Assessed the variation of sea ice radiative forcing over the Arctic region from 1982 to 2100 and estimated the cost ...

<!--!introduction!--> Arctic sea ice shrinks rapidly as global warming, further increasing the ocean's absorption of solar heat by reducing surface albedo. A wealth of studies has investigated Arctic sea ice's variability, mechanism and future projection. However, past and future rad...

Full description

Bibliographic Details
Main Author: Hao, Hairui
Format: Conference Object
Language:unknown
Published: GFZ German Research Centre for Geosciences 2023
Subjects:
Online Access:https://dx.doi.org/10.57757/iugg23-3733
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5020810
Description
Summary:<!--!introduction!--> Arctic sea ice shrinks rapidly as global warming, further increasing the ocean's absorption of solar heat by reducing surface albedo. A wealth of studies has investigated Arctic sea ice's variability, mechanism and future projection. However, past and future radiative forcing caused by changes in sea ice albedo and the resulting economic impacts remain to be conducted. In this study, we first analyze the evolution of Arctic sea ice radiative forcing (SIRF) from 1982 to 2100 using a radiative kernel method. Then, the SIRF is converted to a carbon equivalent using the DICE model, and the associated economic effect is further estimated by a replacement cost method. Our results provide a systematic understanding of the radiative effects of Arctic sea ice change on the global climate and corresponding economic impacts. ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ...