TY - JOUR

T1 - Accuracy Assessment of primary production models with and without photoinhibition using Ocean-Colour Climate Change Initiative data in the North East Atlantic Ocean

AU - Lobanova, Polina

AU - Tilstone, Gavin H.

AU - Bashmachnikov, Igor

AU - Brotas, Vanda

PY - 2018/7/1

Y1 - 2018/7/1

N2 - The accuracy of three satellite models of primary production (PP) of varying complexity was assessed against 95 in situ 14C uptake measurements from the North East Atlantic Ocean (NEA). The models were run using the European Space Agency (ESA), Ocean Colour Climate Change Initiative (OC-CCI) version 3.0 data. The objectives of the study were to determine which is the most accurate PP model for the region in different provinces and seasons, what is the accuracy of the models using both high (daily) and low (eight day) temporal resolution OC-CCI data, and whether the performance of the models is improved by implementing a photoinhibition function? The Platt-Sathyendranath primary production model (PP PSM) was the most accurate over all NEA provinces and, specifically, in the Atlantic Arctic province (ARCT) and North Atlantic Drift (NADR) provinces. The implementation of a photoinhibition function in the PP PSM reduced its accuracy, especially at lower range PP. The Vertical Generalized Production Model-VGPM (PP VGPM) tended to over-estimate PP, especially in summer and in the NADR. The accuracy of PP VGPM improved with the implementation of a photoinhibition function in summer. The absorption model of primary production (PP Aph), with and without photoinhibition, was the least accurate model for the NEA. Mapped images of each model showed that the PP VGPM was 150% higher in the NADR compared to PP PSM. In the North Atlantic Subtropical Gyre (NAST) province, PP Aph was 355% higher than PP PSM, whereas PP VGPM was 215% higher. A sensitivity analysis indicated that chlorophyll-a (Chl a), or the absorption of phytoplankton, at 443 nm (a ph (443)) caused the largest error in the estimation of PP, followed by the photosynthetic rate terms and then the irradiance functions used for each model.

AB - The accuracy of three satellite models of primary production (PP) of varying complexity was assessed against 95 in situ 14C uptake measurements from the North East Atlantic Ocean (NEA). The models were run using the European Space Agency (ESA), Ocean Colour Climate Change Initiative (OC-CCI) version 3.0 data. The objectives of the study were to determine which is the most accurate PP model for the region in different provinces and seasons, what is the accuracy of the models using both high (daily) and low (eight day) temporal resolution OC-CCI data, and whether the performance of the models is improved by implementing a photoinhibition function? The Platt-Sathyendranath primary production model (PP PSM) was the most accurate over all NEA provinces and, specifically, in the Atlantic Arctic province (ARCT) and North Atlantic Drift (NADR) provinces. The implementation of a photoinhibition function in the PP PSM reduced its accuracy, especially at lower range PP. The Vertical Generalized Production Model-VGPM (PP VGPM) tended to over-estimate PP, especially in summer and in the NADR. The accuracy of PP VGPM improved with the implementation of a photoinhibition function in summer. The absorption model of primary production (PP Aph), with and without photoinhibition, was the least accurate model for the NEA. Mapped images of each model showed that the PP VGPM was 150% higher in the NADR compared to PP PSM. In the North Atlantic Subtropical Gyre (NAST) province, PP Aph was 355% higher than PP PSM, whereas PP VGPM was 215% higher. A sensitivity analysis indicated that chlorophyll-a (Chl a), or the absorption of phytoplankton, at 443 nm (a ph (443)) caused the largest error in the estimation of PP, followed by the photosynthetic rate terms and then the irradiance functions used for each model.

KW - North Atlantic Ocean

KW - Ocean colour

KW - Photosynthesis

KW - Phytoplankton

KW - Primary production

KW - Remote sensing

UR - http://www.scopus.com/inward/record.url?scp=85050467616&partnerID=8YFLogxK

U2 - 10.3390/rs10071116

DO - 10.3390/rs10071116

M3 - Article

VL - 10

JO - Remote Sensing

JF - Remote Sensing

SN - 2072-4292

IS - 7

M1 - 1116

ER -