Saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical Atlantic Ocean
Meridional distribution of aerosol optical thickness (AOT) over the tropical Atlantic Ocean (30°N – 30°S) was analyzed to assess seasonal variations of meridional AOT asymmetry. Ten-year MERRA Aerosol Reanalysis (MERRAero) data (July 2002 – June 2012) confirms that the Sahara desert emits a signific...
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ftosti:oai:osti.gov:1221473 2023-07-30T04:05:31+02:00 Saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical Atlantic Ocean Kishcha, Pavel Da Sliva, Arlindo Starobinets, Boris Long, Charles N. Kalashnikova, Olga Alpert, Pinhas 2015-11-17 application/pdf http://www.osti.gov/servlets/purl/1221473 https://www.osti.gov/biblio/1221473 https://doi.org/10.1080/01431161.2015.1060646 unknown http://www.osti.gov/servlets/purl/1221473 https://www.osti.gov/biblio/1221473 https://doi.org/10.1080/01431161.2015.1060646 doi:10.1080/01431161.2015.1060646 54 ENVIRONMENTAL SCIENCES 2015 ftosti https://doi.org/10.1080/01431161.2015.1060646 2023-07-11T09:03:33Z Meridional distribution of aerosol optical thickness (AOT) over the tropical Atlantic Ocean (30°N – 30°S) was analyzed to assess seasonal variations of meridional AOT asymmetry. Ten-year MERRA Aerosol Reanalysis (MERRAero) data (July 2002 – June 2012) confirms that the Sahara desert emits a significant amount of dust into the atmosphere over the Atlantic Ocean. Only over the Atlantic Ocean did MERRAero show that desert dust dominates other aerosol species and is responsible for meridional aerosol asymmetry between the tropical North and South Atlantic. Over the 10-year period under consideration, both MISR measurements and MERRAero data showed a pronounced meridional AOT asymmetry. The meridional AOT asymmetry, characterized by the hemispheric ratio (RAOT) of AOT averaged separately over the North and over the South Atlantic, was about 1.7. Seasonally, meridional AOT asymmetry over the Atlantic was the most pronounced between March and July, when dust presence is maximal (RAOT ranged from 2 to 2.4). There was no noticeable meridional aerosol asymmetry in total AOT from September to October. During this period the contribution of carbonaceous aerosols to total AOT in the South Atlantic was comparable to the contribution of dust aerosols to total AOT in the North Atlantic. During the same 10-year period, MODIS cloud fraction (CF) data showed that there was no noticeable asymmetry in meridional CF distribution in different seasons (the hemispheric ratio of CF ranged from 1.0 to 1.2). MODIS CF data illustrated significant cloud cover (CF of 0.7 – 0.9) with limited precipitation ability along the Saharan Air Layer. Other/Unknown Material North Atlantic SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Merra ENVELOPE(12.615,12.615,65.816,65.816) International Journal of Remote Sensing 36 13 3423 3445 |
institution |
Open Polar |
collection |
SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) |
op_collection_id |
ftosti |
language |
unknown |
topic |
54 ENVIRONMENTAL SCIENCES |
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54 ENVIRONMENTAL SCIENCES Kishcha, Pavel Da Sliva, Arlindo Starobinets, Boris Long, Charles N. Kalashnikova, Olga Alpert, Pinhas Saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical Atlantic Ocean |
topic_facet |
54 ENVIRONMENTAL SCIENCES |
description |
Meridional distribution of aerosol optical thickness (AOT) over the tropical Atlantic Ocean (30°N – 30°S) was analyzed to assess seasonal variations of meridional AOT asymmetry. Ten-year MERRA Aerosol Reanalysis (MERRAero) data (July 2002 – June 2012) confirms that the Sahara desert emits a significant amount of dust into the atmosphere over the Atlantic Ocean. Only over the Atlantic Ocean did MERRAero show that desert dust dominates other aerosol species and is responsible for meridional aerosol asymmetry between the tropical North and South Atlantic. Over the 10-year period under consideration, both MISR measurements and MERRAero data showed a pronounced meridional AOT asymmetry. The meridional AOT asymmetry, characterized by the hemispheric ratio (RAOT) of AOT averaged separately over the North and over the South Atlantic, was about 1.7. Seasonally, meridional AOT asymmetry over the Atlantic was the most pronounced between March and July, when dust presence is maximal (RAOT ranged from 2 to 2.4). There was no noticeable meridional aerosol asymmetry in total AOT from September to October. During this period the contribution of carbonaceous aerosols to total AOT in the South Atlantic was comparable to the contribution of dust aerosols to total AOT in the North Atlantic. During the same 10-year period, MODIS cloud fraction (CF) data showed that there was no noticeable asymmetry in meridional CF distribution in different seasons (the hemispheric ratio of CF ranged from 1.0 to 1.2). MODIS CF data illustrated significant cloud cover (CF of 0.7 – 0.9) with limited precipitation ability along the Saharan Air Layer. |
author |
Kishcha, Pavel Da Sliva, Arlindo Starobinets, Boris Long, Charles N. Kalashnikova, Olga Alpert, Pinhas |
author_facet |
Kishcha, Pavel Da Sliva, Arlindo Starobinets, Boris Long, Charles N. Kalashnikova, Olga Alpert, Pinhas |
author_sort |
Kishcha, Pavel |
title |
Saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical Atlantic Ocean |
title_short |
Saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical Atlantic Ocean |
title_full |
Saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical Atlantic Ocean |
title_fullStr |
Saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical Atlantic Ocean |
title_full_unstemmed |
Saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical Atlantic Ocean |
title_sort |
saharan dust as a causal factor of hemispheric asymmetry in aerosols and cloud cover over the tropical atlantic ocean |
publishDate |
2015 |
url |
http://www.osti.gov/servlets/purl/1221473 https://www.osti.gov/biblio/1221473 https://doi.org/10.1080/01431161.2015.1060646 |
long_lat |
ENVELOPE(12.615,12.615,65.816,65.816) |
geographic |
Merra |
geographic_facet |
Merra |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
http://www.osti.gov/servlets/purl/1221473 https://www.osti.gov/biblio/1221473 https://doi.org/10.1080/01431161.2015.1060646 doi:10.1080/01431161.2015.1060646 |
op_doi |
https://doi.org/10.1080/01431161.2015.1060646 |
container_title |
International Journal of Remote Sensing |
container_volume |
36 |
container_issue |
13 |
container_start_page |
3423 |
op_container_end_page |
3445 |
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1772817499246559232 |