
NSF Org: |
OCE Division Of Ocean Sciences |
Recipient: |
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Initial Amendment Date: | March 21, 2008 |
Latest Amendment Date: | March 21, 2008 |
Award Number: | 0743551 |
Award Instrument: | Standard Grant |
Program Manager: |
Donald L. Rice
OCE Division Of Ocean Sciences GEO Directorate for Geosciences |
Start Date: | April 1, 2008 |
End Date: | March 31, 2011 (Estimated) |
Total Intended Award Amount: | $130,119.00 |
Total Awarded Amount to Date: | $130,119.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
2425 CAMPUS RD SINCLAIR RM 1 HONOLULU HI US 96822-2247 (808)956-7800 |
Sponsor Congressional District: |
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Primary Place of Performance: |
2425 CAMPUS RD SINCLAIR RM 1 HONOLULU HI US 96822-2247 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | Chemical Oceanography |
Primary Program Source: |
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Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
Ocean-atmosphere exchange of the radiatively active biogenic trace gas, dimethylsulfide (DMS), is a major source of atmospheric sulfate aerosols: a key element of the global climate system. Climate affects this exchange by determining the physical-chemical characteristics of the upper ocean, thus shaping the marine planktonic ecosystem and the source strength of DMS. Attaining a more complete understanding of the interactions between the marine ecosystem and climate is an exciting challenge, which has barely begun to be explored.
In this study, researchers at the Bigelow Laboratory for Ocean Sciences and the University of Hawaii at Manoa will examine the impact of light levels, sea surface temperature, upwelled nutrients, and winds on the production of DMS and its emission to the atmosphere. These critical linkages in the CLAW Hypothesis potentially determine whether this physical-biological feedback will be positive or negative. Does a modest change in PAR and UV increase or decrease DMS production and emission to the atmosphere? This will be studied in the context of complementary VOCALS projects studying atmospheric portions of CLAW: the oxidation of DMS to sulfate aerosols and their impact on clouds and the Earth?s radiation budget. Evaluating the magnitude and sign of such biotic feedbacks is of major societal and scientific importance. Specifically, the research will address the following themes in the South East Pacific (SEP) waters: (a) how far does the biogeochemical impact of upwelling on DMS production and air-sea flux extend offshore, (b) how do fewer clouds affect biological DMS production and SW concentrations, and (c) How do spatial gradients of SW DMS concentration and flux-controlling factors (e.g., winds) affect DMS fluxes to the atmosphere. The ultimate goal, in the synthesis phase of VOCALS REx and in collaboration with other participating investigators, would be to determine the significance of biotic feedbacks in controlling the radiation budget of the Southeast Pacific.
The project will have several broader impacts. Training of one postdoctoral associate (Bigelow) and one graduate student (Hawaii) will be supported. In addition, the Bigelow PI will continue her participation in rural (local) K-8 programs as well as in the Grant Management Advisory Panel for the NSF ITEST grant Communities for Rural Education, Stewardship, and Technology led by the Island Institute (Rockland, ME). The Hawaii PI will use this data as examples (for problem sets and test questions) in his undergraduate and graduate level oceanography and atmospheric chemistry classes. Both PIs will participate in the VOCALS REx-coordinated broader outreach activities.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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