Remote sensing of seawater and drifting ice in Svalbard fjords by compact Raman LIDAR

TL;DR

This paper presents a lightweight, high-sensitivity compact Raman LIDAR system designed for remote sensing of seawater and drifting ice, demonstrated in Svalbard fjords to analyze water properties influenced by glaciers and open sea.

Contribution

The paper introduces a novel compact Raman LIDAR system suitable for deployment on various vehicles, enabling detailed remote sensing of oceanographic parameters in icy Arctic environments.

Findings

The LIDAR system successfully mapped temperature, phytoplankton, and organic matter distributions.

Glacier influence on water properties was quantitatively characterized.

The system's low weight and power make it suitable for unmanned Arctic monitoring.

Abstract

A compact Raman LIDAR system for remote sensing of sea and drifting ice was developed at the Wave Research Center at the Prokhorov General Physics Institute of the RAS. The developed system is based on a diode pumped solid state YVO4:Nd laser combined with compact spectrograph equipped with gated detector. The system exhibits high sensitivity and can be used for mapping or depth profiling of different parameters within many oceanographic problems. Light weight (~20 kg) and low power consumption (300 W) make possible to install the device on any vehicle including unmanned aircraft or submarine system. The Raman LIDAR presented was used for Svalbard fjords study and analysis of different influence of the open sea and glaciers on the water properties. Temperature, phytoplankton, and dissolved organic matter distributions in the seawater were studied in the Ice Fjord, Van Mijen Fjord and Rinders Fjord. Drifting ice and seawater in the Rinders Fjord were characterized by the Raman spectroscopy and fluorescence. It was found that the Paula Glacier strongly influences the water temperature and chlorophyll distributions in the Van Mijen Fjord and Rinders Fjord. Possible applications of compact LIDAR systems for express monitoring of seawater in the places with high concentration of floating ice or near cold streams in the Arctic Ocean are discussed