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An exploratory study of cloud remote sensing capabilities of the Communication, Ocean and Meteorological Satellite (COMS) imagery

机译:通信,海洋和气象卫星(COMS)影像的云遥感能力的探索性研究

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摘要

The present study documents optimal methods for the retrieval of cloud properties using five channels (0.6, 3.7, 6.7, 10.8 and 12.0 μm) that are used in many geostationary meteorological satellite observations. Those channels are also to be adopted for the Communication, Ocean and Meteorological Satellite (COMS) scheduled to be launched in 2008. The cloud properties focused on are cloud thermodynamic phase, cloud optical thickness, effective particle radius and cloud-top properties with specific uncertainties. Discrete ordinate radiative transfer models are simulated to build up the retrieval algorithm. The cloud observations derived from the Moderate-resolution Imaging Spectroradiometer (MODIS) are compared with the results to assess the validity of the algorithm. The preliminary validation indicates that the additional use of a band at 6.7 μm would be better in discriminating the cloud ice phase. Cloud optical thickness and effective particle radius can also be produced up to, respectively, 64 and 32 μm by functionally eliminating both ground-reflected and cloud- and ground-thermal radiation components at 0.6 and 3.7 μm. Cloud-top temperature (pressure) in ± 3 K (± 50 hPa) uncertainties can be estimated by a simple 10.8-μm method for opaque clouds, and by an infrared ratioing method using 6.7 and 10.8 μm for semitransparent clouds.
机译:本研究记录了用于许多对地静止气象卫星观测的五个通道(0.6、3.7、6.7、10.8和12.0μm)的云特性检索的最佳方法。这些通道也将用于计划于2008年发射的通信,海洋和气象卫星(COMS)。重点关注的云特性是云热力学阶段,云光学厚度,有效粒子半径和具有不确定性的云顶特性。通过模拟离散辐射传递模型来建立检索算法。将来自中等分辨率成像光谱仪(MODIS)的云观测结果与结果进行比较,以评估该算法的有效性。初步验证表明,额外使用6.7μm的谱带会更好地识别云冰相。通过在功能上消除0.6和3.7μm的地面反射分量以及云和地面热辐射分量,还可以分别产生高达64和32μm的云光学厚度和有效粒子半径。对于不透明的云,可以通过简单的10.8-μm方法来估计不确定度为±3 K(±50 hPa)的云顶温度(压力),对于半透明的云,可以通过使用6.7和10.8μm的红外定量方法来估算。

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