Basin scale estimates of sea surface nitrate and new production from remotely sensed sea surface temperature and chlorophyll

The highly variable nature of T-N relationships in oceanic waters has restricted nitrate (N) measurements from remotely sensed sea surface temperature (SST) to small time and space domains. Here we show that if changes in T-N relationships resulting from phytoplankton (chlorophyll a) are taken into account, remote sensing can be exploited to provide high resolution maps of sea surface nitrate (SSN) that are valid over much larger scales than has been previously possible. We illustrate the potential of the method for monitoring basin scale, interannual variations in SSN in the north Pacific Ocean using co-registered imagery of SST and chl a and demonstrate the usefulness of such data for estimating basin scale annual new production.

[1]  Janet W. Campbell,et al.  New production in the North Atlantic derived from seasonal patterns of surface chlorophyll , 1992 .

[2]  Hiroshi Murakami,et al.  The sea surface temperature product algorithm of the Ocean Color and Temperature Scanner (OCTS) and its accuracy , 1998 .

[3]  A. Vézina,et al.  Biological Production of the Oceans - the Case for a Consensus , 1989 .

[4]  David M. Karl,et al.  VERTEX: carbon cycling in the northeast Pacific , 1987 .

[5]  V. Strass,et al.  New production in the summer revealed by the meridional slope of the deep chlorophyll maximum , 1991 .

[6]  Annick Bricaud,et al.  Modeling new production in upwelling centers: A case study of modeling new production from remotely sensed temperature and color , 1989 .

[7]  D. M. Glover,et al.  Dynamics of the transition zone in coastal zone color scanner-sensed ocean color in the North Pacific during oceanographic spring , 1994 .

[8]  B. Peterson,et al.  Particulate organic matter flux and planktonic new production in the deep ocean , 1979, Nature.

[9]  J. Ishizaka,et al.  Meridional distribution and carbon biomass of autotrophic picoplankton in the Central North Pacific Ocean during Late Northern Summer 1990 , 1994 .

[10]  Masanobu Shimada,et al.  Calibration and validation of the ocean color version-3 product from ADEOS OCTS , 1998 .

[11]  T. Platt,et al.  An estimate of global primary production in the ocean from satellite radiometer data , 1995 .

[12]  T. Platt,et al.  Basin-scale estimates of oceanic primary production by remote sensing - The North Atlantic , 1991 .

[13]  Francisco P. Chavez,et al.  Regulation of primary productivity rate in the equatorial Pacific , 1991 .

[14]  Hiromi Oaku,et al.  A method for estimating sea surface nitrate concentrations from remotely sensed SST and chlorophyll a-a case study for the north Pacific Ocean using OCTS/ADEOS data , 1999, IEEE Trans. Geosci. Remote. Sens..

[15]  Thomas M. Powell,et al.  Ecological dynamics in the subarctic Pacific, a possibly iron-limited ecosystem , 1991 .

[16]  T. Platt,et al.  Estimation of new production in the ocean by compound remote sensing , 1991, Nature.

[17]  Samuel E. Buttrey,et al.  Temperature‐nitrate relationships in the central and eastern tropical Pacific , 1996 .

[18]  T. Platt,et al.  Vertical Nitrate Fluxes in the Oligotrophic Ocean , 1986, Science.

[19]  Daniel Kamykowski,et al.  Predicting plant nutrient concentrations from temperature and sigma-t in the upper kilometer of the world ocean , 1986 .

[20]  Richard T. Barber,et al.  Origin and maintenance of a high nitrate condition in the equatorial Pacific , 1996 .

[21]  C. Garside,et al.  Euphotic-zone nutrient algorithms for the NABE and EqPac study sites , 1995 .

[22]  Tokihiro Kono Modification of the Oyashio Water in the Hokkaido and Tohoku areas , 1997 .

[23]  S. Noriki,et al.  Particulate fluxes and major components of settling particles from sediment trap experiments in the Pacific Ocean , 1986 .