Hailstorm Detection by Satellite Microwave Radiometers

Passive microwave measurements from satellites have been used to identify the signature of hail in intense thunderstorms. The scattering signal of hailstones is typically observed as a strong depression of upwelling brightness temperatures from the cloud to the satellite. Although the relation betwe...

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Main Authors: Sante Laviola, Vincenzo Levizzani, Ralph R. Ferraro, James Beauchamp
Format: Article
Language:English
Published: MDPI AG 2020-02-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/4/621
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spelling doaj-98bb3a25f0444c4cbc2d633f757e68562020-11-24T21:02:03ZengMDPI AGRemote Sensing2072-42922020-02-0112462110.3390/rs12040621rs12040621Hailstorm Detection by Satellite Microwave RadiometersSante Laviola0Vincenzo Levizzani1Ralph R. Ferraro2James Beauchamp3CNR-ISAC, via Gobetti 101, 40129 Bologna, ItalyCNR-ISAC, via Gobetti 101, 40129 Bologna, ItalyNOAA-NESDIS, University Research Court, College Park, MD 20740, USAEarth System Science Interdisciplinary Center (ESSIC), University of Maryland, Maryland, MD 20742, USAPassive microwave measurements from satellites have been used to identify the signature of hail in intense thunderstorms. The scattering signal of hailstones is typically observed as a strong depression of upwelling brightness temperatures from the cloud to the satellite. Although the relation between scattering signal and hail diameter is often assumed linear, in this work a logistic model is used which seems to well approximate the complexity of the radiation extinction process by varying the hail cross-section. A novel probability-based method for hail detection originally conceived for AMSU-B/MHS and now extended to ATMS, GMI, and SSMIS, is presented. The measurements of AMSU-B/MHS were analyzed during selected hailstorms over Europe, South America and the US to quantify the extinction of radiation due to the hailstones and large ice aggregates. To this aim, a probabilistic growth model has been developed. The validation analysis based on 12-year surface hail observations over the US (NOAA official reports) collocated with AMSU-B overpasses have demonstrated the high performance of the hail detection method in distinguishing between moderate and severe hailstorms, fitting the seasonality of hail patterns. The flexibility of the method allowed its experimental application to other microwave radiometers equipped with MHS-like frequency channels revealing a high level of portability.https://www.mdpi.com/2072-4292/12/4/621passive microwavessatellitehail
collection DOAJ
language English
format Article
sources DOAJ
author Sante Laviola
Vincenzo Levizzani
Ralph R. Ferraro
James Beauchamp
spellingShingle Sante Laviola
Vincenzo Levizzani
Ralph R. Ferraro
James Beauchamp
Hailstorm Detection by Satellite Microwave Radiometers
Remote Sensing
passive microwaves
satellite
hail
author_facet Sante Laviola
Vincenzo Levizzani
Ralph R. Ferraro
James Beauchamp
author_sort Sante Laviola
title Hailstorm Detection by Satellite Microwave Radiometers
title_short Hailstorm Detection by Satellite Microwave Radiometers
title_full Hailstorm Detection by Satellite Microwave Radiometers
title_fullStr Hailstorm Detection by Satellite Microwave Radiometers
title_full_unstemmed Hailstorm Detection by Satellite Microwave Radiometers
title_sort hailstorm detection by satellite microwave radiometers
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-02-01
description Passive microwave measurements from satellites have been used to identify the signature of hail in intense thunderstorms. The scattering signal of hailstones is typically observed as a strong depression of upwelling brightness temperatures from the cloud to the satellite. Although the relation between scattering signal and hail diameter is often assumed linear, in this work a logistic model is used which seems to well approximate the complexity of the radiation extinction process by varying the hail cross-section. A novel probability-based method for hail detection originally conceived for AMSU-B/MHS and now extended to ATMS, GMI, and SSMIS, is presented. The measurements of AMSU-B/MHS were analyzed during selected hailstorms over Europe, South America and the US to quantify the extinction of radiation due to the hailstones and large ice aggregates. To this aim, a probabilistic growth model has been developed. The validation analysis based on 12-year surface hail observations over the US (NOAA official reports) collocated with AMSU-B overpasses have demonstrated the high performance of the hail detection method in distinguishing between moderate and severe hailstorms, fitting the seasonality of hail patterns. The flexibility of the method allowed its experimental application to other microwave radiometers equipped with MHS-like frequency channels revealing a high level of portability.
topic passive microwaves
satellite
hail
url https://www.mdpi.com/2072-4292/12/4/621
work_keys_str_mv AT santelaviola hailstormdetectionbysatellitemicrowaveradiometers
AT vincenzolevizzani hailstormdetectionbysatellitemicrowaveradiometers
AT ralphrferraro hailstormdetectionbysatellitemicrowaveradiometers
AT jamesbeauchamp hailstormdetectionbysatellitemicrowaveradiometers
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