Abstract

A Parrot Sequoia+ multispectral camera on a Parrot Bluegrass drone registered in four spectral bands (green, red, red edge (RE), and near-infrared (NIR)) to identify glacial outflow zones and determined the meltwater turbidity values in waters in front of the following Antarctic glaciers: Ecology, Dera Icefall, Zalewski, and Krak on King George Island, Southern Shetlands was used. This process was supported by a Red-Green-Blue (RGB) colour model from a Zenmuse X5 camera on an Inspire 2 quadcopter drone. Additional surface water turbidity measurements were carried out using a Yellow Springs Instruments (YSI) sonde EXO2. From this research, it was apparent that for mapping low-turbidity and medium-turbidity waters (<70 formazinenephelometricunits (FNU)), a red spectral band should be used, since it is insensitive to possible surface ice phenomena and registers the presence of both red and white sediments. High-turbidity plumes with elevated FNU values should be identified through the NIR band. Strong correlation coefficients between the reflectance at particular bands and FNU readings (RGreen = 0.85, RRed = 0.85, REdge = 0.84, and RNIR = 0.83) are shown that multispectral mapping using Unmanned Aerial Vehicles (UAVs) can be successfully usedeven in the unfavourable weather conditions and harsh climate of Antarctica. Lastly, the movement of water masses in Admiralty Bay is briefly discussed and supported by the results from EXO2 measurements.

Highlights

  • The Antarctic and Southern Ocean influence the climate of the entire world

  • As thethe water turbidity values, asas well as as thethe spectral reflectance reflectance registered by the Parrot Sequoia+ cameras, differ significantly between specific coves

  • The results provide support for the use of multispectral sensors given by the Zenmuse X5 camera on an Inspire 2 quadcopter drone, which, due to its high-resolution photographs in the natural RGB colour model, identified glacial discharges as well as the recognition of plume shapes and colours

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Summary

Introduction

The sea level of the oceans is dependent on Antarctic ice sheet shifts caused by climate change [1,2]. Antarctic Peninsula is especially vulnerable to the impact of rising temperatures, as it is one of the most rapidly warming regions in the world [3,4]. Peninsula region sensitive to changes in the basal water supply as well as sensitive to the thinning of the terminus, with faster flow leading directly to the sea level rise [7]. According to Vaughan [8], the velocity of glacier melting in this area doubled from 1950 to 2000, and provided increased meltwater and sediment influx, which changes the functional attributes of marine ecosystems [4]

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