ePIC

Substantial advective iron loss diminishes phytoplankton production in the Antarctic Zone

Edit Item Edit Item

General Information:

Citation:
Hoppema, M. , Baar, H. J. W. d. , Fahrbach, E. , Hellmer, H. and Klein, B. (2003): Substantial advective iron loss diminishes phytoplankton production in the Antarctic Zone , Global Biogeochemical Cycles, 17(1), 25 , pp. 1-9 . doi: 10.1029/2002GB001957
Cite this page as:
DOI:
Official URL:
Contact Email:
Download:

Supplementary Information:

Abstract:

Upon one decade of research it is a well established fact that iron limits photosynthetic CO2 fixation and phytoplankton growth in the Southern Ocean - intense blooms are scarse. However, the input of iron to the Southern Ocean is considerable. An important factor for diminished phytoplankton production refers to the meridional circulation of the Southern Ocean. Intense upwelling of Upper Circumpolar Deep Water (UCDW) causes a large iron flux into the surface layer. However, the main entrainment of upwelled UCDW into the surface layer occurs in autumn and winter which strongly restricts the usefullness of iron supply for phytoplankton due to unfavorable light conditions. Moreover, the meridional transport within the Ekman layer is intense enough to export at least 25% of the iron input away form the Antarctic Zone before it can be used by phytoplankton. This also depresses the potential phytoplankton primary production by at least 25%. Most iron that crosses the Polar Front unused leaves the surface ocean north of the Polar Front because the surface water participates in Antarctic Intermediate Water/Mode Water formation.

Further Details:

Imprint
AWI
Policies:
read more
OAI 2.0:
http://epic.awi.de/cgi/oai2
ePIC is powered by:
EPrints 3