Hydrological Excitations of Polar Motion Derived from Different Variables of Fgoals − g2 Climate Model

IF 0.7 Q4 ASTRONOMY & ASTROPHYSICS
M. Wińska
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引用次数: 2

Abstract

Abstract The hydrological contribution to decadal, inter-annual and multi-annual suppress polar motion derived from climate model as well as from GRACE (Gravity Recovery and Climate Experiment) data is discussed here for the period 2002.3-2016.0. The data set used here are Earth Orientation Parameters Combined 04 (EOP C04), Flexible Global Ocean-Atmosphere-Land System Model: Grid-point Version 2 (FGOAL-g2) and Global Land Data Assimilation System (GLDAS) climate models and GRACE CSR RL05 data for polar motion, hydrological and gravimetric excitation, respectively. Several Hydrological Angular Momentum (HAM) functions are calculated here from the selected variables: precipitation, evaporation, runoff, soil moisture, accumulated snow of the FGOALS and GLDAS climate models as well as from the global mass change fields from GRACE data provided by the International Earth Rotation and Reference System Service (IERS) Global Geophysical Fluids Center (GGFC). The contribution of different HAM excitation functions to achieve the full agreement between geodetic observations and geophysical excitation functions of polar motion is studied here.
fgoal−g2气候模式中不同变量对极地运动的水文激励
本文讨论了气候模式和GRACE (Gravity Recovery and climate Experiment)数据在2002.3-2016.0期间对年代际、年际和多年际抑制极运动的水文贡献。本文使用的数据集分别是地球方向参数组合04 (EOP C04)、灵活的全球海洋-大气-陆地系统模型:格点版本2 (FGOAL-g2)和全球陆地数据同化系统(GLDAS)气候模式以及GRACE CSR RL05数据,用于极地运动、水文和重力激励。本文根据FGOALS和GLDAS气候模式的降水、蒸发、径流、土壤湿度、积雪等变量,以及国际地球自转和参考系统服务(IERS)全球地球物理流体中心(GGFC)提供的GRACE数据中的全球质量变化场,计算了几个水文角动量(HAM)函数。研究了不同的地磁激励函数对实现大地观测与地球物理极运动激励函数完全一致的贡献。
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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来源期刊
CiteScore
1.00
自引率
11.10%
发文量
0
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