AHI-Derived Daytime Cloud Optical/Microphysical Properties and Their Evaluations With the Collection-6.1 MOD06 Product

Cloud optical/microphysical properties (COMPs) with a high spatiotemporal resolution are required for monitoring the evolution of convective clouds, studying aerosol-cloud-precipitation interactions, and evaluating cloud microphysics parameterization schemes in weather and climate models. This study...

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Veröffentlicht in:IEEE transactions on geoscience and remote sensing 2021-08, Vol.59 (8), p.6431-6450
Hauptverfasser: Zhuge, Xiaoyong, Zou, Xiaolei, Wang, Yuan
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Wang, Yuan
description Cloud optical/microphysical properties (COMPs) with a high spatiotemporal resolution are required for monitoring the evolution of convective clouds, studying aerosol-cloud-precipitation interactions, and evaluating cloud microphysics parameterization schemes in weather and climate models. This study applied the bispectral method, commonly used for COMP retrievals, to Advanced Himawari Imager (AHI)/Himawari-8 observations. The AHI daytime cloud optical thickness ( \tau ) and cloud-top particle effective radius ( Re ) retrievals were then evaluated with the Collection-6.1 Moderate Resolution Imaging Spectroradiometer cloud product (MOD06) for a three-month period from June 1, 2017, to August 31, 2017. Overall, the AHI-retrieved COMP results are in good agreement with the MOD06 product. The correlation coefficients of \tau and Re between the AHI retrievals and MOD06 products are 0.76-0.89 and 0.63-0.87, respectively. Overestimations are mainly observed in the 1.6- \mu \text{m} Re (Re 1.6 ) and ice-phase 3.9- \mu \text{m} Re (Re 3.9 ) retrievals. There are \tau dependencies in the retrieval biases of \tau and Re 1.6 , as well as angular dependencies in the retrieval biases of \tau and ice-phase Re 3.9 . Moreover, the monthly mean composites for three COMP retrievals from the MOD06 and AHI algorithms are compared. Significant differences are only found between the two Re 1.6 products. This study also finds that AHI-retrieved Re and \tau values have a diurnal variation over land but not over oceans.
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This study applied the bispectral method, commonly used for COMP retrievals, to Advanced Himawari Imager (AHI)/Himawari-8 observations. The AHI daytime cloud optical thickness (<inline-formula> <tex-math notation="LaTeX">\tau </tex-math></inline-formula>) and cloud-top particle effective radius ( Re ) retrievals were then evaluated with the Collection-6.1 Moderate Resolution Imaging Spectroradiometer cloud product (MOD06) for a three-month period from June 1, 2017, to August 31, 2017. Overall, the AHI-retrieved COMP results are in good agreement with the MOD06 product. The correlation coefficients of <inline-formula> <tex-math notation="LaTeX">\tau </tex-math></inline-formula> and Re between the AHI retrievals and MOD06 products are 0.76-0.89 and 0.63-0.87, respectively. 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This study applied the bispectral method, commonly used for COMP retrievals, to Advanced Himawari Imager (AHI)/Himawari-8 observations. The AHI daytime cloud optical thickness (<inline-formula> <tex-math notation="LaTeX">\tau </tex-math></inline-formula>) and cloud-top particle effective radius ( Re ) retrievals were then evaluated with the Collection-6.1 Moderate Resolution Imaging Spectroradiometer cloud product (MOD06) for a three-month period from June 1, 2017, to August 31, 2017. Overall, the AHI-retrieved COMP results are in good agreement with the MOD06 product. The correlation coefficients of <inline-formula> <tex-math notation="LaTeX">\tau </tex-math></inline-formula> and Re between the AHI retrievals and MOD06 products are 0.76-0.89 and 0.63-0.87, respectively. Overestimations are mainly observed in the 1.6-<inline-formula> <tex-math notation="LaTeX">\mu \text{m} </tex-math></inline-formula> Re (Re 1.6 ) and ice-phase 3.9-<inline-formula> <tex-math notation="LaTeX">\mu \text{m} </tex-math></inline-formula> Re (Re 3.9 ) retrievals. There are <inline-formula> <tex-math notation="LaTeX">\tau </tex-math></inline-formula> dependencies in the retrieval biases of <inline-formula> <tex-math notation="LaTeX">\tau </tex-math></inline-formula> and Re 1.6 , as well as angular dependencies in the retrieval biases of <inline-formula> <tex-math notation="LaTeX">\tau </tex-math></inline-formula> and ice-phase Re 3.9 . Moreover, the monthly mean composites for three COMP retrievals from the MOD06 and AHI algorithms are compared. Significant differences are only found between the two Re 1.6 products. This study also finds that AHI-retrieved Re and <inline-formula> <tex-math notation="LaTeX">\tau </tex-math></inline-formula> values have a diurnal variation over land but not over oceans.]]></abstract><cop>New York</cop><pub>IEEE</pub><doi>10.1109/TGRS.2020.3027017</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0002-9333-4055</orcidid><orcidid>https://orcid.org/0000-0002-7721-9364</orcidid><orcidid>https://orcid.org/0000-0002-6583-1476</orcidid></addata></record>
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source IEEE Electronic Library (IEL)
subjects Algorithms
Climate models
Cloud computing
Cloud optical thickness
cloud-top particle effective radius
Clouds
Coefficients
Convective clouds
Correlation coefficient
Correlation coefficients
Daytime
Diurnal variations
Himawari
Meteorological satellites
Meteorology
Microphysics
Moderate Resolution Imaging Spectroradiometer (MODIS)
MODIS
Oceans
Optical imaging
Optical properties
Optical sensors
Optical thickness
Parameterization
Properties
Resolution
Retrieval
Satellite broadcasting
Spectroradiometers
title AHI-Derived Daytime Cloud Optical/Microphysical Properties and Their Evaluations With the Collection-6.1 MOD06 Product
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