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COSIPY v1.3 – an open-source coupled snowpack and ice surface energy and mass balance model

机译:Cosipy V1.3 - 一个开源耦合的积雪和冰表面能量和质量平衡模型

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Glacier changes are a vivid example of how environmental systems react to a changing climate. Distributed surface mass balance models, which translate the meteorological conditions on glaciers into local melting rates, help to attribute and detect glacier mass and volume responses to changes in the climate drivers. A well-calibrated model is a suitable test bed for sensitivity, detection, and attribution analyses for many scientific applications and often serves as a tool for quantifying the inherent uncertainties. Here, we present the open-source COupled Snowpack and Ice surface energy and mass balance model in PYthon (COSIPY), which provides a flexible and user-friendly framework for modeling distributed snow and glacier mass changes. The model has a modular structure so that the exchange of routines or parameterizations of physical processes is possible with little effort for the user. The framework consists of a computational kernel, which forms the runtime environment and takes care of the initialization, the input–output routines, and the parallelization, as well as the grid and data structures. This structure offers maximum flexibility without having to worry about the internal numerical flow. The adaptive subsurface scheme allows an efficient and fast calculation of the otherwise computationally demanding fundamental equations. The surface energy balance scheme uses established standard parameterizations for radiation as well as for the energy exchange between atmosphere and surface. The schemes are coupled by solving both surface energy balance and subsurface fluxes iteratively such that consistent surface skin temperature is returned at the interface. COSIPY uses a one-dimensional approach limited to the vertical fluxes of energy and matter but neglects any lateral processes. Accordingly, the model can be easily set up in parallel computational environments for calculating both energy balance and climatic surface mass balance of glacier surfaces based on flexible horizontal grids and with varying temporal resolution. The model is made available on a freely accessible site and can be used for non-profit purposes. Scientists are encouraged to actively participate in the extension and improvement of the model code.
机译:冰川变化的系统环境如何应对气候变化的一个生动的例子。分布式表面物质平衡模型,冰川气象条件转化为局部熔化率,帮助属性和检测冰川的质量和体积的反应在气候变化的驱动程序。良好的校准模型是灵敏度,检测合适的试验台,和归属分析了许多科学应用和通常用作用于定量固有的不确定性的工具。在这里,我们目前的开源加上积雪和冰面能量和质量平衡模型在Python(COSIPY),它提供了分布式建模积雪和冰川的质量变化灵活和人性化的框架。该模型具有模块化结构,使例程或物理过程参数化的的交流是可能的用户很少的努力。该框架包括一个计算内核,形成运行环境和需要初始化,输入输出程序,以及并行化,以及网格和数据结构的照顾。这种结构提供了最大的灵活性,而不必担心内部的数字流。自适应地下方案允许否则计算要求基本方程的有效和快速的计算。表面能量平衡方案使用用于辐射以及用于气氛和表面之间的能量交换建立的标准参数化。该方案通过求解两个表面能量平衡和地下通量耦合迭代,使得一致的表面皮肤温度在界面处返回。 COSIPY使用限于能量的垂直磁通的一维的方法和物质,但忽略任何横向进程。因此,该模型可容易地设置在并行计算环境中,用于计算两个能量平衡和基于灵活水平网格冰川表面的气候表面质量平衡和具有不同的时间分辨率。该模型提供一个可自由访问的网站,可用于非营利目的。鼓励科学家积极参与型号代码的扩展和完善。

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