Constraining oceanic dust deposition using surface
[1] We use measurements of ocean surface dissolved Al, a global Biogeochemical Elemental Cycling (BEC) ocean model, and the global Dust Entrainment and Deposition (DEAD) model to constrain dust deposition to the oceans. Our Al database contains all available measurements with best coverage in the At...
Main Authors: | , , , , |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Subjects: | |
Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.159.9790 http://dust.ess.uci.edu/ppr/ppr_HMZ08.pdf |
id |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.159.9790 |
---|---|
record_format |
openpolar |
spelling |
ftciteseerx:oai:CiteSeerX.psu:10.1.1.159.9790 2023-05-15T18:25:28+02:00 Constraining oceanic dust deposition using surface Qin Han J. Keith Moore Charles Zender Chris Measures David Hydes The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.159.9790 http://dust.ess.uci.edu/ppr/ppr_HMZ08.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.159.9790 http://dust.ess.uci.edu/ppr/ppr_HMZ08.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://dust.ess.uci.edu/ppr/ppr_HMZ08.pdf text ftciteseerx 2016-01-07T15:39:06Z [1] We use measurements of ocean surface dissolved Al, a global Biogeochemical Elemental Cycling (BEC) ocean model, and the global Dust Entrainment and Deposition (DEAD) model to constrain dust deposition to the oceans. Our Al database contains all available measurements with best coverage in the Atlantic. Vertical profiles and seasonal data exist in limited regions. Observations show that surface dissolved Al is distributed similarly to the dust deposition predicted by DEAD and other models. There is an equatorial Atlantic Al maximum that decreases toward higher latitudes. There are high Al concentrations in the Mediterranean Sea and the Arabian Sea and low concentrations in the Pacific and the Southern Ocean. The ocean basins maintain more distinct Al profiles than Fe profiles in the upper ocean, consistent with a weaker biological influence on Al than Fe. The BEC-predicted surface dissolved Al compares relatively well with observations. The Al distribution reflects the combined effects of Al input from dust and Al removal by particle scavenging and biological uptake by diatoms. Model-observed biases suggest a southward shift of maximum dust deposition compared to current dust model Text Southern Ocean Unknown Pacific Southern Ocean |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
[1] We use measurements of ocean surface dissolved Al, a global Biogeochemical Elemental Cycling (BEC) ocean model, and the global Dust Entrainment and Deposition (DEAD) model to constrain dust deposition to the oceans. Our Al database contains all available measurements with best coverage in the Atlantic. Vertical profiles and seasonal data exist in limited regions. Observations show that surface dissolved Al is distributed similarly to the dust deposition predicted by DEAD and other models. There is an equatorial Atlantic Al maximum that decreases toward higher latitudes. There are high Al concentrations in the Mediterranean Sea and the Arabian Sea and low concentrations in the Pacific and the Southern Ocean. The ocean basins maintain more distinct Al profiles than Fe profiles in the upper ocean, consistent with a weaker biological influence on Al than Fe. The BEC-predicted surface dissolved Al compares relatively well with observations. The Al distribution reflects the combined effects of Al input from dust and Al removal by particle scavenging and biological uptake by diatoms. Model-observed biases suggest a southward shift of maximum dust deposition compared to current dust model |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Qin Han J. Keith Moore Charles Zender Chris Measures David Hydes |
spellingShingle |
Qin Han J. Keith Moore Charles Zender Chris Measures David Hydes Constraining oceanic dust deposition using surface |
author_facet |
Qin Han J. Keith Moore Charles Zender Chris Measures David Hydes |
author_sort |
Qin Han |
title |
Constraining oceanic dust deposition using surface |
title_short |
Constraining oceanic dust deposition using surface |
title_full |
Constraining oceanic dust deposition using surface |
title_fullStr |
Constraining oceanic dust deposition using surface |
title_full_unstemmed |
Constraining oceanic dust deposition using surface |
title_sort |
constraining oceanic dust deposition using surface |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.159.9790 http://dust.ess.uci.edu/ppr/ppr_HMZ08.pdf |
geographic |
Pacific Southern Ocean |
geographic_facet |
Pacific Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
http://dust.ess.uci.edu/ppr/ppr_HMZ08.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.159.9790 http://dust.ess.uci.edu/ppr/ppr_HMZ08.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766206949231165440 |