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Mapping technique of climate fields between GCM's and ice models

机译:GCM与冰模型之间气候场的制图技术

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Here, we present a mapping method OBLIMAP, which projects and interpolates fields like surface temperature, surface mass balance, and surface height between a geographical based coordinate system of a Global Circulation Model (GCM) and a rectangular based Ice Model (IM). We derive an oblique stereographic projection and its inverse, which holds for any area at the Earth surface, and can be combined with two different interpolation methods. The first one is suited to interpolate the projected fields of a coarse GCM grid on a fine meshed IM grid. The second one is appropriate for the opposite case. Both grids are allowed to be arbitrary and irregularly spaced. Therefore the OBLIMAP technique is suitable for any GCM-IM combination. After a first scan of the GCM grid coordinates and the specification of the IM grid, fast mapping of various fields is possible. To and fro (GCM-IM-GCM) mapping tests with the Climate Community System Model (CCSM) at T42 resolution (~313 km) and the Regional Atmospheric Climate Model (RACMO) at ~11 km, show average temperature differences of less than 0.1 K with small standard deviations. OBLIMAP, available at GMD, is an accurate, robust and well-documented mapping method for coupling an IM with a GCM or to map state of the art initial and forcing fields available at geographical coordinates to any local IM grid with an optimal centered projection.
机译:在这里,我们介绍了一种映射方法OBLIMAP,该方法在全球循环模型(GCM)的基于地理的坐标系和基于矩形的冰模型(IM)之间投影和插值诸如表面温度,表面质量平衡和表面高度的字段。我们推导出了一个倾斜的立体投影及其倒数,它适用于地球表面的任何区域,并且可以与两种不同的插值方法结合使用。第一个适合于将粗GCM网格的投影场插值到细网格IM网格上。第二种适用于相反的情况。两个网格都可以是任意的且不规则地间隔。因此,OBLIMAP技术适用于任何GCM-IM组合。在第一次扫描GCM网格坐标和IM网格的规格后,可以快速映射各个字段。使用T42分辨率(〜313 km)的气候共同体系统模型(CCSM)和〜11 km的区域大气气候模型(RACMO)的来回(GCM-IM-GCM)映射测试显示平均温度差小于0.1 K,标准偏差小。 GMD上的OBLIMAP是一种准确,健壮且有据可查的映射方法,用于将IM与GCM耦合或将地理坐标上可用的现有技术的初始场和​​强迫场映射到具有最佳中心投影的任何本地IM网格。

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