Abstract

Abstract. Glacier fluctuations contribute to variations in sea level and historical glacier length fluctuations are natural indicators of past climate change. To study these subjects, long-term information of glacier change is needed. In this paper we present a data set of global long-term glacier length fluctuations. The data set is a compilation of available information on changes in glacier length worldwide, including both measured and reconstructed glacier length fluctuations. All 471 length series start before 1950 and cover at least four decades. The longest record starts in 1535, but the majority of time series start after 1850. The number of available records decreases again after 1962. The data set has global coverage including records from all continents. However, the Canadian Arctic is not represented in the data set. The available glacier length series show relatively small fluctuations until the mid-19th century, followed by a global retreat. The retreat was strongest in the first half of the 20th century, although large variability in the length change of the different glaciers is observed. During the 20th century, calving glaciers retreated more than land-terminating glaciers, but their relative length change was approximately equal. Besides calving, the glacier slope is the most important glacier property determining length change: steep glaciers have retreated less than glaciers with a gentle slope.

Highlights

  • Glaciers have been one of the main contributors to sealevel change during the last century (Gregory et al, 2013)

  • Using the presented data set, we analyze the temporal evolution of the observed global glacier length changes, including a regional differentiation, and we analyze how length changes are related to the glacier geometry and the climate setting of glaciers

  • The correlation between slope and length change is confirmed by the observed glacier length changes over the 20th century: large retreats are rare for steep glaciers (Fig. 11a)

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Summary

Introduction

Glaciers have been one of the main contributors to sealevel change during the last century (Gregory et al, 2013). Quantitative information on glacier fluctuations over previous centuries provide long-term context for recently observed climatic changes of the last several decades (e.g., Oerlemans, 2005; Leclercq and Oerlemans, 2012; Lüthi, 2014). Length fluctuations that combines different sources of information. It has been constructed over the course of several years (Klok and Oerlemans, 2004; Oerlemans, 2005) and contains information of worldwide glacier length changes in a uniform format. Using the presented data set, we analyze the temporal evolution of the observed global glacier length changes, including a regional differentiation, and we analyze how length changes are related to the glacier geometry and the climate setting of glaciers

Glacier length data
Additional glacier information
Spatial and temporal coverage
Regional differentiation
Alaska
West Canada and US
Low latitudes
Southern Andes
Antarctica
Global and regional length change
Dependence of length change on glacier properties
Findings
Concluding summary and outlook
Full Text
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