Glacier Recession in the Peruvian Andes: Climatic Forcing, Hydrologic Impact and Comparative Rates Over Time

  • Bryan G. Mark
  • Geoffrey O. Seltzer
Part of the Advances in Global Change Research book series (AGLO, volume 23)


Tropical glaciers are intriguing and apparently rapidly disappearing components of the cryosphere that literally crown a vast ecosystem of global significance. Half of the Earth’s surface area lies between the tropics of Capricorn and Cancer, wherein a staggering 75% of the global population resides (Thompson 2000). Tropical glaciers are highly sensitive to climate changes over different temporal and spatial scales, notably ENSO, and are important hydrological resources in tropical highlands (Francou et al. 1995; 2000; this volume; Wagnon et al. 2001; Kaser and Osmaston 2002). Moreover, resolving the complex dynamics and variability of the tropical climate over longer time periods presents important goals to the global modelling community. Compiling an accurate understanding of the timing and climate response of tropical glaciers in the past is a crucial source of palaeoclimatic information for the validation and comparison of climate models (e.g. Farrera et al. 1999; Hostetier and Clark 2000; Porter 2001; Harrison et al. 2002; Seltzer et al. 2002). Deciphering the relative strength of different climatic forcing mechanisms on tropical glacier behaviour and quantifying hydrological changes associated with glacier recession are therefore relevant to interpreting the past climate and predicting the impact of future climate changes. Much scientific, social and political attention now concerns future changes in climate, with temperature change predominant.


Climate forcing Glacier recession Hydrology Peruvian Andes Rates of deglaciation Terrain modelling 


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Copyright information

© Springer 2005

Authors and Affiliations

  • Bryan G. Mark
    • 1
    • 2
  • Geoffrey O. Seltzer
    • 3
  1. 1.Max Planck Institute for BiogeochemistryJenaGermany
  2. 2.c/o Department of GeographyUniversity of GlasgowGlasgowUK
  3. 3.Department of Earth SciencesSyracuse UniversitySyracuseUSA

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