Global distribution changes in coccolithophore blooms

The global distribution of high Remote-sensing reflectance (Rrs) waters visible from satellite, likely associated with coccolithophore blooms, has changed markedly over the past 40 years. Over that period there has globally been an overall decrease in bloom area of 1.15 million km2 but with notable...

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Main Authors: Duncan, Eliza K, Clewley, Daniel, Smyth, Timothy James
Format: Other/Unknown Material
Language:unknown
Published: Authorea, Inc. 2023
Subjects:
Online Access:http://dx.doi.org/10.22541/essoar.169651337.71151879/v1
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spelling crwinnower:10.22541/essoar.169651337.71151879/v1 2024-06-02T07:55:41+00:00 Global distribution changes in coccolithophore blooms Duncan, Eliza K Clewley, Daniel Smyth, Timothy James 2023 http://dx.doi.org/10.22541/essoar.169651337.71151879/v1 unknown Authorea, Inc. posted-content 2023 crwinnower https://doi.org/10.22541/essoar.169651337.71151879/v1 2024-05-07T14:19:27Z The global distribution of high Remote-sensing reflectance (Rrs) waters visible from satellite, likely associated with coccolithophore blooms, has changed markedly over the past 40 years. Over that period there has globally been an overall decrease in bloom area of 1.15 million km2 but with notable Rrs increases in the Barents Sea and the Antarctic Ocean. The primary drivers of these fundamental changes to ocean biogeochemistry have been investigated using Machine Learning techniques together with contemporaneous global multi-decadal time-series of sea-surface temperature (SST); wind speed and stress; sea level anomaly (SLA); photosynthetically available radiation (PAR) and; mixed layer depth (MLD). When split into ocean provinces different drivers of positive and negative trends in Rrs were found to dominate in different regions, but generally increases were found to coincide with changes to SST, PAR and reductions to wind-speed. Other/Unknown Material Antarc* Antarctic Antarctic Ocean Barents Sea The Winnower Antarctic Antarctic Ocean Barents Sea The Antarctic
institution Open Polar
collection The Winnower
op_collection_id crwinnower
language unknown
description The global distribution of high Remote-sensing reflectance (Rrs) waters visible from satellite, likely associated with coccolithophore blooms, has changed markedly over the past 40 years. Over that period there has globally been an overall decrease in bloom area of 1.15 million km2 but with notable Rrs increases in the Barents Sea and the Antarctic Ocean. The primary drivers of these fundamental changes to ocean biogeochemistry have been investigated using Machine Learning techniques together with contemporaneous global multi-decadal time-series of sea-surface temperature (SST); wind speed and stress; sea level anomaly (SLA); photosynthetically available radiation (PAR) and; mixed layer depth (MLD). When split into ocean provinces different drivers of positive and negative trends in Rrs were found to dominate in different regions, but generally increases were found to coincide with changes to SST, PAR and reductions to wind-speed.
format Other/Unknown Material
author Duncan, Eliza K
Clewley, Daniel
Smyth, Timothy James
spellingShingle Duncan, Eliza K
Clewley, Daniel
Smyth, Timothy James
Global distribution changes in coccolithophore blooms
author_facet Duncan, Eliza K
Clewley, Daniel
Smyth, Timothy James
author_sort Duncan, Eliza K
title Global distribution changes in coccolithophore blooms
title_short Global distribution changes in coccolithophore blooms
title_full Global distribution changes in coccolithophore blooms
title_fullStr Global distribution changes in coccolithophore blooms
title_full_unstemmed Global distribution changes in coccolithophore blooms
title_sort global distribution changes in coccolithophore blooms
publisher Authorea, Inc.
publishDate 2023
url http://dx.doi.org/10.22541/essoar.169651337.71151879/v1
geographic Antarctic
Antarctic Ocean
Barents Sea
The Antarctic
geographic_facet Antarctic
Antarctic Ocean
Barents Sea
The Antarctic
genre Antarc*
Antarctic
Antarctic Ocean
Barents Sea
genre_facet Antarc*
Antarctic
Antarctic Ocean
Barents Sea
op_doi https://doi.org/10.22541/essoar.169651337.71151879/v1
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