ic rct stations than at the warm “spring ” ones. This probably results from the enhanced ice permeability as spring arrives, which allows deposition, (2) upwelling and turbulent diffusion, (3) sediment resuspension and lateral advection, and (4) melting sea ice and icebergs (Löscher et al., 1997;...

Full description

Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Iron biogeochemistry
Fe inputs
Sea ice
East Antarctica
Antarc*
Antarctica
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.577.830
http://dev.ulb.ac.be/glaciol/articles/Lannuzel_2007_Marine Chemistry_Distribution and biogeochemical behaviour of iron in the East Antarctic sea ice.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.577.830
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.577.830 2023-05-15T14:04:40+02:00 The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.577.830 http://dev.ulb.ac.be/glaciol/articles/Lannuzel_2007_Marine Chemistry_Distribution and biogeochemical behaviour of iron in the East Antarctic sea ice.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.577.830 http://dev.ulb.ac.be/glaciol/articles/Lannuzel_2007_Marine Chemistry_Distribution and biogeochemical behaviour of iron in the East Antarctic sea ice.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://dev.ulb.ac.be/glaciol/articles/Lannuzel_2007_Marine Chemistry_Distribution and biogeochemical behaviour of iron in the East Antarctic sea ice.pdf Iron biogeochemistry Fe inputs Sea ice East Antarctica text ftciteseerx 2016-01-08T12:50:20Z ic rct stations than at the warm “spring ” ones. This probably results from the enhanced ice permeability as spring arrives, which allows deposition, (2) upwelling and turbulent diffusion, (3) sediment resuspension and lateral advection, and (4) melting sea ice and icebergs (Löscher et al., 1997; Text Antarc* Antarctica East Antarctica Sea ice Unknown East Antarctica
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Iron biogeochemistry
Fe inputs
Sea ice
East Antarctica
spellingShingle Iron biogeochemistry
Fe inputs
Sea ice
East Antarctica
topic_facet Iron biogeochemistry
Fe inputs
Sea ice
East Antarctica
description ic rct stations than at the warm “spring ” ones. This probably results from the enhanced ice permeability as spring arrives, which allows deposition, (2) upwelling and turbulent diffusion, (3) sediment resuspension and lateral advection, and (4) melting sea ice and icebergs (Löscher et al., 1997;
author2 The Pennsylvania State University CiteSeerX Archives
format Text
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.577.830
http://dev.ulb.ac.be/glaciol/articles/Lannuzel_2007_Marine Chemistry_Distribution and biogeochemical behaviour of iron in the East Antarctic sea ice.pdf
geographic East Antarctica
geographic_facet East Antarctica
genre Antarc*
Antarctica
East Antarctica
Sea ice
genre_facet Antarc*
Antarctica
East Antarctica
Sea ice
op_source http://dev.ulb.ac.be/glaciol/articles/Lannuzel_2007_Marine Chemistry_Distribution and biogeochemical behaviour of iron in the East Antarctic sea ice.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.577.830
http://dev.ulb.ac.be/glaciol/articles/Lannuzel_2007_Marine Chemistry_Distribution and biogeochemical behaviour of iron in the East Antarctic sea ice.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766275880053637120

Similar Items