Carbon-based ocean productivity and phytoplankton physiology from space

Boss, Emmanuel; Shea, Donald M.; Siegel, David A.; Behrenfeld, Michael J.

doi:10.1029/2004GB002299

Record: found
Abstract: not found
Article: not found

Carbon-based ocean productivity and phytoplankton physiology from space : PHYTOPLANKTON GROWTH RATES AND OCEAN PRODUCTIVITY

Author(s): Michael J. Behrenfeld , Emmanuel Boss , David A. Siegel , Donald M. Shea

Publication date Created: March 2005

Publication date (Print): March 2005

Journal: Global Biogeochemical Cycles

Publisher: American Geophysical Union (AGU)

Read this article at

ScienceOpenPublisher

Bookmark

There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

Abstract

Related collections

Most cited references 34

Record: found
Abstract: not found
Article: not found

Oceanic primary production: 2. Estimation at global scale from satellite (Coastal Zone Color Scanner) chlorophyll

Andre Morel, David Antoine, Jean-Michel André (1996)

0 comments Cited 259 times – based on 0 reviews      Review now

Bookmark

Record: found
Abstract: not found
Article: not found

Biological and Chemical Response of the Equatorial Pacific Ocean to the 1997-98 El Niño

F. Chavez (1999)

0 comments Cited 188 times – based on 0 reviews      Review now

Bookmark

Record: found
Abstract: found
Article: not found

Biospheric primary production during an ENSO transition.

M J Behrenfeld, J T Randerson, C R McClain … (2001)

The Sea-viewing Wide Field-of-view Sensor (SeaWiFS) provides global monthly measurements of both oceanic phytoplankton chlorophyll biomass and light harvesting by land plants. These measurements allowed the comparison of simultaneous ocean and land net primary production (NPP) responses to a major El Niño to La Niña transition. Between September 1997 and August 2000, biospheric NPP varied by 6 petagrams of carbon per year (from 111 to 117 petagrams of carbon per year). Increases in ocean NPP were pronounced in tropical regions where El Niño-Southern Oscillation (ENSO) impacts on upwelling and nutrient availability were greatest. Globally, land NPP did not exhibit a clear ENSO response, although regional changes were substantial.