Japan Geoscience Union Meeting 2019

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-CC Cryospheric Sciences & Cold District Environment

[A-CC27] Glaciology

Wed. May 29, 2019 9:00 AM - 10:30 AM 303 (3F)

convener:Takayuki Nuimura(Tokyo Denki University), Ishikawa Mamoru(Hokkaido University), Kzutaka Tateyama(National University Corporation Kitami Institute of Technology), Hiroto Nagai(Waseda Univ., School of Education), Chairperson:Hiroto Nagai(Japan Aerospace Exploration Agency)

10:15 AM - 10:30 AM

[ACC27-06] Quantify the range of projections of future changes in glacier mass caused by differences among observed past climate datasets

*Megumi Watanabe1, Aki Yanagawa2, Yukiko Hirabayashi3, Satoshi Watanabe4, Shinjiro Kanae1 (1.Tokyo Institute of Technology, 2.Meisei University, 3.Shibaura Institute of Technology, 4.The University of Tokyo)

Keywords:propagation of uncertainty, glacier model, bias correction, calibration, air temperature, precipitation

Observed climate data used as input in glacier models are expected to differ among datasets particularly at high elevations. Differences among datasets have not yet been described as a cause of uncertainty in projections of future changes in glacier mass, although uncertainty caused by varying future climate projections among general circulation models (GCMs) has often been discussed. Differences among climate datasets are expected to propagate as uncertainty in future changes in glacier mass due to bias correction of GCMs and calibration of glacier models. We project ensemble future changes in the mass of glaciers in Asia through the year 2100 using a glacier model. A set of 18 combinations of inputs, including two observed past air temperature datasets, three observed past precipitation datasets, and future air temperature and precipitation projections from three GCMs were used. The uncertainty in projected changes in glacier mass was partitioned into three distinct sources: GCM uncertainty, observed past air temperature uncertainty, and observed past precipitation uncertainty. Our findings indicate that, in addition to the differences in climate projections among GCMs, differences among climate datasets can propagate uncertainty into projected changes in glacier mass. Significant differences in observed precipitation did not cause major uncertainty in projected changes in glacier mass.