2020
DOI: 10.1007/978-3-030-24568-9_7
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Introduction to Passive Microwave Retrieval Methods

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Cited by 21 publications
(10 citation statements)
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“…For high-intensity precipitation, some researchers consider that the underestimation of IMERG stems from the inherent limitations of PMW and infrared (IR) estimation algorithms (Zhang et al, 2019). PMW-based and IR-based algorithms estimate land precipitation from the scattering signal of frozen hydrometeors and cloud top temperature, respectively [75][76][77]. Therefore, they have difficulty in accurately capturing heavy precipitation (such as convective storms) that are weakly linked to cloud top temperature or have no/few ice particles.…”
Section: Evaluation For Different Precipitation Intensitiesmentioning
confidence: 99%
“…For high-intensity precipitation, some researchers consider that the underestimation of IMERG stems from the inherent limitations of PMW and infrared (IR) estimation algorithms (Zhang et al, 2019). PMW-based and IR-based algorithms estimate land precipitation from the scattering signal of frozen hydrometeors and cloud top temperature, respectively [75][76][77]. Therefore, they have difficulty in accurately capturing heavy precipitation (such as convective storms) that are weakly linked to cloud top temperature or have no/few ice particles.…”
Section: Evaluation For Different Precipitation Intensitiesmentioning
confidence: 99%
“…Initial schemes used fundamental characteristics of radiation emitted from raindrops over the oceans to convert the observed brightness temperatures (Tbs) into rain rates. Over land, due to higher background emissivities, higher frequency channels had to be utilised such as the 89 GHz that first flew on the Special Sensor Microwave Imager (SSMI) from 1987 (see [9]), exploiting the scattering signal caused by precipitation-sized ice particles. Multi-channel retrieval schemes exploit the emission and scattering responses at different frequencies to improve the retrievals, although separate techniques are often required for ocean vs. land retrievals [18].…”
Section: Precipitation Retrievalsmentioning
confidence: 99%
“…While imagery of cloud tops (which allow measures of reflectivity, cloud top characteristics and cloud top temperature) are useful, the precipitation falling from the base of the cloud must be inferred from these cloud top properties. Consequently, the mainstay of current precipitation observations is based upon passive microwave (PMW) sensors that are sensitive to the hydrometeor particles within and falling from the base of the clouds (see [9]).…”
Section: Introductionmentioning
confidence: 99%
“…Visible and IR techniques are capable of providing estimates of precipitation at relatively fine temporal and spatial scales from geostationary (GEO) and low Earth orbiting (LEO) platforms, but such estimates are indirect since they depend upon relationships between the cloud-top characteristics and precipitation at the surface [1]. Passive microwave (PMW) observations are more direct since hydrometeors are the main source of atmospheric attenuation and scattering [2]. However, since PMW sensors only occupy LEOs, multiple sensors are required to provide sufficient temporal and spatial coverage of the globe.…”
Section: Introductionmentioning
confidence: 99%