Global chlorophyll distribution induced by mesoscale eddies

While mesoscale eddies can trap and transport chlorophyll (CHL) within the water columns, satellite measurements can only observe CHL at the sea surface. Here, we estimate the eddy-induced CHL distribution based on satellite observations, Argo float measurements, and global empirical models. The com...

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Published in:Remote Sensing of Environment
Main Authors: Zhao, Dandan, Xu, Yongsheng, Zhang, Xiangguang, Huang, Chao
Format: Report
Language:English
Published: ELSEVIER SCIENCE INC 2021
Subjects:
SEA
Online Access:http://ir.qdio.ac.cn/handle/337002/170043
https://doi.org/10.1016/j.rse.2020.112245
id ftchinacasciocas:oai:ir.qdio.ac.cn:337002/170043
record_format openpolar
spelling ftchinacasciocas:oai:ir.qdio.ac.cn:337002/170043 2023-05-15T17:33:06+02:00 Global chlorophyll distribution induced by mesoscale eddies Zhao, Dandan Xu, Yongsheng Zhang, Xiangguang Huang, Chao 2021-03-01 http://ir.qdio.ac.cn/handle/337002/170043 https://doi.org/10.1016/j.rse.2020.112245 英语 eng ELSEVIER SCIENCE INC REMOTE SENSING OF ENVIRONMENT http://ir.qdio.ac.cn/handle/337002/170043 doi:10.1016/j.rse.2020.112245 Environmental Sciences & Ecology Remote Sensing Imaging Science & Photographic Technology Environmental Sciences IN-SITU NORTH-ATLANTIC SATELLITE ALTIMETRY EDDY PROPERTIES ALASKAN STREAM OCEAN SOUTH VARIABILITY TRANSPORT SEA 期刊论文 2021 ftchinacasciocas https://doi.org/10.1016/j.rse.2020.112245 2022-06-27T05:43:33Z While mesoscale eddies can trap and transport chlorophyll (CHL) within the water columns, satellite measurements can only observe CHL at the sea surface. Here, we estimate the eddy-induced CHL distribution based on satellite observations, Argo float measurements, and global empirical models. The combination of satellite altimeter data and Argo measurements is used to detect eddy boundaries by tracking the outermost closed contours of potential vorticity (PV) at depth; then, sea surface CHL from satellite observations, together with their vertical distributions estimated from models are used to derive the CHL within eddy boundaries. We find that the CHL trapped by eddies can reach 3.2 x 10(12) g, which is about half of the total CHL in the ocean; the global time-mean CHL eddy-induced zonal transport adds up to 5.7 x 10(3) g/s westward. The results show that oceanic mesoscale eddies play an important role in the elevated CHL in the interior of the ocean. Report North Atlantic Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Remote Sensing of Environment 254 112245
institution Open Polar
collection Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR
op_collection_id ftchinacasciocas
language English
topic Environmental Sciences & Ecology
Remote Sensing
Imaging Science & Photographic Technology
Environmental Sciences
IN-SITU
NORTH-ATLANTIC
SATELLITE ALTIMETRY
EDDY PROPERTIES
ALASKAN STREAM
OCEAN
SOUTH
VARIABILITY
TRANSPORT
SEA
spellingShingle Environmental Sciences & Ecology
Remote Sensing
Imaging Science & Photographic Technology
Environmental Sciences
IN-SITU
NORTH-ATLANTIC
SATELLITE ALTIMETRY
EDDY PROPERTIES
ALASKAN STREAM
OCEAN
SOUTH
VARIABILITY
TRANSPORT
SEA
Zhao, Dandan
Xu, Yongsheng
Zhang, Xiangguang
Huang, Chao
Global chlorophyll distribution induced by mesoscale eddies
topic_facet Environmental Sciences & Ecology
Remote Sensing
Imaging Science & Photographic Technology
Environmental Sciences
IN-SITU
NORTH-ATLANTIC
SATELLITE ALTIMETRY
EDDY PROPERTIES
ALASKAN STREAM
OCEAN
SOUTH
VARIABILITY
TRANSPORT
SEA
description While mesoscale eddies can trap and transport chlorophyll (CHL) within the water columns, satellite measurements can only observe CHL at the sea surface. Here, we estimate the eddy-induced CHL distribution based on satellite observations, Argo float measurements, and global empirical models. The combination of satellite altimeter data and Argo measurements is used to detect eddy boundaries by tracking the outermost closed contours of potential vorticity (PV) at depth; then, sea surface CHL from satellite observations, together with their vertical distributions estimated from models are used to derive the CHL within eddy boundaries. We find that the CHL trapped by eddies can reach 3.2 x 10(12) g, which is about half of the total CHL in the ocean; the global time-mean CHL eddy-induced zonal transport adds up to 5.7 x 10(3) g/s westward. The results show that oceanic mesoscale eddies play an important role in the elevated CHL in the interior of the ocean.
format Report
author Zhao, Dandan
Xu, Yongsheng
Zhang, Xiangguang
Huang, Chao
author_facet Zhao, Dandan
Xu, Yongsheng
Zhang, Xiangguang
Huang, Chao
author_sort Zhao, Dandan
title Global chlorophyll distribution induced by mesoscale eddies
title_short Global chlorophyll distribution induced by mesoscale eddies
title_full Global chlorophyll distribution induced by mesoscale eddies
title_fullStr Global chlorophyll distribution induced by mesoscale eddies
title_full_unstemmed Global chlorophyll distribution induced by mesoscale eddies
title_sort global chlorophyll distribution induced by mesoscale eddies
publisher ELSEVIER SCIENCE INC
publishDate 2021
url http://ir.qdio.ac.cn/handle/337002/170043
https://doi.org/10.1016/j.rse.2020.112245
genre North Atlantic
genre_facet North Atlantic
op_relation REMOTE SENSING OF ENVIRONMENT
http://ir.qdio.ac.cn/handle/337002/170043
doi:10.1016/j.rse.2020.112245
op_doi https://doi.org/10.1016/j.rse.2020.112245
container_title Remote Sensing of Environment
container_volume 254
container_start_page 112245
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