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Forecasting Ocean Chlorophyll in the Equatorial Pacific

Using a global ocean biogeochemical model combined with a forecast of physical oceanic and atmospheric variables from the NASA Global Modeling and Assimilation Office, we assess the skill of a chlorophyll concentrations forecast in the Equatorial Pacific for the period 2012–2015 with a focus on the...

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Autores principales: Rousseaux, Cecile S., Gregg, Watson W.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: 2017
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5747543/
https://www.ncbi.nlm.nih.gov/pubmed/29291196
http://dx.doi.org/10.3389/fmars.2017.00236
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author Rousseaux, Cecile S.
Gregg, Watson W.
author_facet Rousseaux, Cecile S.
Gregg, Watson W.
author_sort Rousseaux, Cecile S.
collection PubMed
description Using a global ocean biogeochemical model combined with a forecast of physical oceanic and atmospheric variables from the NASA Global Modeling and Assimilation Office, we assess the skill of a chlorophyll concentrations forecast in the Equatorial Pacific for the period 2012–2015 with a focus on the forecast of the onset of the 2015 El Niño event. Using a series of retrospective 9-month hindcasts, we assess the uncertainties of the forecasted chlorophyll by comparing the monthly total chlorophyll concentration from the forecast with the corresponding monthly ocean chlorophyll data from the Suomi-National Polar-orbiting Partnership Visible Infrared Imaging Radiometer Suite (S-NPP VIIRS) satellite. The forecast was able to reproduce the phasing of the variability in chlorophyll concentration in the Equatorial Pacific, including the beginning of the 2015–2016 El Niño. The anomaly correlation coefficient (ACC) was significant (p < 0.05) for forecast at 1-month (R = 0.33), 8-month (R = 0.42) and 9-month (R = 0.41) lead times. The root mean square error (RMSE) increased from 0.0399 μg chl L(−1) for the 1-month lead forecast to a maximum of 0.0472 μg chl L(−1) for the 9-month lead forecast indicating that the forecast of the amplitude of chlorophyll concentration variability was getting worse. Forecasts with a 3-month lead time were on average the closest to the S-NPP VIIRS data (23% or 0.033 μg chl L(−1)) while the forecast with a 9-month lead time were the furthest (31% or 0.042 μg chl L(−1)). These results indicate the potential for forecasting chlorophyll concentration in this region but also highlights various deficiencies and suggestions for improvements to the current biogeochemical forecasting system. This system provides an initial basis for future applications including the effects of El Niño events on fisheries and other ocean resources given improvements identified in the analysis of these results.
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spelling pubmed-57475432017-12-29 Forecasting Ocean Chlorophyll in the Equatorial Pacific Rousseaux, Cecile S. Gregg, Watson W. Front Mar Sci Article Using a global ocean biogeochemical model combined with a forecast of physical oceanic and atmospheric variables from the NASA Global Modeling and Assimilation Office, we assess the skill of a chlorophyll concentrations forecast in the Equatorial Pacific for the period 2012–2015 with a focus on the forecast of the onset of the 2015 El Niño event. Using a series of retrospective 9-month hindcasts, we assess the uncertainties of the forecasted chlorophyll by comparing the monthly total chlorophyll concentration from the forecast with the corresponding monthly ocean chlorophyll data from the Suomi-National Polar-orbiting Partnership Visible Infrared Imaging Radiometer Suite (S-NPP VIIRS) satellite. The forecast was able to reproduce the phasing of the variability in chlorophyll concentration in the Equatorial Pacific, including the beginning of the 2015–2016 El Niño. The anomaly correlation coefficient (ACC) was significant (p < 0.05) for forecast at 1-month (R = 0.33), 8-month (R = 0.42) and 9-month (R = 0.41) lead times. The root mean square error (RMSE) increased from 0.0399 μg chl L(−1) for the 1-month lead forecast to a maximum of 0.0472 μg chl L(−1) for the 9-month lead forecast indicating that the forecast of the amplitude of chlorophyll concentration variability was getting worse. Forecasts with a 3-month lead time were on average the closest to the S-NPP VIIRS data (23% or 0.033 μg chl L(−1)) while the forecast with a 9-month lead time were the furthest (31% or 0.042 μg chl L(−1)). These results indicate the potential for forecasting chlorophyll concentration in this region but also highlights various deficiencies and suggestions for improvements to the current biogeochemical forecasting system. This system provides an initial basis for future applications including the effects of El Niño events on fisheries and other ocean resources given improvements identified in the analysis of these results. 2017-07-26 2017 /pmc/articles/PMC5747543/ /pubmed/29291196 http://dx.doi.org/10.3389/fmars.2017.00236 Text en http://creativecommons.org/licenses/by/4.0/ This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
spellingShingle Article
Rousseaux, Cecile S.
Gregg, Watson W.
Forecasting Ocean Chlorophyll in the Equatorial Pacific
title Forecasting Ocean Chlorophyll in the Equatorial Pacific
title_full Forecasting Ocean Chlorophyll in the Equatorial Pacific
title_fullStr Forecasting Ocean Chlorophyll in the Equatorial Pacific
title_full_unstemmed Forecasting Ocean Chlorophyll in the Equatorial Pacific
title_short Forecasting Ocean Chlorophyll in the Equatorial Pacific
title_sort forecasting ocean chlorophyll in the equatorial pacific
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5747543/
https://www.ncbi.nlm.nih.gov/pubmed/29291196
http://dx.doi.org/10.3389/fmars.2017.00236
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