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arXiv 1902.04669physics.ao-phphysics.class-phphysics.flu-dynphysics.geo-ph
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气候模式中水、能量和熵收支的新诊断工具

A new diagnostic tool for water, energy and entropy budgets in climate models

Valerio Lembo, Frank Lunkeit, Valerio Lucarini

摘要:

这项工作提出了一种新的诊断工具,用于研究气候系统的热力学,具有广泛的应用,从敏感性研究到模型调整。它包括一些分别用于评估内能收支、水文循环、洛伦兹能量循环和物质熵产生的模块。该程序接收地面和大气层顶(TOA)的能量通量作为输入,用于计算大气层顶(TOA)、地面和大气中的能量收支作为残差。经向焓输运也计算从纬向平均能量收支通量的发散,在两个半球的峰值的位置和强度,然后提供作为输出。降雨,降雪和潜热通量作为输入计算水的质量和潜能预算。如果提供陆地-海洋掩模,则分别计算大陆和海洋上的所需数量。该诊断工具还计算洛伦兹能量循环(LEC)及其储存/转换项作为年度平均全球和半球值。为了实现这一点,需要提供对流层水平风速和温度的三维日场作为输入。两种方法已经实施的物质熵产生的计算,一个依赖于在大气中的辐射热通量的收敛(间接方法),一个结合发生在气候系统中的不可逆过程,特别是在边界层中的热通量,水文循环和动能耗散从LEC的残差检索。诊断工具的一个版本被纳入地球系统模型电子评估工具(ESMValTool)社区诊断,以评估即将推出的CMIP 6模型模拟的性能。

英文摘要:

This work presents a novel diagnostic tool for studying the thermodynamics of the climate systems with a wide range of applications, from sensitivity studies to model tuning. It includes a number of modules for assessing the internal energy budget, the hydrological cycle, the Lorenz Energy Cycle and the material entropy production, respectively. The routine receives as inputs energy fluxes at surface and at the Top-of-Atmosphere (TOA), for the computation of energy budgets at Top-of-Atmosphere (TOA), at the surface, and in the atmosphere as a residual. Meridional enthalpy transports are also computed from the divergence of the zonal mean energy budget fluxes; location and intensity of peaks in the two hemispheres are then provided as outputs. Rainfall, snowfall and latent heat fluxes are received as inputs for computing the water mass and latent energy budgets. If a land-sea mask is provided, the required quantities are separately computed over continents and oceans. The diagnostic tool also computes the Lorenz Energy Cycle (LEC) and its storage/conversion terms as annual mean global and hemispheric values. In order to achieve this, one needs to provide as input three-dimensional daily fields of horizontal wind velocity and temperature in the troposphere. Two methods have been implemented for the computation of the material entropy production, one relying on the convergence of radiative heat fluxes in the atmosphere (indirect method), one combining the irreversible processes occurring in the climate system, particularly heat fluxes in the boundary layer, the hydrological cycle and the kinetic energy dissipation as retrieved from the residuals of the LEC. A version of the diagnostic tool is included in the Earth System Model eValuation Tool (ESMValTool) community diagnostics, in order to assess the performances of soon available CMIP6 model simulations.

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