An Adjoint Force-restore Model for Glacier Terminus Fluctuations
Abstract
A linear inverse formula comprises the basis for an individual treatment of 7 central Asian (25-55°N; 70-95°E) glaciers. The linear forward model is based on first order glacier dynamics, and requires the knowledge of reference states of forcing and glacier perturbation magnitude. In this study, the adjoint based 4D-var method was applied to optimally determine the reference states and make it possible to start the integration at an arbitrarily chosen time, and thus suitable to use the availability of the coupled general circulation model (CGCM) predictions of future temperature scenarios. Two sensitive yet uncertain glacier parameters and reference states at year 1900 are inferred from observed glacier length records distributed irregularly over the 20th century and the regional mean annual temperature anomaly (against 1961-1990 reference) time series. We rotated the temperature forcing for the Hadley Centre- Climatic Research Unit of the University of East Anglia (HadCRUT2), the Global Historical Climatology Network (GHCN) observations, and the ensemble mean of multiple CGCM runs and compared the retrieval results. Because of the high resemblance between the three data sources after 1960, it was decided practicable to use the observed temperature as forcing in retrieving the model parameters and initial states and then run an extended period with forcing from ensemble mean CGCM temperature of the next century. The length fluctuation is estimated for the transient climate period with 9 CGCM simulations under SRES A2 (a strong emission scenario from the Special report on Emissions Scenarios). For the 60-year period 2000- 2060, all glaciers experienced salient shrinkage, especially those with gentle slopes. Although nearly one-third the year 2000 length will be reduced for some small glaciers, the very existence of the glaciers studied here is not threatened by year 2060. The differences in individual glacier responses are very large. No straightforward relationship is found between glacier size and fractional change of its length.
- Publication:
-
AGU Fall Meeting Abstracts
- Pub Date:
- December 2006
- Bibcode:
- 2006AGUFM.C31A1235R
- Keywords:
-
- 0500 COMPUTATIONAL GEOPHYSICS (3200;
- 3252;
- 7833);
- 0720 Glaciers;
- 0774 Dynamics;
- 0776 Glaciology (1621;
- 1827;
- 1863);
- 0798 Modeling