Biogeochemical modelling of the feedback between ocean biota and climate at polar latitudes




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Biogeochemical modelling of the feedback between ocean biota and climate at polar latitudes

Entry ID: ASAC_2584

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Summary

Abstract: Metadata record for data from ASAC Project 2584
See the link below for public details on this project.

The Southern Ocean plays a significant role in the biogeochemical cycling of sulphur due to high spring-summer fluxes of dimethylsulfide (DMS), particularly south of 60 degrees S. Recent DMS flux perturbation simulations have recently highlighted the key role of the SO between 50-70 degrees S in ... the DMS-climate feedback hypothesis [Gabric et al., 2003; Gabric et al., 2004]. This project examines the interactions and feedback between marine polar plankton and global climate through the use of biogeochemical and global climate models, and explores the sensitivity of climate to the current and future biogenic production of dimethylsulphide at polar latitudes.

This was a modelling project, and as such did not collect any data of its own.

Taken from the abstracts of the referenced papers:

The global climate is intimately connected to changes in the polar oceans. The variability of sea ice coverage affects deep-water formations and large-scale thermohaline circulation patterns. The polar radiative budget is sensitive to sea-ice loss and consequent surface albedo changes. Aerosols and polar cloud microphysics are crucial players in the radioactive energy balance of the Arctic Ocean. The main biogenic source of sulfate aerosols to the atmosphere above remote seas is dimethylsulfide (DMS).
Recent research suggests the flux of DMS to the Arctic atmosphere may change markedly under global warming. This paper describes climate data and DMS production (based on the five years from 1998 to 2002) in the region of the Barents Sea (30-35 degrees E and 70-80 degrees N). A DMS model is introduced together with an updated calibration method. A genetic algorithm is used to calibrate the chlorophyll-a (CHL) measurements (based on satellite SeaWiFS data) and DMS content (determined from cruise data collected in the Arctic). Significant interannual variation of the CHL amount leads to significant interannual variability in the observed and modelled production of DMS in the study region. Strong DMS production in 1998 could have been caused by a large amount of ice algae being released in the southern region.
Forcings from a general circulation model (CSIRO Mk3) were applied to the calibrated DMS model to predict the zonal mean sea-to-air flux of DMS for contemporary and enhanced greenhouse conditions at 70-80 degrees N. It was found that significantly decreasing ice coverage, increasing sea surface temperature and decreasing mixed-layer depth could lead to annual DMS flux increases of more than 100% by the time of equivalent CO2 tripling (the year 2080). This significant perturbation in the aerosol climate could have a
large impact on the regional Arctic heat budget and consequences for global warming.

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The response of oceanic phytoplankton to climate forcing in the Arctic Ocean has attracted increasing attention due to its special geographical position and potential susceptibility to global warming. Here, we examine the relationship between satellite derived (sea-viewing wide field-of-view sensor, SeaWiFS) surface chlorophyll-a (CHL) distribution and climatic conditions in the Barents Sea (30-35 degrees E, 70-80 degrees N) for the period 1998-2002. We separately examined the regions north and south of the Polar Front (~76 degrees N). Although field data are rather limited, the satellite CHL distribution was generally consistent with cruise observations. The temporal and spatial distribution of CHL was strongly influenced by the light regime, mixed layer depth, wind speed and ice cover. Maximum CHL values were found in the marginal sea-ice zone (72-73 degrees N) and not in the ice-free region further south (70-71 degrees N). This indicates that melt-water is an important contributor to higher CHL production. The vernal phytoplankton bloom generally started in late March, reaching its peak in late April.
A second, smaller CHL peak occurred regularly in late summer (September). Of the 5 years, 2002 had the highest CHL production in the southern region, likely
due to earlier ice melting and stronger solar irradiance in spring and summer.

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Arctic ecosystems and global climate are closely related. This paper studies the distributions and the coupling relationship between Chlorophyll a (Chl a) and aerosol optical thickness (AOD) in Greenland Sea (10 degrees W - 10 degrees E, 70 degrees N - 85 degrees N) during 2003-2009 using satellite ocean colour data from MODIS Aqua. The regression analysis of EViews shows that Chl a and AOD are correlated with a time lag. Based on the lag of Chl a and AOD, co-integration inquiry finds that there is co-integration between them, which means that they will have a long-term equilibrium relationship. In general, Chl a starts from March, and gradually increases to a peak in July. The peak of AOD is usually in May, 11 weeks before Chl a. After shifting the time lag, the correlation between Chl a and AOD is 0.98 in the spring in 80 degrees N - 85 degrees N. Apart from the year of 2005, when Chl a and AOD had no time lag, the other years' intervals increased about 6 weeks within the 7 years. The peaks of AOD shifted one and a half months ahead, while Chl a also shifted about two months ahead. In northern part (75 degrees N - 85 degrees N), Chl a and AOD were much higher in the summer and autumn of 2009 than those in other years. The reason could be the much larger ice melting and higher AOD. The results indicate that the global warming has significant impact on the ecosystem in the Arctic Ocean.

Related URL

Link: VIEW PROJECT HOME PAGE

Description: Public information for ASAC project 2584

Geographic Coverage

(Click for Interactive Map)

Spatial coordinates

N: -50.0

S: -70.0

E: 180.0

W: -180.0

(View on interactive map)

N: 85.0

S: 70.0

E: 35.0

W: -10.0

(View on interactive map)

Temporal Coverage

Start Date: 2004-10-01

Stop Date: 2007-03-31

Location Keywords

OCEAN > ARCTIC OCEAN

OCEAN > SOUTHERN OCEAN

Science Keywords

OCEANS > OCEAN CHEMISTRY > NUTRIENTS

OCEANS > OCEAN CHEMISTRY > PIGMENTS > CHLOROPHYLL

OCEANS > OCEAN CHEMISTRY > CHLOROPHYLL

ISO Topic Category

OCEANS

Quality The Dates provided in temporal coverage are approximate only, and represent the beginning and end of the 2004 - 2007 Antarctic seasons.
The latitudes and longitudes provided in spatial coverage are approximate only.

Access Constraints PDF copies of three of the referenced papers are available for download to AAD staff only at the provided URL.

Use Constraints This data set conforms to the PICCCBY Attribution License
(http://creativecommons.org/licenses/by/3.0/).

Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=ASAC_2584 when using these data.

This "Biogeochemical modelling of the feedback between ocean biota and climate at polar latitudes" is licensed under a Creative Commons Attribution 3.0 Unported License.

Ancillary Keywords

dms

sulphur

dimethylsulfide

chlorophyll a

Data Set Progress

COMPLETE

Data Center

Australian Antarctic Data Centre, Australia

Data Center URL: http://data.aad.gov.au

Data Center Personnel
Name: DATA OFFICER AADC Phone: +61 3 6232 3244 Fax: +61 3 6232 3351 Email: metadata at aad.gov.au Contact Address: Australian Antarctic Division 203 Channel Highway City: Kingston Province or State: Tasmania Postal Code: 7050 Country: Australia

Distribution

Distribution Media: HTTP

Distribution Size: 2 MB

Distribution Format: pdf

Fees: Free

Personnel

ALBERT GABRIC

Role: INVESTIGATOR

Role: TECHNICAL CONTACT

Phone: +61 7 3875 7513

Fax: +61 7 3875 7459

Email: a.gabric at mailbox.gu.edu.au

Contact Address:

GRIFFITH UNIVERSITY

FACULTY OF ENVIRONMENTAL SCIENCE

City: NATHAN

Province or State: QLD

Postal Code: 4111

Country: Australia

DAVE CONNELL

Role: DIF AUTHOR

Phone: +61 3 6232 3244

Fax: +61 3 6232 3351

Email: dave.connell at aad.gov.au

Contact Address:

Australian Antarctic Division

203 Channel Highway

City: Kingston

Province or State: Tasmania

Postal Code: 7050

Country: Australia

Publications/References

Qu Bo, Lu Hailang, AlbertJ.Gabric, Lin Daorong, Qian Feng, Zhao Weihua (2011), Using MODIS satellite data to analyse the relationship between chlorophyll a and aerosol optical depth in the Greenland Sea., Chinese Journal of Polar Research, 23, 1, 68-76

Creation and Review Dates

DIF Creation Date: 2006-07-27

Last DIF Revision Date: 2011-11-29

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