Abstract

The north and south poles of the earth (hereinafter referred to as the polar regions) are important components of the earth system. Changes in the material balance and movement of the polar ice shelf reflect the influence of the polar regions on global climate change and are also a response to global climate change. Through a comprehensive investigation of ice-shelf kinematics, with sufficient accuracy, it is possible to obtain ice-shelf elevation, movement-state data, ice-shelf material balance state, and the ice-shelf movement dynamics mechanism. Due to the extremely harsh environment in polar regions, remote sensing is currently widely used. Manual and equipment monitoring methods show insufficient accuracy or discontinuous time series. There is an urgent need to obtain continuous real-time ice-shelf kinematics-related parameters on the ground to verify the reliability of the parameters obtained by satellite remote sensing. These parameters should be combined with remote sensing monitoring to provide data support. In this paper, a monitoring system for the movement of polar ice and shelf ice cover is developed, and it is proposed that various data can be acquired by integrating high-precision GPS (global positioning system) and other sensors. Solutions to the problem of low-temperature power supply in the polar regions, data acquisition and storage strategies, and remote communication methods are proposed. Testing and remote sensing validation verified that the developed acquisition system can fulfill the requirements for monitoring the movement of the polar unmanned ice shelves and ice sheets.

Highlights

  • With the advent of satellite remote sensing technology and new measuring technology, more and larger-scale parameters related to iceshelf kinematics have been obtained, including the grounding line of the ice shelf, ice flow velocity, strain rate, ice elevation, ice-shelf thickness and width, net surface accumulation rate, bottom freeze-thaw rate, and tidal information related to vertical height changes of the ice shelf [5]

  • The large-area instantaneous imaging characteristics of remote sensing technology have greatly promoted the study of ice-shelf kinematics, but the reliability of the parameters obtained by satellite remote sensing still needs validation using observations from ground stations

  • Sensors 2021, 21, 7822 ice-shelf kinematics, but the reliability of the parameters obtained by satellite remote sensing still needs validation using observations from ground stations

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Summary

Introduction

Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations. With the advent of satellite remote sensing technology and new measuring technology, more and larger-scale parameters related to iceshelf kinematics have been obtained, including the grounding line of the ice shelf, ice flow velocity, strain rate, ice elevation, ice-shelf thickness and width, net surface accumulation rate, bottom freeze-thaw rate, and tidal information related to vertical height changes of the ice shelf [5]. The large-area instantaneous imaging characteristics of remote sensing technology have greatly promoted the study of ice-shelf kinematics, but the reliability of the parameters obtained by satellite remote sensing still needs validation using observations from ground stations. Data of large-area instantaneous observations [14]

Overall
Hardware Design
The Core Processor
Data Storage
GPS Data Collection
Intelligent Solar Energy Power-Management System
Communication
Embedded Software System
Absolute Position
Relative Positioning
Selection of System Observation Strategies
System Test
Test of the GPS Receiver Positioning Measurement Error
Ordinary Point Positioning and Precise Point Positioning
Test of the System-Monitoring Error
Test of the Power-Management System
Test of Other Features
Operation in Antarctic Regions
Remote Sensing Validation
GPS Monitoring Data
High-Resolution Remote Sensing Image
11 August 2018
Result Analysis
Expectation
Full Text
Published version (Free)

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