
Modeling modern glacier response to climate changes along the A ndes C ordillera: A multiscale review
Author(s) -
Fernández Alfonso,
Mark Bryan G.
Publication year - 2016
Publication title -
journal of advances in modeling earth systems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 3.03
H-Index - 58
ISSN - 1942-2466
DOI - 10.1002/2015ms000482
Subject(s) - downscaling , glacier , scale (ratio) , climate model , range (aeronautics) , climatology , energy balance , climate change , glacier mass balance , environmental science , spatial ecology , computer science , physical geography , geology , geography , ecology , cartography , oceanography , materials science , composite material , biology
Here we review the literature preferentially concerned with modern glacier‐climate modeling along the Andes. We find a diverse range of modeling approaches, from empirical/statistical models to relatively complex energy balance procedures. We analyzed these models at three different spatial scales. First, we review global approaches that have included the Andes. Second, we depict and analyze modeling exercises aimed at studying Andean glaciers as a whole. Our revision shows only two studies dealing with glacier modeling at this continental scale. We contend that this regional approach is increasingly necessary because it allows for connecting the “average‐out” tendency of global studies to local observations or models, in order to comprehend scales of variability and heterogeneity. Third, we revise small‐scale modeling, finding that the overwhelming number of studies have targeted glaciers in Patagonia. We also find that most studies use temperature‐index models and that energy balance models are still not widely utilized. However, there is no clear spatial pattern of model complexity. We conclude with a discussion of both the limitations of certain approaches, as for example the use of short calibration periods for long‐term modeling, and also the opportunities for improved understanding afforded by new methods and techniques, such as climatic downscaling. We also propose ways to future developments, in which observations and models can be combined to improve current understanding of volumetric glacier changes and their climate causes.