Rain rates are estimated from brightness temperature measured with a Microwave Scanning Radiometer (MSR) carried on board the Marine Observation Satellite 1 (MOS-1). Estimations are made using a rain rate retrieval algorithm based on a radiative-transfer model assuming rain spaced uniformly over the ocean. These values are compared with a Satellite-Derived Index of Precipitation Intensity (SI), which estimates the rain rate from visible and infrared images of a Geostationary Meteorological Satellite in conjunction with rain observation by a radar network of the Japan Meteorological Agency. Good correlation between MSR and SI derived rain rates validates the rain-rate retrieval algorithm.
MSR, MOS-1, SI, GMS, rain measurement
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Yuji OHSAKI, Masaharu FUJITA, "An Intercomparison between MSR and SI Retrieved Rain Rates" in IEICE TRANSACTIONS on Communications,
vol. E75-B, no. 5, pp. 422-426, May 1992, doi: .
Abstract: Rain rates are estimated from brightness temperature measured with a Microwave Scanning Radiometer (MSR) carried on board the Marine Observation Satellite 1 (MOS-1). Estimations are made using a rain rate retrieval algorithm based on a radiative-transfer model assuming rain spaced uniformly over the ocean. These values are compared with a Satellite-Derived Index of Precipitation Intensity (SI), which estimates the rain rate from visible and infrared images of a Geostationary Meteorological Satellite in conjunction with rain observation by a radar network of the Japan Meteorological Agency. Good correlation between MSR and SI derived rain rates validates the rain-rate retrieval algorithm.
URL: https://global.ieice.org/en_transactions/communications/10.1587/e75-b_5_422/_p
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@ARTICLE{e75-b_5_422,
author={Yuji OHSAKI, Masaharu FUJITA, },
journal={IEICE TRANSACTIONS on Communications},
title={An Intercomparison between MSR and SI Retrieved Rain Rates},
year={1992},
volume={E75-B},
number={5},
pages={422-426},
abstract={Rain rates are estimated from brightness temperature measured with a Microwave Scanning Radiometer (MSR) carried on board the Marine Observation Satellite 1 (MOS-1). Estimations are made using a rain rate retrieval algorithm based on a radiative-transfer model assuming rain spaced uniformly over the ocean. These values are compared with a Satellite-Derived Index of Precipitation Intensity (SI), which estimates the rain rate from visible and infrared images of a Geostationary Meteorological Satellite in conjunction with rain observation by a radar network of the Japan Meteorological Agency. Good correlation between MSR and SI derived rain rates validates the rain-rate retrieval algorithm.},
keywords={},
doi={},
ISSN={},
month={May},}
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TY - JOUR
TI - An Intercomparison between MSR and SI Retrieved Rain Rates
T2 - IEICE TRANSACTIONS on Communications
SP - 422
EP - 426
AU - Yuji OHSAKI
AU - Masaharu FUJITA
PY - 1992
DO -
JO - IEICE TRANSACTIONS on Communications
SN -
VL - E75-B
IS - 5
JA - IEICE TRANSACTIONS on Communications
Y1 - May 1992
AB - Rain rates are estimated from brightness temperature measured with a Microwave Scanning Radiometer (MSR) carried on board the Marine Observation Satellite 1 (MOS-1). Estimations are made using a rain rate retrieval algorithm based on a radiative-transfer model assuming rain spaced uniformly over the ocean. These values are compared with a Satellite-Derived Index of Precipitation Intensity (SI), which estimates the rain rate from visible and infrared images of a Geostationary Meteorological Satellite in conjunction with rain observation by a radar network of the Japan Meteorological Agency. Good correlation between MSR and SI derived rain rates validates the rain-rate retrieval algorithm.
ER -