N: 90 S: -90 E: 180 W: -180
Description
This is the narrow-swath MODIS/Aqua subset along CloudSat field of view track. The goal of the narrow-swath subset is to select and return MODIS data that are within +-5 km across the CloudSat track. I.e. the resultant MODIS subset swath is sought to be about 10 km cross-track. However, the original MYD06_L2 has data of 5- and 1-km pixels. Thus, MAC06S0 cross-track width is 3- and 11-pixels, depending on the parameter, and the resultant swath is about 15- and 10-km, correspondingly. Along-track, all MODIS pixels from the original product are preserved.
In the standard product, the level-2 MODIS cloud product consists of cloud optical and physical parameters. These parameters are derived using remotely sensed infrared, visible and near infrared solar reflected radiances. MODIS infrared channel radiances are used to derive cloud top temperature, cloud top height, effective emissivity, cloud phase (ice vs. water, opaque vs. non-opaque), and cloud fraction under both daytime and nighttime conditions. MODIS visible radiances are used to derive cloud optical thickness and effective particle radius and cloud shadow effects. Near infrared solar reflected radiance provides additional information in the retrieval of cloud particle phase (ice vs. water, clouds vs. snow).
The shortname for this level-2 MODIS cloud product is MAC06S0.
YD06_L2 and the principal investigators for this product are MODIS scientists Dr. Bo-Cai Gao (gao@rsd.nrl.navy.mil) for cirrus cloud detection; Dr. Paul Menzel (paulm@ssec.wisc.edu) for cloud top properties; and Dr. Michael King(king@climate.gsfc.nasa.gov) for cloud optical properties.
(The shortname for this product is MAC06S0).
Product Summary
Citation
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Documents
GENERAL DOCUMENTATION
Publications Citing This Dataset
| Title | Year Sort ascending | Author | Topic |
|---|---|---|---|
| Understanding Errors in Cloud Liquid Water Path Retrievals Derived from CloudSat Path-Integrated Attenuation | Lebsock, Matthew, Takahashi, Hanii, Roy, Richard, Kurowski, Marcin J., Oreopoulos, Lazaros | Cloud Frequency, Cloud Emissivity, Cloud Liquid Water/Ice, Cloud Optical Depth/Thickness, Cloud Reflectance, Cloud Top Pressure, Cloud Top Temperature, Cloud Droplet Concentration/Size | |
| Multiple factors explaining the deficiency of cloud profiling radar on detecting oceanic warm clouds | Liu, Dongyang, Liu, Qi, Liu, Guosheng, Wei, Junbo, Deng, Shumei, Fu, Yunfei | Cloud Frequency, Cloud Emissivity, Cloud Liquid Water/Ice, Cloud Optical Depth/Thickness, Cloud Reflectance, Cloud Top Pressure, Cloud Top Temperature, Cloud Droplet Concentration/Size | |
| Oceanic singlelayer warm clouds missed by the cloud profiling radar as inferred from modis and caliop measurements | Liu, Dongyang, Liu, Qi, Qi, Lin, Fu, Yunfei | Cloud Frequency, Cloud Emissivity, Cloud Liquid Water/Ice, Cloud Optical Depth/Thickness, Cloud Reflectance, Cloud Top Pressure, Cloud Top Temperature, Cloud Droplet Concentration/Size | |
| Underestimation of oceanic warm cloud occurrences by the Cloud Profiling Radar aboard CloudSat | Liu, Dongyang, Liu, Qi, Zhou, Lingli | Cloud Frequency, Cloud Emissivity, Cloud Liquid Water/Ice, Cloud Optical Depth/Thickness, Cloud Reflectance, Cloud Top Pressure, Cloud Top Temperature, Cloud Droplet Concentration/Size | |
| Satellite estimates of precipitation susceptibility in lowlevel marine stratiform clouds | Terai, C. R., Wood, R., Kubar, T. L. | Cloud Frequency, Cloud Emissivity, Cloud Liquid Water/Ice, Cloud Optical Depth/Thickness, Cloud Reflectance, Cloud Top Pressure, Cloud Top Temperature, Cloud Droplet Concentration/Size | |
| Detecting opaque and nonopaque tropical upper tropospheric ice clouds: A trispectral technique based on the MODIS 812 m window bands | Hong, Gang, Yang, Ping, Heidinger, Andrew K., Pavolonis, Michael J., Baum, Bryan A., Platnick, Steven E. | INFRARED FLUX, VISIBLE FLUX, Terrain Elevation, Attitude Characteristics, ORBITAL CHARACTERISTICS, VIEWING GEOMETRY, Cloud Frequency, Cloud Emissivity, Cloud Liquid Water/Ice, Cloud Optical Depth/Thickness, Cloud Reflectance, Cloud Top Pressure, Cloud Top Temperature, Cloud Droplet Concentration/Size | |
| Understanding the importance of microphysics and macrophysics for warm rain in marine low clouds. Part I: Satellite observations | Kubar, Terence L., Hartmann, Dennis L., Wood, Robert | Cloud Frequency, Cloud Emissivity, Cloud Liquid Water/Ice, Cloud Optical Depth/Thickness, Cloud Reflectance, Cloud Top Pressure, Cloud Top Temperature, Cloud Droplet Concentration/Size | |
| Investigation of clearsky occurrence rate estimated from CALIOP and MODIS observations | Eguchi, Nawo, Yokota, Tatsuya | Cloud Frequency, Cloud Emissivity, Cloud Liquid Water/Ice, Cloud Optical Depth/Thickness, Cloud Reflectance, Cloud Top Pressure, Cloud Top Temperature, Cloud Droplet Concentration/Size |