The flux of soluble organic‐iron(III) complexes from sediments represents a source of stable iron(III) to estuarine waters and to the continental shelf

By  

LIMNOLOGY AND OCEANOGRAPHY, Vol. 56, Iss. 5, 2011-09 ,pp. : 1811-1823

John Wiley & Sons Inc

Access to resources Recommend Favorite

Baroclinic energy flux at the continental shelf edge modified by wind‐mixing

By  

GEOPHYSICAL RESEARCH LETTERS, Vol. 42, Iss. 6, 2015-03 ,pp. : 1826-1833

John Wiley & Sons Inc

Access to resources Recommend Favorite

The carbon dioxide system on the Mississippi River‐dominated continental shelf in the northern Gulf of Mexico: 1. Distribution and air‐sea CO2 flux

By  

JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, Vol. 120, Iss. 3, 2015-03 ,pp. : 1429-1445

John Wiley & Sons Inc

Access to resources Recommend Favorite

Validation of the summertime surface energy budget of Larsen C Ice Shelf (Antarctica) as represented in three high‐resolution atmospheric models

By  

JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES, Vol. 120, Iss. 4, 2015-02 ,pp. : 1335-1347

John Wiley & Sons Inc

Access to resources Recommend Favorite

Reassembling Gondwana: A new high quality constraint from vibroseis exploration of the sub‐ice shelf geology of the East Antarctic continental margin

By  

JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH, Vol. 119, Iss. 12, 2014-12 ,pp. : 9171-9182

John Wiley & Sons Inc

Access to resources Recommend Favorite