Effects of typhoons on primary production and dissolved oxygen in the East China Sea

Previous investigations confirm that typhoons deliver both dissolved oxygen and nutrient sources via promoting vertical/lateral exchanges between water masses. The former one replenishes oxygen for the bottom water and prevents persistent oxygen depletion, while the latter one facilitates primary pr...

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Published inFrontiers in Marine Science Vol. 11
Main Authors Yang, Wen, Wu, Haokun, Zhang, Wenxia
Format Journal Article
LanguageEnglish
Published Lausanne Frontiers Research Foundation 22.03.2024
Frontiers Media S.A
Subjects
Biogeochemistry
Bottom water
Changjiang estuary
Chlorophyll
Climate change
coastal hypoxia
Cyclones
Deoxygenation
Dissolved oxygen
dissolved oxygen budget
Estuaries
Estuarine dynamics
Hurricanes
Hypoxia
Nutrient sources
Oxygen
Oxygen consumption
Oxygen depletion
Plankton
Primary production
Tropical cyclones
typhoon
Typhoons
Water masses
East China Sea
China
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Abstract Previous investigations confirm that typhoons deliver both dissolved oxygen and nutrient sources via promoting vertical/lateral exchanges between water masses. The former one replenishes oxygen for the bottom water and prevents persistent oxygen depletion, while the latter one facilitates primary production and subsequent subsurface oxygen consumption. However, it is left unknown if typhoons ultimately result in net gain or loss of dissolved oxygen during the passage. Tropical cyclone information, satellite observations, and numerical simulations were used to investigate the response of primary production and dissolved oxygen dynamics to typhoons. Results imply that both typhoon intensity, and distance between typhoon track and the Changjiang estuary control the magnitude of responses in primary production, air-sea oxygen flux, advection-induced oxygen variation, and oxygen consumption variation. The model-based oxygen budget analysis indicated that oxygen content increased after the passage of all typhoons occurred between 2011-2020. The findings in this study suggest that typhoons ultimately result in net gain of oxygen. The increased strength and frequency of typhoon in the warming future would play an important role in counteracting deoxygenation, which is likely to slow down the pace of deterioration of the seasonal hypoxia in this region.
AbstractList Previous investigations confirm that typhoons deliver both dissolved oxygen and nutrient sources via promoting vertical/lateral exchanges between water masses. The former one replenishes oxygen for the bottom water and prevents persistent oxygen depletion, while the latter one facilitates primary production and subsequent subsurface oxygen consumption. However, it is left unknown if typhoons ultimately result in net gain or loss of dissolved oxygen during the passage. Tropical cyclone information, satellite observations, and numerical simulations were used to investigate the response of primary production and dissolved oxygen dynamics to typhoons. Results imply that both typhoon intensity, and distance between typhoon track and the Changjiang estuary control the magnitude of responses in primary production, air-sea oxygen flux, advection-induced oxygen variation, and oxygen consumption variation. The modelbased oxygen budget analysis indicated that oxygen content increased after the passage of all typhoons occurred between 2011-2020. The findings in this study suggest that typhoons ultimately result in net gain of oxygen. The increased strength and frequency of typhoon in the warming future would play an important role in counteracting deoxygenation, which is likely to slow down the pace of deterioration of the seasonal hypoxia in this region.
Previous investigations confirm that typhoons deliver both dissolved oxygen and nutrient sources via promoting vertical/lateral exchanges between water masses. The former one replenishes oxygen for the bottom water and prevents persistent oxygen depletion, while the latter one facilitates primary production and subsequent subsurface oxygen consumption. However, it is left unknown if typhoons ultimately result in net gain or loss of dissolved oxygen during the passage. Tropical cyclone information, satellite observations, and numerical simulations were used to investigate the response of primary production and dissolved oxygen dynamics to typhoons. Results imply that both typhoon intensity, and distance between typhoon track and the Changjiang estuary control the magnitude of responses in primary production, air-sea oxygen flux, advection-induced oxygen variation, and oxygen consumption variation. The model-based oxygen budget analysis indicated that oxygen content increased after the passage of all typhoons occurred between 2011-2020. The findings in this study suggest that typhoons ultimately result in net gain of oxygen. The increased strength and frequency of typhoon in the warming future would play an important role in counteracting deoxygenation, which is likely to slow down the pace of deterioration of the seasonal hypoxia in this region.
Author Yang, Wen
Zhang, Wenxia
Wu, Haokun
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Snippet Previous investigations confirm that typhoons deliver both dissolved oxygen and nutrient sources via promoting vertical/lateral exchanges between water masses....
SourceID doaj
proquest
crossref
SourceType Open Website
Aggregation Database
SubjectTerms Biogeochemistry
Bottom water
Changjiang estuary
Chlorophyll
Climate change
coastal hypoxia
Cyclones
Deoxygenation
Dissolved oxygen
dissolved oxygen budget
Estuaries
Estuarine dynamics
Hurricanes
Hypoxia
Nutrient sources
Oxygen
Oxygen consumption
Oxygen depletion
Plankton
Primary production
Tropical cyclones
typhoon
Typhoons
Water masses
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Title Effects of typhoons on primary production and dissolved oxygen in the East China Sea
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