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Solar radiative transfer parameterizations for three-dimensional effects in cloudy atmospheres

机译:在阴天气氛中三维效应的太阳辐射传输参数化

摘要

This thesis addresses two major problems in the field of radiative transfer (RT) in theearth’s atmosphere. The first problem is linked with the need for significant computationalresources of RT in a three-dimensional (3D) atmospheric model. Although only highlyefficient one-dimensional (1D) RT models are employed for each pixel of the model domainseparately and independently, it is still not possible to utilize these models on a frequentbasis, compared to the rate at which meteorological variables are computed. That meansthat the calculated radiative properties (RP) are held constant for a longer period of time,while the prognostic meteorological variables are updated at a rapid rate. Even thoughthere is no detailed study about the consequences of this disproportion, an attempt wasmade to develop an RT model which permits the fast computation of basic radiative transferproperties which could be used in the future to update this information more frequently.The developed model is based on the application of the radiative transfer perturbationtheory to realistic cloud fields column by column. It turned out that the application,intended to replace the Independent Pixel Approximation (IPA), see below, is possibleand promising within the assumptions and constraints of the utilized methods. It couldbe demonstrated that, depending on the actual case, errors in the pixel transmission andreflection stay bounded to values of up to 10%−15%. In one case the achieved accelerationcould be investigated. It was about a factor of four compared to the direct application ofthe usual forward variant of the model, although no numerical optimization was carriedout.The second problem concerns the realistic treatment of the 3D interactions of clouds andsolar radiation. As implied in the above paragraph, 1D RT models are usually employedcolumn by column which suppresses the exchange of radiation between those columns.Thus, fundamental 3D effects are neglected by this so-called Independent Pixel Approximation(IPA). These comprise not only small scale contributions due to diffuse radiativetransport, but also large scale patterns like geometric effects of the inclined solar illumination.Examples are blurred radiative structures due to radiative smoothing and theshifted location of shadows and bright areas. To parameterize those effects strong effortshave been undertaken during the last couple of years. However, no method has proven tobe completely satisfactory and ready for implementation. To carry this research one stepfurther two approaches have been adopted and extended. The first is the concept of theTilted Independent Pixel Approximation (TIPA). In contrast to the IPA, which ignores thesolar geometry, this method correctly accounts for the slant illumination due to the correcttracking of the direct beam. As a result, the optical parameters in the slant columns arearranged in a more realistic order and the attenuation and the positions of the RP are lesserroneous. To further improve this method a transformation has been developed whichyields 3D resolution of the RP in the original grid. Since the TIPA still does not includeany diffuse radiative exchange as another approach the Nonlocal Independent Pixel Approximation(NIPA) has been explored. This technique uses 1D results and carries outa convolution product to distribute RP across column boundaries. In order to arrive ata fully independent treatment of this method a simplified derivation of the convolutionparameters was developed. Finally, TIPA and NIPA are combined to form NTIPA. Theseapproaches have proven to be superior to IPA with respect to several aspects. The improvementranges from several percent to 50% if maximum errors of the transmitted andreflected light are considered. Criteria like the distribution of the errors or the verticalprofiles of the RP are also more preferable than their counterparts derived by IPA.
机译:本文解决了地球大气辐射传输(RT)领域中的两个主要问题。第一个问题与在三维(3D)大气模型中需要大量的RT计算资源有关。尽管只有高效的一维(1D)RT模型被单独和独立地用于模型域的每个像素,但是与计算气象变量的速率相比,仍然无法频繁地使用这些模型。这意味着计算出的辐射特性(RP)可以在更长的时间内保持恒定,而预测的气象变量则可以快速更新。即使尚未考虑到这种不均衡的后果的详细研究,也试图开发一个RT模型,该模型允许快速计算基本辐射传递特性,将来可用于更频繁地更新此信息。辐射传递扰动理论在逼真的云场中的应用事实证明,旨在取代独立像素逼近(IPA)(见下文)的应用程序是可能的,并且在所用方法的假设和约束内很有希望。可以证明,取决于实际情况,像素透射和反射中的误差将保持在最高10%-15%的值内。在一种情况下,可以研究所达到的加速度。尽管没有进行数值优化,但与直接应用该模型通常的正向变体相比,它大约是四分之一。第二个问题涉及对云层和太阳辐射的3D相互作用的现实处理。如上一段所暗示的,一维RT模型通常采用逐列的方式来抑制那些列之间的辐射交换,因此基本的3D效果被所谓的独立像素近似(IPA)所忽略。这些不仅包括由于扩散辐射传输引起的小规模贡献,还包括诸如倾斜太阳能照明的几何效应之类的大尺度图案。例如由于辐射平滑以及阴影和明亮区域的位置偏移而导致的辐射结构模糊。为了参数化这些效果,在最近几年中已经进行了很大的努力。但是,没有一种方法被证明是完全令人满意并且可以实施的。为了进行这项研究,已经采用和扩展了另外两种方法。第一个是倾斜独立像素近似(TIPA)的概念。与IPA忽略了太阳的几何形状相反,该方法正确地考虑了由于直接光束的正确跟踪而产生的倾斜照明。结果,倾斜列中的光学参数以更现实的顺序排列,并且RP的衰减和位置更小。为了进一步改进此方法,已开发出一种转换,该转换可在原始网格中获得RP的3D分辨率。由于TIPA仍不包括任何漫射辐射交换作为另一种方法,因此已探索了非局部独立像素近似(NIPA)。该技术使用一维结果并执行卷积积以将RP分布在列边界上。为了得到该方法的完全独立的处理,开发了卷积参数的简化推导。最后,将TIPA和NIPA合并为NTIPA。在某些方面,这些方法已被证明优于IPA。如果考虑到透射光和反射光的最大误差,则改进范围为百分之几到50%。像误差分布或RP的垂直剖面这样的标准也比IPA得出的标准更可取。

著录项

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    Jerg Matthias;

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  • 年度 2006
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