Anatomy of the Annular Solar Eclipse of 26 December 2019 and Its Impact on Land- Atmosphere Interactions Over an Arid Region
The impact of 26 December 2019 annular solar eclipse (ASE) on meteorological conditions over the southeastern Arabian Peninsula is investigated. Observations sourced from the spinning enhanced visible and infrared imager (SEVIRI) and vertical temperature profiles measured by a microwave radiometer w...
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Veröffentlicht in: | IEEE geoscience and remote sensing letters 2021-08, Vol.18 (8), p.1312-1316 |
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description | The impact of 26 December 2019 annular solar eclipse (ASE) on meteorological conditions over the southeastern Arabian Peninsula is investigated. Observations sourced from the spinning enhanced visible and infrared imager (SEVIRI) and vertical temperature profiles measured by a microwave radiometer were used. The ASE, which began at 03:36:37.9 Universal Time Coordinated (UTC), that is, 31 m 29.9 s after sunrise, left a significant imprint on the land surface temperature (LST). In particular, in some regions, the LST dropped by more than 4 °C, in comparison to the previous day. In situ soil properties, in particular soil texture, were also found to have modulated the effects of the ASE, with loamy soils experiencing higher heating/cooling rates than sandy soils. Finally, the analysis of atmospheric profiles indicated that the eclipse influenced the flow throughout the atmospheric boundary layer, with a stable layer that was 45-min longer and 90-m deeper compared with the preceding day. |
doi_str_mv | 10.1109/LGRS.2020.3003084 |
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Observations sourced from the spinning enhanced visible and infrared imager (SEVIRI) and vertical temperature profiles measured by a microwave radiometer were used. The ASE, which began at 03:36:37.9 Universal Time Coordinated (UTC), that is, 31 m 29.9 s after sunrise, left a significant imprint on the land surface temperature (LST). In particular, in some regions, the LST dropped by more than 4 °C, in comparison to the previous day. In situ soil properties, in particular soil texture, were also found to have modulated the effects of the ASE, with loamy soils experiencing higher heating/cooling rates than sandy soils. Finally, the analysis of atmospheric profiles indicated that the eclipse influenced the flow throughout the atmospheric boundary layer, with a stable layer that was 45-min longer and 90-m deeper compared with the preceding day.</description><identifier>ISSN: 1545-598X</identifier><identifier>EISSN: 1558-0571</identifier><identifier>DOI: 10.1109/LGRS.2020.3003084</identifier><identifier>CODEN: IGRSBY</identifier><language>eng</language><publisher>Piscataway: IEEE</publisher><subject>Annular solar eclipse (ASE) ; arid region ; Arid regions ; Arid zones ; Atmospheric boundary layer ; Boundary layers ; Cooling rate ; Infrared radiometers ; Land surface temperature ; Loam ; Meteorological conditions ; Meteorological satellites ; microwave radiometer (MWR) ; Microwave radiometers ; Microwave radiometry ; Ocean temperature ; Radiometers ; Sandy soils ; Sea surface ; Soil ; Soil analysis ; Soil properties ; Soil texture ; Solar eclipses ; spinning enhanced visible and infrared imager (SEVIRI) land surface temperature (LST) ; Sunrise ; Surface temperature ; Surface topography ; Temperature ; Temperature profile ; Temperature profiles ; Texture ; Universal time</subject><ispartof>IEEE geoscience and remote sensing letters, 2021-08, Vol.18 (8), p.1312-1316</ispartof><rights>Copyright The Institute of Electrical and Electronics Engineers, Inc. (IEEE) 2021</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c336t-17a7c0a92766075de61267404424e5eba9109be0f0282a0cbbec2826fe4c33453</citedby><cites>FETCH-LOGICAL-c336t-17a7c0a92766075de61267404424e5eba9109be0f0282a0cbbec2826fe4c33453</cites><orcidid>0000-0003-0006-2685 ; 0000-0002-7587-0006 ; 0000-0002-6609-1385 ; 0000-0001-8746-5262 ; 0000-0003-0066-6040 ; 0000-0002-8562-7368 ; 0000-0002-1241-7319 ; 0000-0002-5039-412X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://ieeexplore.ieee.org/document/9126854$$EHTML$$P50$$Gieee$$Hfree_for_read</linktohtml><link.rule.ids>314,780,784,796,27924,27925,54758</link.rule.ids></links><search><creatorcontrib>Nelli, Narendra Reddy</creatorcontrib><creatorcontrib>Temimi, Marouane</creatorcontrib><creatorcontrib>Fonseca, Ricardo</creatorcontrib><creatorcontrib>Francis, Diana</creatorcontrib><creatorcontrib>Nesterov, Oleksandr</creatorcontrib><creatorcontrib>Abida, Rachid</creatorcontrib><creatorcontrib>Weston, Michael</creatorcontrib><creatorcontrib>Kumar, Anurag</creatorcontrib><title>Anatomy of the Annular Solar Eclipse of 26 December 2019 and Its Impact on Land- Atmosphere Interactions Over an Arid Region</title><title>IEEE geoscience and remote sensing letters</title><addtitle>LGRS</addtitle><description>The impact of 26 December 2019 annular solar eclipse (ASE) on meteorological conditions over the southeastern Arabian Peninsula is investigated. Observations sourced from the spinning enhanced visible and infrared imager (SEVIRI) and vertical temperature profiles measured by a microwave radiometer were used. The ASE, which began at 03:36:37.9 Universal Time Coordinated (UTC), that is, 31 m 29.9 s after sunrise, left a significant imprint on the land surface temperature (LST). In particular, in some regions, the LST dropped by more than 4 °C, in comparison to the previous day. In situ soil properties, in particular soil texture, were also found to have modulated the effects of the ASE, with loamy soils experiencing higher heating/cooling rates than sandy soils. Finally, the analysis of atmospheric profiles indicated that the eclipse influenced the flow throughout the atmospheric boundary layer, with a stable layer that was 45-min longer and 90-m deeper compared with the preceding day.</description><subject>Annular solar eclipse (ASE)</subject><subject>arid region</subject><subject>Arid regions</subject><subject>Arid zones</subject><subject>Atmospheric boundary layer</subject><subject>Boundary layers</subject><subject>Cooling rate</subject><subject>Infrared radiometers</subject><subject>Land surface temperature</subject><subject>Loam</subject><subject>Meteorological conditions</subject><subject>Meteorological satellites</subject><subject>microwave radiometer (MWR)</subject><subject>Microwave radiometers</subject><subject>Microwave radiometry</subject><subject>Ocean temperature</subject><subject>Radiometers</subject><subject>Sandy soils</subject><subject>Sea surface</subject><subject>Soil</subject><subject>Soil analysis</subject><subject>Soil properties</subject><subject>Soil texture</subject><subject>Solar eclipses</subject><subject>spinning enhanced visible and infrared imager (SEVIRI) land surface temperature (LST)</subject><subject>Sunrise</subject><subject>Surface temperature</subject><subject>Surface topography</subject><subject>Temperature</subject><subject>Temperature profile</subject><subject>Temperature profiles</subject><subject>Texture</subject><subject>Universal time</subject><issn>1545-598X</issn><issn>1558-0571</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ESBDL</sourceid><sourceid>RIE</sourceid><recordid>eNo9kNFLwzAQxosoOKd_gPgS8LnzkiZp-1imzkJhsCn4VtLu6jrWpCadMPCPN2XDl7vj7vu-g18Q3FOYUQrpU7FYrWcMGMwigAgSfhFMqBBJCCKml-PMRSjS5PM6uHFuB8B4ksST4DfTajDdkZiGDFskmdaHvbJkbcb6Uu_b3uF4ZJI8Y41dhZYwoClRekPywZG861U9EKNJ4VchyYbOuH6LFkmuB7T-2BrtyPLHO5UmmW03ZIVffnkbXDVq7_Du3KfBx-vL-_wtLJaLfJ4VYR1FcghprOIaVMpiKSEWG5SUyZgD54yjwEqlnkCF0ABLmIK6qrD2k2yQ-wAuomnweMrtrfk-oBvKnTlY7V-WTIhIpJQx6VX0pKqtcc5iU_a27ZQ9lhTKEXI5Qi5HyOUZsvc8nDwtIv7rfZ5MBI_-ADmidgY</recordid><startdate>20210801</startdate><enddate>20210801</enddate><creator>Nelli, Narendra Reddy</creator><creator>Temimi, Marouane</creator><creator>Fonseca, Ricardo</creator><creator>Francis, Diana</creator><creator>Nesterov, Oleksandr</creator><creator>Abida, Rachid</creator><creator>Weston, Michael</creator><creator>Kumar, Anurag</creator><general>IEEE</general><general>The Institute of Electrical and Electronics Engineers, Inc. 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Observations sourced from the spinning enhanced visible and infrared imager (SEVIRI) and vertical temperature profiles measured by a microwave radiometer were used. The ASE, which began at 03:36:37.9 Universal Time Coordinated (UTC), that is, 31 m 29.9 s after sunrise, left a significant imprint on the land surface temperature (LST). In particular, in some regions, the LST dropped by more than 4 °C, in comparison to the previous day. In situ soil properties, in particular soil texture, were also found to have modulated the effects of the ASE, with loamy soils experiencing higher heating/cooling rates than sandy soils. Finally, the analysis of atmospheric profiles indicated that the eclipse influenced the flow throughout the atmospheric boundary layer, with a stable layer that was 45-min longer and 90-m deeper compared with the preceding day.</abstract><cop>Piscataway</cop><pub>IEEE</pub><doi>10.1109/LGRS.2020.3003084</doi><tpages>5</tpages><orcidid>https://orcid.org/0000-0003-0006-2685</orcidid><orcidid>https://orcid.org/0000-0002-7587-0006</orcidid><orcidid>https://orcid.org/0000-0002-6609-1385</orcidid><orcidid>https://orcid.org/0000-0001-8746-5262</orcidid><orcidid>https://orcid.org/0000-0003-0066-6040</orcidid><orcidid>https://orcid.org/0000-0002-8562-7368</orcidid><orcidid>https://orcid.org/0000-0002-1241-7319</orcidid><orcidid>https://orcid.org/0000-0002-5039-412X</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Annular solar eclipse (ASE) arid region Arid regions Arid zones Atmospheric boundary layer Boundary layers Cooling rate Infrared radiometers Land surface temperature Loam Meteorological conditions Meteorological satellites microwave radiometer (MWR) Microwave radiometers Microwave radiometry Ocean temperature Radiometers Sandy soils Sea surface Soil Soil analysis Soil properties Soil texture Solar eclipses spinning enhanced visible and infrared imager (SEVIRI) land surface temperature (LST) Sunrise Surface temperature Surface topography Temperature Temperature profile Temperature profiles Texture Universal time |
title | Anatomy of the Annular Solar Eclipse of 26 December 2019 and Its Impact on Land- Atmosphere Interactions Over an Arid Region |
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