Prospects for Detecting Volcanic Events with Microwave Radiometry

Identifying volcanic activity on worlds with optically thick atmospheres with passive microwave radiometry has been proposed as a means of skirting the atmospheric interference that plagues near infrared observations. By probing deeper into the surface, microwave radiometers may also be sensitive to...

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Main Authors: Shannon M. MacKenzie, Ralph D. Lorenz
Format: Article
Language:English
Published: MDPI AG 2020-08-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/16/2544
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spelling doaj-b835b1b474ef4493b57568ebd64343b52020-11-25T02:54:54ZengMDPI AGRemote Sensing2072-42922020-08-01122544254410.3390/rs12162544Prospects for Detecting Volcanic Events with Microwave RadiometryShannon M. MacKenzie0Ralph D. Lorenz1Applied Physics Laboratory, Johns Hopkins University, 1001 Johns Hopkins Road, Laurel, MD 20723, USAApplied Physics Laboratory, Johns Hopkins University, 1001 Johns Hopkins Road, Laurel, MD 20723, USAIdentifying volcanic activity on worlds with optically thick atmospheres with passive microwave radiometry has been proposed as a means of skirting the atmospheric interference that plagues near infrared observations. By probing deeper into the surface, microwave radiometers may also be sensitive to older flows and thus amenable for investigations where repeat observations are infrequent. In this investigation we explore the feasibility of this tactic using data from the Soil Moisture Active Passive (SMAP) mission in three case studies: the 2018 Kilauea eruption, the 2018 Oct-Nov eruption at Fuego, and the ongoing activity at Erta Ale in Ethiopia. We find that despite SMAP’s superior spatial resolution, observing flows that are small fractions of the observing footprint are difficult to detect—even in resampled data products. Furthermore, the absorptivity of the flow, which can be temperature dependent, can limit the depths to which SMAP is sensitive. We thus demonstrate that the lower limit of detectability at L-band (1.41 GHz) is in practice higher than expected from first principles.https://www.mdpi.com/2072-4292/12/16/2544volcanoes, SMAP, microwave radiometry
collection DOAJ
language English
format Article
sources DOAJ
author Shannon M. MacKenzie
Ralph D. Lorenz
spellingShingle Shannon M. MacKenzie
Ralph D. Lorenz
Prospects for Detecting Volcanic Events with Microwave Radiometry
Remote Sensing
volcanoes, SMAP, microwave radiometry
author_facet Shannon M. MacKenzie
Ralph D. Lorenz
author_sort Shannon M. MacKenzie
title Prospects for Detecting Volcanic Events with Microwave Radiometry
title_short Prospects for Detecting Volcanic Events with Microwave Radiometry
title_full Prospects for Detecting Volcanic Events with Microwave Radiometry
title_fullStr Prospects for Detecting Volcanic Events with Microwave Radiometry
title_full_unstemmed Prospects for Detecting Volcanic Events with Microwave Radiometry
title_sort prospects for detecting volcanic events with microwave radiometry
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-08-01
description Identifying volcanic activity on worlds with optically thick atmospheres with passive microwave radiometry has been proposed as a means of skirting the atmospheric interference that plagues near infrared observations. By probing deeper into the surface, microwave radiometers may also be sensitive to older flows and thus amenable for investigations where repeat observations are infrequent. In this investigation we explore the feasibility of this tactic using data from the Soil Moisture Active Passive (SMAP) mission in three case studies: the 2018 Kilauea eruption, the 2018 Oct-Nov eruption at Fuego, and the ongoing activity at Erta Ale in Ethiopia. We find that despite SMAP’s superior spatial resolution, observing flows that are small fractions of the observing footprint are difficult to detect—even in resampled data products. Furthermore, the absorptivity of the flow, which can be temperature dependent, can limit the depths to which SMAP is sensitive. We thus demonstrate that the lower limit of detectability at L-band (1.41 GHz) is in practice higher than expected from first principles.
topic volcanoes, SMAP, microwave radiometry
url https://www.mdpi.com/2072-4292/12/16/2544
work_keys_str_mv AT shannonmmackenzie prospectsfordetectingvolcaniceventswithmicrowaveradiometry
AT ralphdlorenz prospectsfordetectingvolcaniceventswithmicrowaveradiometry
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