Permafrost Retrogressive Thaw Slump Dissolved Organic Matter Molecular Signatures on the Peel Plateau, Canada

The Arctic is warming at a rate twice that of other global ecosystems and changing climate conditions in the Arctic are mobilizing long frozen permafrost stores of organic carbon. In regions of extensive ground ice, thawing permafrost can cause land subsidence, and the creation of thermokarst featur...

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Bibliographic Details
Other Authors: Moore, Megan (author), Spencer, Robert G. M. (professor directing thesis), Atwood, Alyssa Regine (committee member), Chanton, Jeffrey P. (committee member), Florida State University (degree granting institution), College of Arts and Sciences (degree granting college), Department of Earth, Ocean, and Atmospheric Science (degree granting department)
Format: Master Thesis
Language:English
Published: Florida State University 2023
Subjects:
Ice
Online Access:https://diginole.lib.fsu.edu/islandora/object/fsu%3A887466/datastream/TN/view/Permafrost%20Retrogressive%20Thaw%20Slump%20Dissolved%20Organic%20Matter%20Molecular%20Signatures%20on%20the%20Peel%20Plateau,%20Canada.jpg