Abstract
Remote sensing of ocean colour allows to analyze spatial and temporal variability of chlorophyll-a concentration (Chl) in a subsurface layer and estimate primary production of phytoplankton (PP) at regional and global scales. However, improvement of remote sensing algorithms requires systematical validation of satellite data by in situ observations. In this work, we compare satellite-derived and field estimates of Chl and modeled PP in the western part of the Japan/East Sea (35-440 N, 130-1370 E) in spring 2004 and autumn 2005 and 2011. As satellite PP we use its VGPM estimates from Ocean Productivity database. Field PP is calculated on the base of in situ observations of Chl, assimilation value, diffuse attenuation coefficient and sea surface temperature using two models: VGPM and a model developed in V.I. Il'ichev Pacific Oceanological Institute (POI). Comparison shows fair correlation between satellite-derived and field data: r = 0.56-0.63 for modeled PP and r = 0.58 for Chl. Their averaged estimates for all stations of observation have small difference, which, however, may be about 1.5-1.7 times in some periods. On average, satellite Chl overestimates in situ observations, while satellite estimates of PP are less than PP calculated with the use of the model developed by POI but greater than PP calculated using VGPM. The difference between modeled satellite and field PP estimates is due to features of vertical distribution of Chl within the euphotic zone and the difference in values of assimilation number used in the models.
| Original language | Russian |
|---|---|
| Pages (from-to) | 135-147 |
| Number of pages | 13 |
| Journal | Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa |
| Volume | 14 |
| Issue number | 2 |
| DOIs | |
| Publication status | Published - 2017 |
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Scopus subject areas
- Computer Science Applications
- Computer Networks and Communications
- Computers in Earth Sciences
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Primary production of phytoplankton and concentration of chlorophyll-a in the western part of the Japan/East Sea from remote sensing and field data. / Lobanova, P. V.; Zvalinski, V. I.; Tishchenko, P. Ya.
In: Sovremennye Problemy Distantsionnogo Zondirovaniya Zemli iz Kosmosa, Vol. 14, No. 2, 2017, p. 135-147.Research output
TY - JOUR
T1 - Primary production of phytoplankton and concentration of chlorophyll-a in the western part of the Japan/East Sea from remote sensing and field data
AU - Lobanova, P. V.
AU - Zvalinski, V. I.
AU - Tishchenko, P. Ya
PY - 2017
Y1 - 2017
N2 - Remote sensing of ocean colour allows to analyze spatial and temporal variability of chlorophyll-a concentration (Chl) in a subsurface layer and estimate primary production of phytoplankton (PP) at regional and global scales. However, improvement of remote sensing algorithms requires systematical validation of satellite data by in situ observations. In this work, we compare satellite-derived and field estimates of Chl and modeled PP in the western part of the Japan/East Sea (35-440 N, 130-1370 E) in spring 2004 and autumn 2005 and 2011. As satellite PP we use its VGPM estimates from Ocean Productivity database. Field PP is calculated on the base of in situ observations of Chl, assimilation value, diffuse attenuation coefficient and sea surface temperature using two models: VGPM and a model developed in V.I. Il'ichev Pacific Oceanological Institute (POI). Comparison shows fair correlation between satellite-derived and field data: r = 0.56-0.63 for modeled PP and r = 0.58 for Chl. Their averaged estimates for all stations of observation have small difference, which, however, may be about 1.5-1.7 times in some periods. On average, satellite Chl overestimates in situ observations, while satellite estimates of PP are less than PP calculated with the use of the model developed by POI but greater than PP calculated using VGPM. The difference between modeled satellite and field PP estimates is due to features of vertical distribution of Chl within the euphotic zone and the difference in values of assimilation number used in the models.
AB - Remote sensing of ocean colour allows to analyze spatial and temporal variability of chlorophyll-a concentration (Chl) in a subsurface layer and estimate primary production of phytoplankton (PP) at regional and global scales. However, improvement of remote sensing algorithms requires systematical validation of satellite data by in situ observations. In this work, we compare satellite-derived and field estimates of Chl and modeled PP in the western part of the Japan/East Sea (35-440 N, 130-1370 E) in spring 2004 and autumn 2005 and 2011. As satellite PP we use its VGPM estimates from Ocean Productivity database. Field PP is calculated on the base of in situ observations of Chl, assimilation value, diffuse attenuation coefficient and sea surface temperature using two models: VGPM and a model developed in V.I. Il'ichev Pacific Oceanological Institute (POI). Comparison shows fair correlation between satellite-derived and field data: r = 0.56-0.63 for modeled PP and r = 0.58 for Chl. Their averaged estimates for all stations of observation have small difference, which, however, may be about 1.5-1.7 times in some periods. On average, satellite Chl overestimates in situ observations, while satellite estimates of PP are less than PP calculated with the use of the model developed by POI but greater than PP calculated using VGPM. The difference between modeled satellite and field PP estimates is due to features of vertical distribution of Chl within the euphotic zone and the difference in values of assimilation number used in the models.
KW - Chlorophyll-a concentration
KW - Models of primary production
KW - Ocean colour
KW - Primary production
KW - Remote sensing
KW - The Japan/East Sea
UR - http://www.scopus.com/inward/record.url?scp=85020103666&partnerID=8YFLogxK
U2 - 10.21046/2070-7401-2017-14-2-135-147
DO - 10.21046/2070-7401-2017-14-2-135-147
M3 - статья
AN - SCOPUS:85020103666
VL - 14
SP - 135
EP - 147
JO - СОВРЕМЕННЫЕ ПРОБЛЕМЫ ДИСТАНЦИОННОГО ЗОНДИРОВАНИЯ ЗЕМЛИ ИЗ КОСМОСА
JF - СОВРЕМЕННЫЕ ПРОБЛЕМЫ ДИСТАНЦИОННОГО ЗОНДИРОВАНИЯ ЗЕМЛИ ИЗ КОСМОСА
SN - 2070-7401
IS - 2
ER -