TY - JOUR
T1 - Retrieval of cloud physical parameters from ground based observations of microwave atmospheric radiation and transmitted solar radiation
AU - Ishida, Haruma
AU - Hayasaka, Tadahiro
AU - Tanaka, Masayuki
PY - 1998
Y1 - 1998
N2 - Several methods are proposed in this study to retrieve some cloud physical parameters from ground-based simultaneous observations with a microwave radiometer and other instruments. When cloud is thin, liquid water path and columnar water vapor amount can be retrieved to be consistent with measured intensities of two frequencies around 20 GHz and around 30 GHz under the assumption of homogeneous cloud temperature. In this retrieval procedure, cloud temperature, which affects the calculated value of liquid water path seriously, is given from measurement with a infrared radiative thermometer. The effective radius of cloud particles is also derived from comparing the measured downward solar flux on the ground surface to calculated one. For the thick cloud, which is expected that the temperature difference between top and bottom of cloud is large, cloud top temperature is also retrieved from narrow view angle measurements of transmitted radiance of solar radiation at two wavelengths in addition to microwave measurements. The liquid water path is deduced from the comparison of measured radiances at the two wavelengths to the calculated values, thus the appropriate cloud top temperature can be retrieved to be consistent with the measured microwave intensity at two frequencies. Practices suggested that the observation with a microwave radiometer and a pyrnometer enables to derive the detail of cloud structure.
AB - Several methods are proposed in this study to retrieve some cloud physical parameters from ground-based simultaneous observations with a microwave radiometer and other instruments. When cloud is thin, liquid water path and columnar water vapor amount can be retrieved to be consistent with measured intensities of two frequencies around 20 GHz and around 30 GHz under the assumption of homogeneous cloud temperature. In this retrieval procedure, cloud temperature, which affects the calculated value of liquid water path seriously, is given from measurement with a infrared radiative thermometer. The effective radius of cloud particles is also derived from comparing the measured downward solar flux on the ground surface to calculated one. For the thick cloud, which is expected that the temperature difference between top and bottom of cloud is large, cloud top temperature is also retrieved from narrow view angle measurements of transmitted radiance of solar radiation at two wavelengths in addition to microwave measurements. The liquid water path is deduced from the comparison of measured radiances at the two wavelengths to the calculated values, thus the appropriate cloud top temperature can be retrieved to be consistent with the measured microwave intensity at two frequencies. Practices suggested that the observation with a microwave radiometer and a pyrnometer enables to derive the detail of cloud structure.
KW - Ground-based microwave radiometer
KW - Retrieval algorithms
KW - Simultaneous observations
UR - http://www.scopus.com/inward/record.url?scp=0038071529&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0038071529&partnerID=8YFLogxK
U2 - 10.1117/12.319493
DO - 10.1117/12.319493
M3 - Conference article
AN - SCOPUS:0038071529
SN - 0277-786X
VL - 3503
SP - 414
EP - 422
JO - Proceedings of SPIE - The International Society for Optical Engineering
JF - Proceedings of SPIE - The International Society for Optical Engineering
T2 - Microwave Remote Sensing of the Atmosphere and Environment
Y2 - 15 September 1998 through 17 September 1998
ER -