Climate change impacts on the ocean’s biological carbon pump in a CMIP6 Earth System Model:

Thesis advisor: Hilary Palevsky The ocean plays a key role in global carbon cycling, taking up CO2 from the atmosphere. A fraction of this CO2 is converted into organic carbon through primary production in the surface ocean and sequestered in the deep ocean through a process known as the biological...

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Main Author: Walker, Stevie
Format: Thesis
Language:English
Published: Boston College 2021
Subjects:
Online Access:http://hdl.handle.net/2345/bc-ir:109224
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spelling ftbostoncollir:oai:dlib.bc.edu:bc-ir_109224 2023-05-15T17:35:36+02:00 Climate change impacts on the ocean’s biological carbon pump in a CMIP6 Earth System Model: Walker, Stevie 2021 electronic application/pdf http://hdl.handle.net/2345/bc-ir:109224 English eng Boston College Copyright is held by the author, with all rights reserved, unless otherwise noted. marine biogeochemistry ocean carbon cycling Earth System Models climate change impacts biological pump Text thesis 2021 ftbostoncollir 2022-03-05T18:33:26Z Thesis advisor: Hilary Palevsky The ocean plays a key role in global carbon cycling, taking up CO2 from the atmosphere. A fraction of this CO2 is converted into organic carbon through primary production in the surface ocean and sequestered in the deep ocean through a process known as the biological pump. The ability of the biological pump to sequester carbon away from the atmosphere is influenced by the interaction between the annual cycle of ocean mixed layer depth (MLD), primary production, and ecosystem processes that influence export efficiency. Gravitational sinking of particulate organic carbon (POC) is the largest component of the biological pump and the aspect that is best represented in Earth System Models (ESMs). I use ESM data from CESM2, an ESM participating in the Coupled Model Intercomparison Project Phase 6 (CMIP6), to investigate how a high-emissions climate change scenario will impact POC flux globally and regionally over the 21st century. The model simulates a 4.4% decrease in global POC flux at the 100 m depth horizon, from 7.12 Pg C/yr in the short-term (2014-2034) to 6.81 Pg C/yr in the long-term (2079-2099), indicating that the biological pump will become less efficient overall at sequestering carbon. However, the extent of change varies across the globe, including the largest POC flux declines in the North Atlantic, where the maximum annual MLD is projected to shoal immensely. In the future, a multi-model comparison across ESMs will allow for further analysis on the variability of these changes to the biological pump. Thesis (BS) — Boston College, 2021. Submitted to: Boston College. College of Arts and Sciences. Discipline: Departmental Honors. Discipline: Earth and Environmental Science. Thesis North Atlantic Boston College: eScholarship@BC
institution Open Polar
collection Boston College: eScholarship@BC
op_collection_id ftbostoncollir
language English
topic marine biogeochemistry
ocean carbon cycling
Earth System Models
climate change impacts
biological pump
spellingShingle marine biogeochemistry
ocean carbon cycling
Earth System Models
climate change impacts
biological pump
Walker, Stevie
Climate change impacts on the ocean’s biological carbon pump in a CMIP6 Earth System Model:
topic_facet marine biogeochemistry
ocean carbon cycling
Earth System Models
climate change impacts
biological pump
description Thesis advisor: Hilary Palevsky The ocean plays a key role in global carbon cycling, taking up CO2 from the atmosphere. A fraction of this CO2 is converted into organic carbon through primary production in the surface ocean and sequestered in the deep ocean through a process known as the biological pump. The ability of the biological pump to sequester carbon away from the atmosphere is influenced by the interaction between the annual cycle of ocean mixed layer depth (MLD), primary production, and ecosystem processes that influence export efficiency. Gravitational sinking of particulate organic carbon (POC) is the largest component of the biological pump and the aspect that is best represented in Earth System Models (ESMs). I use ESM data from CESM2, an ESM participating in the Coupled Model Intercomparison Project Phase 6 (CMIP6), to investigate how a high-emissions climate change scenario will impact POC flux globally and regionally over the 21st century. The model simulates a 4.4% decrease in global POC flux at the 100 m depth horizon, from 7.12 Pg C/yr in the short-term (2014-2034) to 6.81 Pg C/yr in the long-term (2079-2099), indicating that the biological pump will become less efficient overall at sequestering carbon. However, the extent of change varies across the globe, including the largest POC flux declines in the North Atlantic, where the maximum annual MLD is projected to shoal immensely. In the future, a multi-model comparison across ESMs will allow for further analysis on the variability of these changes to the biological pump. Thesis (BS) — Boston College, 2021. Submitted to: Boston College. College of Arts and Sciences. Discipline: Departmental Honors. Discipline: Earth and Environmental Science.
format Thesis
author Walker, Stevie
author_facet Walker, Stevie
author_sort Walker, Stevie
title Climate change impacts on the ocean’s biological carbon pump in a CMIP6 Earth System Model:
title_short Climate change impacts on the ocean’s biological carbon pump in a CMIP6 Earth System Model:
title_full Climate change impacts on the ocean’s biological carbon pump in a CMIP6 Earth System Model:
title_fullStr Climate change impacts on the ocean’s biological carbon pump in a CMIP6 Earth System Model:
title_full_unstemmed Climate change impacts on the ocean’s biological carbon pump in a CMIP6 Earth System Model:
title_sort climate change impacts on the ocean’s biological carbon pump in a cmip6 earth system model:
publisher Boston College
publishDate 2021
url http://hdl.handle.net/2345/bc-ir:109224
genre North Atlantic
genre_facet North Atlantic
op_rights Copyright is held by the author, with all rights reserved, unless otherwise noted.
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