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Planck Weighted Transmittance and Correction of Solar Reflection for Broadband Infrared Satellite Channels

机译:普朗克加权透射比和宽带红外卫星信道的太阳反射校正

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Three approximations methods to calculate the level-tospacetransmittance, used in fast radiative transfer model,are studied for five infrared broadband channels. Two ofthem are Planck-weighted transmittances, in which oneinvolves the effective layer temperature of a layer (PW1),and the other involves temperatures at the interfacebetween layers (PW2). The third one is not includingtemperature at all (ORD). It is found that under allcircumstances method PW1 is better than method PW2compared to the line-by-line (LBL) calculation. Planckweightedmethods are more sensitive to atmosphericsurface temperatures compared to ORD method.Based on these simulations and comparisons, when theband correction is larger (greater than 1), PW1 methodshould be used to take account of the Planck radiancechanging with the transmittance within the band spectral.When considering the solar contribution in daytime,correction of the solar reflection has been made for nearinfrared broadband channels (~3.7 μm) when using PW1transmittance. The solar transmittance is predicted byusing explanatory variables as PW1 transmittance, secantof zenith angle, and surface temperature. With thecorrection, the error reduces to more reasonable level.
机译:三种近似方法来计算水平空间 透射率,用于快速辐射传输模型, 研究了五个红外宽带信道。两个 它们是普朗克加权透射率,其中一个 涉及层的有效层温度(PW1), 另一个涉及界面温度 层之间(PW2)。第三个不包括 最高温度(ORD)。发现在所有 情况下方法PW1优于方法PW2 与逐行(LBL)计算相比。普朗克加权 方法对大气更敏感 与ORD方法相比的表面温度。 根据这些模拟和比较, 波段校正较大(大于1),PW1方法 应该用于考虑普朗克辐射 随光谱范围内的透射率而变化。 考虑白天的太阳辐射量时, 已对近距离的太阳反射进行了校正 使用PW1时的红外宽带通道(〜3.7μm) 透射率。通过以下公式预测太阳光透射率 使用解释变量作为PW1透射率,割线 天顶角和表面温度的关系随着 校正后,误差降低到更合理的水平。

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