Abstract

Aims: To develop a new satellite -based mixed-phase cloud retrieval algorithm for improving mixed-phase cloud liquid water path (LWP) retrievals by combining Moderate Resolution Imaging Spectroradiometer (MODIS), CloudSat, and Cloud -Aerosol Lidar and Infrared Pathfinder Satellite Observations (CALIPSO) measurements. Study Design:Algorithm development and evaluation by using collocated NASA A

Highlights

  • Clouds are important because of their roles in the global hydrological cycle and transport of heat and moisture from low latitudes towards the poles [1,2]

  • A mixed-phase cloud retrieval algorithm was developed for stratiform mixed-phase clouds by using multi sensor measurements from the NASA A-Train satellites

  • Similar to the operational Moderate Resolution Imaging Spectroradiometer (MODIS) algorithm, the following main assumptions were used in the forward model: (1) plane-parallel atmosphere with a liquid water layer over an ice layer representing stratiform mixed-phase clouds

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Summary

INTRODUCTION

Clouds are important because of their roles in the global hydrological cycle and transport of heat and moisture from low latitudes towards the poles [1,2]. [16] showed that middle-level stratiform mixed-phase cover is over 5% globally These mixedphase clouds have significant radiative impacts at the top of the atmosphere (TOA) and the surface [17].the properties and evolutions of these mixed-phase clouds are difficult to simulate [18,19]. Treating the stratiform mixed-phase clouds with two separate liquid and ice layers is a validapproximation for radiative transfer calculations, it does not fully describe the details of the mixedphase clouds These stratiform clouds with liquid dominated mixed-phase layer with ice virga below is commonly observed over the polar regions; study by Zhang, et al [16] showed that they are observed globally and have profound impact on the radiative balance of the earth

The Forward Model
A Calculation Example of Lookup Table
Retrieve LWP and re
ERROR ANALYSIS
Sensitivity to Surface Albedo
Sensitivity to IWP
Validation Using Operational MODIS Retrievals of Liquid Water Clouds
Validation using Collocated Ground-Based Measurements of Mixed-Phase Clouds
APPLICATION TO A-TRAIN MEASUREMENTS
Findings
SUMMARY AND CONCLUSION
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