Bayesian calibration of firn densification models

被引:12
|
作者
Verjans, Vincent [1 ]
Leeson, Amber A. [1 ]
Nemeth, Christopher [2 ]
Stevens, C. Max [3 ]
Munneke, Peter Kuipers [4 ]
Noel, Brice [4 ]
van Wessem, Jan Melchior [4 ]
机构
[1] Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4QY, England
[2] Univ Lancaster, Dept Math & Stat, Lancaster LA1 4YF, England
[3] Univ Washington, Dept Earth & Space Sci, Seattle, WA USA
[4] Univ Utrecht, Inst Marine & Atmospher Res Utrecht, Utrecht, Netherlands
来源
CRYOSPHERE | 2020年 / 14卷 / 09期
基金
英国工程与自然科学研究理事会;
关键词
GREENLAND ICE-SHEET; SURFACE MASS-BALANCE; DENSITY PROFILES; ACCUMULATION; SNOW; COMPACTION; GLACIER; VARIABILITY; CLIMATE; STREAMS;
D O I
10.5194/tc-14-3017-2020
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Firn densification modelling is key to understanding ice sheet mass balance, ice sheet surface elevation change, and the age difference between ice and the air in enclosed air bubbles. This has resulted in the development of many firn models, all relying to a certain degree on parameter calibration against observed data. We present a novel Bayesian calibration method for these parameters and apply it to three existing firn models. Using an extensive dataset of firn cores from Greenland and Antarctica, we reach optimal parameter estimates applicable to both ice sheets. We then use these to simulate firn density and evaluate against independent observations. Our simulations show a significant decrease (24% and 56 %) in observation-model discrepancy for two models and a smaller increase (15 %) for the third. As opposed to current methods, the Bayesian framework allows for robust uncertainty analysis related to parameter values. Based on our results, we review some inherent model assumptions and demonstrate how firn model choice and uncertainties in parameter values cause spread in key model outputs.
引用
收藏
页码:3017 / 3032
页数:16
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