Abstract

In the field of iceberg and glacier calving studies, it is important to collect comprehensive datasets of populations of icebergs. Particularly, calving of lake-terminating glaciers has been understudied. The aim of this work is to present an object-based method of iceberg detection and to create an inventory of icebergs located in a proglacial lagoon of San Quintín glacier, Northern Patagonia Icefield, Chile. This dataset is created using high-resolution WorldView-2 imagery and a derived DEM. We use it to briefly discuss the iceberg size distribution and area–volume scaling. Segmentation of the multispectral imagery produced a map of objects, which were classified with use of Random Forest supervised classification algorithm. An intermediate classification product was corrected with a ruleset exploiting contextual information and a watershed algorithm that was used to divide multiple touching icebergs into separate objects. Common theoretical heavy-tail statistical distributions were tested as descriptors of iceberg area and volume distributions. Power law models were proposed for the area–volume relationship. The proposed method performed well over the open lake detecting correctly icebergs in all size bands except 5–15 m2 where many icebergs were missed. A section of the lagoon with ice melange was not reliably mapped due to uniformity of the area in the imagery and DEM. The precision of the DEM limited the scaling effort to icebergs taller than 1.7 m and larger than 99 m2, despite the inventory containing icebergs as small as 4 m2. The work demonstrates viability of object-based analysis for lacustrine iceberg detection and shows that the statistical properties of iceberg population at San Quintín glacier match those of populations produced by tidewater glaciers.

Highlights

  • Lacustrine calving of glaciers is mechanical detachment of icebergs when a glacier terminates in fresh water [1,2]

  • The objective of this paper is to present a method of mapping of icebergs with use of Object-Based Image Analysis (OBIA) techniques on high-resolution optical satellite imagery

  • We provide two measures of uncertainty of the iceberg map created with the method described above: the error of the number of icebergs detected by the algorithm and the error of the surface area of an extracted iceberg

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Summary

Introduction

Lacustrine calving of glaciers is mechanical detachment of icebergs when a glacier terminates in fresh water [1,2]. Lacustrine calving very often produces small icebergs which are hardly detectable on medium resolution satellite data This is the case with small tidewater glaciers. In such cases, methods which measure the calving events instead of the floating iceberg population are used to quantify ice fluxes, such as LiDAR scanning, seismic and acoustic measurements [10] or time-lapse terrestrial photography [11,12]. Methods which measure the calving events instead of the floating iceberg population are used to quantify ice fluxes, such as LiDAR scanning, seismic and acoustic measurements [10] or time-lapse terrestrial photography [11,12] These in-situ techniques do not differ significantly in application near tidewater or lake-terminating glaciers. Scarcity of lacustrine iceberg and calving datasets was pointed out as a factor hindering research into the calving’s impact on lake-terminating glacier dynamics [12]

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