基于WRF-CTSM的北欧芬诺斯坎迪亚水文气候变量评价

IF 3.8 2区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Iris Mužić, Øivind Hodnebrog, Yeliz A. Yilmaz, Terje K. Berntsen, David M. Lawrence, Negin Sobhani
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引用次数: 0

摘要

本研究首次对陆地-大气耦合区域气候模式WRF-CTSM进行了评价。它包括天气研究和预报模型(WRF)和社区地面系统模型(CTSM)(使用与社区陆地模型版本5 (CLM5)相同的配置)。评估是在北欧芬诺斯坎迪亚(挪威、瑞典和芬兰)进行的,因为气候模式对高纬度地区关键水文气候变量的表示存在不确定性,因为这些地区在不断变化的气候中经历了加速的转变。采用水平网格间距10.5 km的13年WRF-CTSM模拟(2010-2022),评估模式在模拟平均、最小和最大2 m温度、降水、积雪(雪深、雪水当量、积雪覆盖时间分数)和地表能量平衡分量方面的偏差。该分析基于与公开观测数据集的年、季、月和日均值比较,这些数据集包括区域尺度网格化台站和卫星数据集,以及地面站的点比例尺观测数据。该模型显示了与所有考虑变量的评估数据集的强大一致性。此外,还可以相当精确地捕获2 m温度、降水、积雪变量和潜热的原位尺度条件。因此,WRF-CTSM被认为是评估北欧芬诺斯坎迪亚陆地-大气相互作用的有力研究工具。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

The Evaluation of Hydroclimatic Variables Over Nordic Fennoscandia Using WRF-CTSM

The Evaluation of Hydroclimatic Variables Over Nordic Fennoscandia Using WRF-CTSM

This study is the first to evaluate the state-of-the-art coupled land-atmosphere regional climate model WRF-CTSM. It comprises the Weather Research and Forecasting model, WRF, and the Community Terrestrial Systems Model, CTSM (using a configuration that is the same as the Community Land Model Version 5, CLM5). The evaluation is conducted over Nordic Fennoscandia (Norway, Sweden, and Finland) since there is uncertainty in climate models' representation of key hydroclimatic variables in high-latitude regions as they experience accelerated transformation in a changing climate. A 13-year WRF-CTSM simulation (2010–2022) is performed using a 10.5 km horizontal grid spacing to assess the model biases in simulating mean, minimum, and maximum 2 m temperature, precipitation, snow cover (snow depth, snow water equivalent, fractional snow-covered duration), and surface energy balance components. The analysis is based on annual, seasonal, monthly, and daily mean comparisons against openly available observational data sets, comprising regional scale gridded station-based and satellite-based data sets, as well as point scale observations from ground stations. The model shows robust agreement with the evaluation data sets across all considered variables. Furthermore, in situ scale conditions in 2 m temperature, precipitation, snow cover variables, and latent heat are captured with considerable precision. WRF-CTSM is thus considered a powerful research tool for the assessment of land-atmosphere interactions over Nordic Fennoscandia.

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来源期刊
Journal of Geophysical Research: Atmospheres
Journal of Geophysical Research: Atmospheres Earth and Planetary Sciences-Geophysics
CiteScore
7.30
自引率
11.40%
发文量
684
期刊介绍: JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.
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