Abstract

Abstract. Glacier mass loss is among the clearest indicators of atmospheric warming. The observation of these changes is one of the major objectives of the international climate monitoring strategy developed by the Global Climate Observing System (GCOS). Long-term glacier mass balance measurements are furthermore the basis for calibrating and validating models simulating future runoff of glacierised catchments. This is essential for Central Asia, which is one of the driest continental regions of the Northern Hemisphere. In the highly populated regions, water shortage due to decreased glacierisation potentially leads to pronounced political instability, drastic ecological changes and endangered food security. As a consequence of the collapse of the former Soviet Union, however, many valuable glacier monitoring sites in the Tien Shan and Pamir Mountains were abandoned. In recent years, multinational actors have re-established a set of important in situ measuring sites to continue the invaluable long-term data series. This paper introduces the applied monitoring strategy for selected glaciers in the Kyrgyz and Uzbek Tien Shan and Pamir, highlights the existing and the new measurements on these glaciers, and presents an example for how the old and new data can be combined to establish multi-decadal mass balance time series. This is crucial for understanding the impact of climate change on glaciers in this region.

Highlights

  • Glacier fluctuations in mountain areas have been monitored in various parts of the world for more than a century (Haeberli et al, 2007; Zemp et al, 2015), and glacier changes are considered to be reliable indicators of worldwide atmospheric warming trends (IPCC, 2013)

  • Embedded in Global Climate Observing System (GCOS) is the Global Terrestrial Network for Glaciers (GTN-G) operated by the World Glacier Monitoring Service (WGMS), the Published by Copernicus Publications on behalf of the European Geosciences Union

  • We demonstrate that a valuable glaciological dataset is available for the Central Asian mountains, for the Tien Shan, despite different historical backgrounds and changing methodological aspects

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Summary

Introduction

Glacier fluctuations in mountain areas have been monitored in various parts of the world for more than a century (Haeberli et al, 2007; Zemp et al, 2015), and glacier changes are considered to be reliable indicators of worldwide atmospheric warming trends (IPCC, 2013). Mountain glaciers and ice caps are important for early-detection strategies in global climate-related observations. Glaciers are one of the “essential climate variables” (ECVs) in the Global Climate Observing System (GCOS). Embedded in GCOS is the Global Terrestrial Network for Glaciers (GTN-G) operated by the World Glacier Monitoring Service (WGMS), the Published by Copernicus Publications on behalf of the European Geosciences Union. M. Hoelzle et al.: Re-establishing glacier monitoring

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