error (RMSE). The results show:the main sen-sitive parameters for the Crocus model are 20 at Nyalam Station,15 at Purang Station,and 13 at Pagri Station;the best snow depth simulation effect of the Crocus model is achieved at Nyalam Station (correlation coefficient of 0.989,ratios of standard deviation of 0.990,Nash efficiency coefficient of 0.978,mean difference of 0.276,root mean square error of 4.280),followed by Purang Station and Pagri Station;among these,the snow settlement,accumulation,and melting processes at Nyalam Station are well simulated,and Purang Station shows superior simulation effects when snow is thick,while Pagri Station overestimates snow depth in March-April each year,but the trend is generally consistent. The daily snow depth simulation results of three stations basically reflect the daily variation process of snow depth. The localization of the Crocus model in this paper is a useful supplement to the snow process simulation research. This paper hopes to provide scientific basis and infor-mation for understanding and revealing the snow process in Xizang Autonomous Region,and also provide strong support for improving the regional climate prediction level,effective management of water resources,disaster prevention and response.

snow depthCrocus snow modelsnow depth simulationUQ-Pylsensitivity analysis,parameter optimization

陶星宇、柳锦宝、拉珍、巴桑、高瑜莲、赵爽、汪菀蔚

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屏山县气象局,四川宜宾 645350

成都信息工程大学资源环境学院,四川成都 610200

西藏自治区气候中心,西藏拉萨 850001

西藏高原大气环境科学研究所,西藏拉萨 850001

北京师范大学地理科学学部环境变化与自然灾害教育部重点实验室,北京 100875

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积雪深度 Crocus积雪模型 雪深模拟 UQ-Pyl 敏感性分析 参数率定

国家自然科学基金项目四川省科技厅重点研发计划项目四川省科技厅重点研发计划项目中国气象局创新发展专项

420650082021YFS03282020YFG0146CXFZ2021J055

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(4)