表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験

We present a series of numerical experiments of Greenland ice sheet under global warming condition using Ice sheet model for Integrated Earth system Studies (ICIES). In this study, influence on the simulation from the difference in the method to compute the surface mass balance is focused. Typically...

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Main Authors: 齋藤, 冬樹, 阿部, 彩子, 高橋, 邦生, SAITO, Fuyuki, Ayako, ABE-OUCHI, Kunio, TAKAHASHI
Language:English
Published: 2013
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/11690/files/OM_SaitoFuyuki_1.pdf
https://nipr.repo.nii.ac.jp/records/11690
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author 齋藤, 冬樹
阿部, 彩子
高橋, 邦生
SAITO, Fuyuki
Ayako, ABE-OUCHI
Kunio, TAKAHASHI
author_facet 齋藤, 冬樹
阿部, 彩子
高橋, 邦生
SAITO, Fuyuki
Ayako, ABE-OUCHI
Kunio, TAKAHASHI
author_sort 齋藤, 冬樹
collection National Institute of Polar Research Repository, Japan
description We present a series of numerical experiments of Greenland ice sheet under global warming condition using Ice sheet model for Integrated Earth system Studies (ICIES). In this study, influence on the simulation from the difference in the method to compute the surface mass balance is focused. Typically, ice sheet simulation is driven by a reference-anomaly method, in which the surface temperature and/or the accumulation are decomposed into the reference terms (e.g., observation), the anomaly (e.g., climate scenario from climate models). Then the surface melting is computed using parameterization such as positive degree-day (PDD) method with the temperature. These decomposed terms have own uncertainties, which may influence the ice-sheet simulation. In this study, impact of these properties to the present-day control case, as well as the response under uniform warming condition are discussed, which is thought be a useful and basic information of the property/sensitivity of the Greenland ice sheet. In addition, several initialization methods (free spin-up, fixed-topography spin-up, etc) are applied to ICIES in order to evaluate the influence of the error in the present-day simulated topography to the shortterm response of Greenland ice sheet. 第4回極域科学シンポジウム 個別セッション:[OM] 気水圏 11月15日(金) 統計数理研究所 3階セミナー室1(D305) conference object
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
geographic Greenland
geographic_facet Greenland
id ftnipr:oai:nipr.repo.nii.ac.jp:00011690
institution Open Polar
language English
op_collection_id ftnipr
op_relation https://nipr.repo.nii.ac.jp/record/11690/files/OM_SaitoFuyuki_1.pdf
https://nipr.repo.nii.ac.jp/records/11690
publishDate 2013
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00011690 2025-04-13T14:19:41+00:00 表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験 Sensitivity of Response of Greenland Ice Sheet to Global Warming on Surface Mass Balance and Initialization methods 齋藤, 冬樹 阿部, 彩子 高橋, 邦生 SAITO, Fuyuki Ayako, ABE-OUCHI Kunio, TAKAHASHI 2013-11-15 application/pdf https://nipr.repo.nii.ac.jp/record/11690/files/OM_SaitoFuyuki_1.pdf https://nipr.repo.nii.ac.jp/records/11690 eng eng https://nipr.repo.nii.ac.jp/record/11690/files/OM_SaitoFuyuki_1.pdf https://nipr.repo.nii.ac.jp/records/11690 2013 ftnipr 2025-03-19T10:19:57Z We present a series of numerical experiments of Greenland ice sheet under global warming condition using Ice sheet model for Integrated Earth system Studies (ICIES). In this study, influence on the simulation from the difference in the method to compute the surface mass balance is focused. Typically, ice sheet simulation is driven by a reference-anomaly method, in which the surface temperature and/or the accumulation are decomposed into the reference terms (e.g., observation), the anomaly (e.g., climate scenario from climate models). Then the surface melting is computed using parameterization such as positive degree-day (PDD) method with the temperature. These decomposed terms have own uncertainties, which may influence the ice-sheet simulation. In this study, impact of these properties to the present-day control case, as well as the response under uniform warming condition are discussed, which is thought be a useful and basic information of the property/sensitivity of the Greenland ice sheet. In addition, several initialization methods (free spin-up, fixed-topography spin-up, etc) are applied to ICIES in order to evaluate the influence of the error in the present-day simulated topography to the shortterm response of Greenland ice sheet. 第4回極域科学シンポジウム 個別セッション:[OM] 気水圏 11月15日(金) 統計数理研究所 3階セミナー室1(D305) conference object Other/Unknown Material Greenland Ice Sheet National Institute of Polar Research Repository, Japan Greenland
spellingShingle 齋藤, 冬樹
阿部, 彩子
高橋, 邦生
SAITO, Fuyuki
Ayako, ABE-OUCHI
Kunio, TAKAHASHI
表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験
title 表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験
title_full 表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験
title_fullStr 表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験
title_full_unstemmed 表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験
title_short 表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験
title_sort 表面質量収支モデルおよび初期化方法に対するグリーンランド温暖化応答の感度実験
url https://nipr.repo.nii.ac.jp/record/11690/files/OM_SaitoFuyuki_1.pdf
https://nipr.repo.nii.ac.jp/records/11690