Seasonality of sporadic physical processes driving temperature and nutrient high‐frequency variability in the coastal ocean off southeast Australia
Identifieur interne : 003D25 ( Main/Exploration ); précédent : 003D24; suivant : 003D26Seasonality of sporadic physical processes driving temperature and nutrient high‐frequency variability in the coastal ocean off southeast Australia
Auteurs : Vincent Rossi [Australie] ; Amandine Schaeffer [Australie] ; Julie Wood [Australie] ; Guillaume Galibert [Australie] ; Brad Morris [Australie] ; Joel Sudre [France] ; Moninya Roughan [Australie] ; Anya M. Waite [Australie]Source :
- Journal of Geophysical Research: Oceans [ 2169-9275 ] ; 2014-01.
Abstract
Physical processes forced by alongshore winds and currents are known to strongly influence the biogeochemistry of coastal waters. Combining in situ observations (moored platforms, hydrographic surveys) and satellite data (sea surface wind and sea surface height), we investigate the transient occurrence of wind‐driven upwelling/downwelling and current‐driven upwelling events off southeast Australia. Remote‐sensed indices are developed and calibrated with multiannual time series of in situ temperature and current measurements at two shelf locations. Based on archives up to 10 years long, climatological analyses of these indices reveal various latitudinal regimes with respect to seasonality, magnitude, duration of events, and their driving mechanisms (wind or current). Generally, downwelling‐favorable winds prevail in this region; however, we demonstrate that up to 10 wind‐driven upwelling days per month occur during spring/summer at 28–33.5°S and up to 5 days in summer further south. Current‐driven upwelling upstream of the East Australian Current separation zone (∼32°S) occurs twice as often as downstream. Using independent in situ data sets, we show that the response of the coastal ocean is consistent with our climatology of shelf processes: upwelling leads to a large range of temperatures and elevated nutrient concentrations on the shelf, maximized in the wind‐driven case, while downwelling results in destratified nutrient‐poor waters. The combination of these sporadic wind‐ and current‐driven processes may drive an important part of the high‐frequency variability of coastal temperature and nutrient content. Our results suggest that localized nutrient enrichment events of variable magnitude are favored at specific latitudes and seasons, potentially impacting coastal ecosystems.
Url:
DOI: 10.1002/2013JC009284
Affiliations:
- Australie, France
- Midi-Pyrénées, Nouvelle-Galles du Sud, Occitanie (région administrative)
- Sydney, Toulouse
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Combining in situ observations (moored platforms, hydrographic surveys) and satellite data (sea surface wind and sea surface height), we investigate the transient occurrence of wind‐driven upwelling/downwelling and current‐driven upwelling events off southeast Australia. Remote‐sensed indices are developed and calibrated with multiannual time series of in situ temperature and current measurements at two shelf locations. Based on archives up to 10 years long, climatological analyses of these indices reveal various latitudinal regimes with respect to seasonality, magnitude, duration of events, and their driving mechanisms (wind or current). Generally, downwelling‐favorable winds prevail in this region; however, we demonstrate that up to 10 wind‐driven upwelling days per month occur during spring/summer at 28–33.5°S and up to 5 days in summer further south. Current‐driven upwelling upstream of the East Australian Current separation zone (∼32°S) occurs twice as often as downstream. Using independent in situ data sets, we show that the response of the coastal ocean is consistent with our climatology of shelf processes: upwelling leads to a large range of temperatures and elevated nutrient concentrations on the shelf, maximized in the wind‐driven case, while downwelling results in destratified nutrient‐poor waters. The combination of these sporadic wind‐ and current‐driven processes may drive an important part of the high‐frequency variability of coastal temperature and nutrient content. Our results suggest that localized nutrient enrichment events of variable magnitude are favored at specific latitudes and seasons, potentially impacting coastal ecosystems.</div></front></TEI><affiliations><list><country><li>Australie</li><li>France</li></country><region><li>Midi-Pyrénées</li><li>Nouvelle-Galles du Sud</li><li>Occitanie (région administrative)</li></region><settlement><li>Sydney</li><li>Toulouse</li></settlement></list><tree><country name="Australie"><region name="Nouvelle-Galles du Sud"><name sortKey="Rossi, Vincent" sort="Rossi, Vincent" uniqKey="Rossi V" first="Vincent" last="Rossi">Vincent Rossi</name></region><name sortKey="Galibert, Guillaume" sort="Galibert, Guillaume" uniqKey="Galibert G" first="Guillaume" last="Galibert">Guillaume Galibert</name><name sortKey="Morris, Brad" sort="Morris, Brad" uniqKey="Morris B" first="Brad" last="Morris">Brad Morris</name><name sortKey="Roughan, Moninya" sort="Roughan, Moninya" uniqKey="Roughan M" first="Moninya" last="Roughan">Moninya Roughan</name><name sortKey="Schaeffer, Amandine" sort="Schaeffer, Amandine" uniqKey="Schaeffer A" first="Amandine" last="Schaeffer">Amandine Schaeffer</name><name sortKey="Waite, Anya M" sort="Waite, Anya M" uniqKey="Waite A" first="Anya M." last="Waite">Anya M. Waite</name><name sortKey="Wood, Julie" sort="Wood, Julie" uniqKey="Wood J" first="Julie" last="Wood">Julie Wood</name></country><country name="France"><region name="Occitanie (région administrative)"><name sortKey="Sudre, Joel" sort="Sudre, Joel" uniqKey="Sudre J" first="Joel" last="Sudre">Joel Sudre</name></region></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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