Projected Oceanographical Changes in the Baltic Sea until 2100

In this article, the concepts and background of regional climate modeling of the future Baltic Sea are summarized and state-of-the-art projections, climate change impact studies, and challenges are discussed. The focus is on projected oceanographic changes in future climate. However, as these change...

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Main Authors: Meier, H.E. Markus, Saraiva, Sofia
Format: Book Part
Language:English
Published: Oxford University Press 2020
Subjects:
Online Access:http://dx.doi.org/10.1093/acrefore/9780190228620.013.699
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spelling croxfordunivpr:10.1093/acrefore/9780190228620.013.699 2024-09-30T14:43:13+00:00 Projected Oceanographical Changes in the Baltic Sea until 2100 Meier, H.E. Markus Saraiva, Sofia 2020 http://dx.doi.org/10.1093/acrefore/9780190228620.013.699 en eng Oxford University Press Oxford Research Encyclopedia of Climate Science ISBN 9780190228620 reference-entry 2020 croxfordunivpr https://doi.org/10.1093/acrefore/9780190228620.013.699 2024-09-17T04:32:07Z In this article, the concepts and background of regional climate modeling of the future Baltic Sea are summarized and state-of-the-art projections, climate change impact studies, and challenges are discussed. The focus is on projected oceanographic changes in future climate. However, as these changes may have a significant impact on biogeochemical cycling, nutrient load scenario simulations in future climates are briefly discussed as well. The Baltic Sea is special compared to other coastal seas as it is a tideless, semi-enclosed sea with large freshwater and nutrient supply from a partly heavily populated catchment area and a long response time of about 30 years, and as it is, in the early 21st century, warming faster than any other coastal sea in the world. Hence, policymakers request the development of nutrient load abatement strategies in future climate. For this purpose, large ensembles of coupled climate–environmental scenario simulations based upon high-resolution circulation models were developed to estimate changes in water temperature, salinity, sea-ice cover, sea level, oxygen, nutrient, and phytoplankton concentrations, and water transparency, together with uncertainty ranges. Uncertainties in scenario simulations of the Baltic Sea are considerable. Sources of uncertainties are global and regional climate model biases, natural variability, and unknown greenhouse gas emission and nutrient load scenarios. Unknown early 21st-century and future bioavailable nutrient loads from land and atmosphere and the experimental setup of the dynamical downscaling technique are perhaps the largest sources of uncertainties for marine biogeochemistry projections. The high uncertainties might potentially be reducible through investments in new multi-model ensemble simulations that are built on better experimental setups, improved models, and more plausible nutrient loads. The development of community models for the Baltic Sea region with improved performance and common coordinated experiments of scenario simulations is ... Book Part Sea ice Oxford University Press
institution Open Polar
collection Oxford University Press
op_collection_id croxfordunivpr
language English
description In this article, the concepts and background of regional climate modeling of the future Baltic Sea are summarized and state-of-the-art projections, climate change impact studies, and challenges are discussed. The focus is on projected oceanographic changes in future climate. However, as these changes may have a significant impact on biogeochemical cycling, nutrient load scenario simulations in future climates are briefly discussed as well. The Baltic Sea is special compared to other coastal seas as it is a tideless, semi-enclosed sea with large freshwater and nutrient supply from a partly heavily populated catchment area and a long response time of about 30 years, and as it is, in the early 21st century, warming faster than any other coastal sea in the world. Hence, policymakers request the development of nutrient load abatement strategies in future climate. For this purpose, large ensembles of coupled climate–environmental scenario simulations based upon high-resolution circulation models were developed to estimate changes in water temperature, salinity, sea-ice cover, sea level, oxygen, nutrient, and phytoplankton concentrations, and water transparency, together with uncertainty ranges. Uncertainties in scenario simulations of the Baltic Sea are considerable. Sources of uncertainties are global and regional climate model biases, natural variability, and unknown greenhouse gas emission and nutrient load scenarios. Unknown early 21st-century and future bioavailable nutrient loads from land and atmosphere and the experimental setup of the dynamical downscaling technique are perhaps the largest sources of uncertainties for marine biogeochemistry projections. The high uncertainties might potentially be reducible through investments in new multi-model ensemble simulations that are built on better experimental setups, improved models, and more plausible nutrient loads. The development of community models for the Baltic Sea region with improved performance and common coordinated experiments of scenario simulations is ...
format Book Part
author Meier, H.E. Markus
Saraiva, Sofia
spellingShingle Meier, H.E. Markus
Saraiva, Sofia
Projected Oceanographical Changes in the Baltic Sea until 2100
author_facet Meier, H.E. Markus
Saraiva, Sofia
author_sort Meier, H.E. Markus
title Projected Oceanographical Changes in the Baltic Sea until 2100
title_short Projected Oceanographical Changes in the Baltic Sea until 2100
title_full Projected Oceanographical Changes in the Baltic Sea until 2100
title_fullStr Projected Oceanographical Changes in the Baltic Sea until 2100
title_full_unstemmed Projected Oceanographical Changes in the Baltic Sea until 2100
title_sort projected oceanographical changes in the baltic sea until 2100
publisher Oxford University Press
publishDate 2020
url http://dx.doi.org/10.1093/acrefore/9780190228620.013.699
genre Sea ice
genre_facet Sea ice
op_source Oxford Research Encyclopedia of Climate Science
ISBN 9780190228620
op_doi https://doi.org/10.1093/acrefore/9780190228620.013.699
_version_ 1811645107289456640