Uncertainties originating from GCM downscaling and bias correction with application to the MIS-11c Greenland Ice Sheet

Abstract ∼  3.9 m contribution to sea-level rise). This result is on the lower bound of existing data- and model-based studies, partly as a consequence of the applied one-way coupling methodology that neglects some feedbacks. Additional uncertainties are examined by comparing two different present-day regional climate analyses for bias correction of temperatures and precipitation, a spread of initialization states and times, and different spatial configurations of precipitation bias corrections. No other factor exhibited greater influence over the simulated Greenland ice sheet than the choice of temperature downscaling scheme.

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
Uncertainties originating from GCM downscaling and bias correction with application to the MIS-11c Greenland Ice Sheet ; volume:20 ; number:2 ; year:2024 ; pages:281-296 ; extent:16
Climate of the past ; 20, Heft 2 (2024), 281-296 (gesamt 16)

Urheber
Crow, Brian R.
Tarasov, Lev
Schulz, Michael
Prange, Matthias

DOI
10.5194/cp-20-281-2024
URN
urn:nbn:de:101:1-2024020803171759465369
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
15.08.2025, 07:28 MESZ

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