Ocean Temperature Profiling Lidar: Analysis of Technology and Potential for Rapid Ocean Observations

Development of ocean measurement technologies can improve monitoring of the global Ocean Heat Content (OHC) and Heat Storage Rate (HSR) that serve as early-warning indices for climate-critical circulation processes such as the Atlantic Meridional Overturning Circulation and provide real-time OHC ass...

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Main Authors: John R. Moisan, Cecile S. Rousseaux, Paul R. Stysley, Gregory B. Clarke, Demetrios P. Poulios
Format: Article
Language:English
Published: MDPI AG 2024-03-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/16/7/1236
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author John R. Moisan
Cecile S. Rousseaux
Paul R. Stysley
Gregory B. Clarke
Demetrios P. Poulios
author_facet John R. Moisan
Cecile S. Rousseaux
Paul R. Stysley
Gregory B. Clarke
Demetrios P. Poulios
author_sort John R. Moisan
collection DOAJ
description Development of ocean measurement technologies can improve monitoring of the global Ocean Heat Content (OHC) and Heat Storage Rate (HSR) that serve as early-warning indices for climate-critical circulation processes such as the Atlantic Meridional Overturning Circulation and provide real-time OHC assessments for tropical cyclone forecast models. This paper examines the potential of remotely measuring ocean temperature profiles using a simulated Brillouin lidar for calculating ocean HSR. A series of data analysis (‘Nature’) and Observational Systems Simulation Experiments (OSSEs) were carried out using 26 years (1992–2017) of daily mean temperature and salinity outputs from the ECCOv4r4 ocean circulation model. The focus of this study is to compare various OSSEs carried out to measure the HSR using a simulated Brillouin lidar against the HSR calculated from the ECCOv4r4 model results. Brillouin lidar simulations are used to predict the probability of detecting a return lidar signal under varying sampling strategies. Correlations were calculated for the difference between sampling strategies. These comparisons ignore the measurement errors inherent in a Brillouin lidar. Brillouin lidar technology and instruments are known to contain numerous, instrument-dependent errors and remain an engineering challenge. A significant decrease in the ability to measuring global ocean HSRs is a consequence of measuring ocean temperature from nadir-pointing instruments that can only take measurements along-track. Other sources of errors include the inability to fully profile ocean regions with deep mixed layers, such as the Southern Ocean and North Atlantic, and ocean regions with high light attenuation levels.
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spelling doaj.art-c03f9d7e5b9d4df0a7ae509d060a8c9d2024-04-12T13:25:42ZengMDPI AGRemote Sensing2072-42922024-03-01167123610.3390/rs16071236Ocean Temperature Profiling Lidar: Analysis of Technology and Potential for Rapid Ocean ObservationsJohn R. Moisan0Cecile S. Rousseaux1Paul R. Stysley2Gregory B. Clarke3Demetrios P. Poulios4NASA Goddard Space Flight Center, Greenbelt, MD 20771, USANASA Goddard Space Flight Center, Greenbelt, MD 20771, USANASA Goddard Space Flight Center, Greenbelt, MD 20771, USANASA Goddard Space Flight Center, Greenbelt, MD 20771, USANASA Goddard Space Flight Center, Greenbelt, MD 20771, USADevelopment of ocean measurement technologies can improve monitoring of the global Ocean Heat Content (OHC) and Heat Storage Rate (HSR) that serve as early-warning indices for climate-critical circulation processes such as the Atlantic Meridional Overturning Circulation and provide real-time OHC assessments for tropical cyclone forecast models. This paper examines the potential of remotely measuring ocean temperature profiles using a simulated Brillouin lidar for calculating ocean HSR. A series of data analysis (‘Nature’) and Observational Systems Simulation Experiments (OSSEs) were carried out using 26 years (1992–2017) of daily mean temperature and salinity outputs from the ECCOv4r4 ocean circulation model. The focus of this study is to compare various OSSEs carried out to measure the HSR using a simulated Brillouin lidar against the HSR calculated from the ECCOv4r4 model results. Brillouin lidar simulations are used to predict the probability of detecting a return lidar signal under varying sampling strategies. Correlations were calculated for the difference between sampling strategies. These comparisons ignore the measurement errors inherent in a Brillouin lidar. Brillouin lidar technology and instruments are known to contain numerous, instrument-dependent errors and remain an engineering challenge. A significant decrease in the ability to measuring global ocean HSRs is a consequence of measuring ocean temperature from nadir-pointing instruments that can only take measurements along-track. Other sources of errors include the inability to fully profile ocean regions with deep mixed layers, such as the Southern Ocean and North Atlantic, and ocean regions with high light attenuation levels.https://www.mdpi.com/2072-4292/16/7/1236lidaroceantemperature profilesheat storageclimate change
spellingShingle John R. Moisan
Cecile S. Rousseaux
Paul R. Stysley
Gregory B. Clarke
Demetrios P. Poulios
Ocean Temperature Profiling Lidar: Analysis of Technology and Potential for Rapid Ocean Observations
Remote Sensing
lidar
ocean
temperature profiles
heat storage
climate change
title Ocean Temperature Profiling Lidar: Analysis of Technology and Potential for Rapid Ocean Observations
title_full Ocean Temperature Profiling Lidar: Analysis of Technology and Potential for Rapid Ocean Observations
title_fullStr Ocean Temperature Profiling Lidar: Analysis of Technology and Potential for Rapid Ocean Observations
title_full_unstemmed Ocean Temperature Profiling Lidar: Analysis of Technology and Potential for Rapid Ocean Observations
title_short Ocean Temperature Profiling Lidar: Analysis of Technology and Potential for Rapid Ocean Observations
title_sort ocean temperature profiling lidar analysis of technology and potential for rapid ocean observations
topic lidar
ocean
temperature profiles
heat storage
climate change
url https://www.mdpi.com/2072-4292/16/7/1236
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