A linear model to derive melt pond depth on Arctic sea ice from hyperspectral data

Melt ponds are key elements in the energy balance of Arctic sea ice. Observing their temporal evolution is crucial for understanding melt processes and predicting sea ice evolution. Remote sensing is the only technique that enables large-scale observations of Arctic sea ice. However, monitoring melt...

Full description

Bibliographic Details
Published in:The Cryosphere
Main Authors: M. König, N. Oppelt
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2020
Subjects:
Online Access:https://doi.org/10.5194/tc-14-2567-2020
https://doaj.org/article/49d417fc272b4f61b4268a6bba87e6a0
id ftdoajarticles:oai:doaj.org/article:49d417fc272b4f61b4268a6bba87e6a0
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:49d417fc272b4f61b4268a6bba87e6a0 2023-05-15T13:11:41+02:00 A linear model to derive melt pond depth on Arctic sea ice from hyperspectral data M. König N. Oppelt 2020-08-01T00:00:00Z https://doi.org/10.5194/tc-14-2567-2020 https://doaj.org/article/49d417fc272b4f61b4268a6bba87e6a0 EN eng Copernicus Publications https://tc.copernicus.org/articles/14/2567/2020/tc-14-2567-2020.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-14-2567-2020 1994-0416 1994-0424 https://doaj.org/article/49d417fc272b4f61b4268a6bba87e6a0 The Cryosphere, Vol 14, Pp 2567-2579 (2020) Environmental sciences GE1-350 Geology QE1-996.5 article 2020 ftdoajarticles https://doi.org/10.5194/tc-14-2567-2020 2022-12-31T11:39:08Z Melt ponds are key elements in the energy balance of Arctic sea ice. Observing their temporal evolution is crucial for understanding melt processes and predicting sea ice evolution. Remote sensing is the only technique that enables large-scale observations of Arctic sea ice. However, monitoring melt pond deepening in this way is challenging because most of the optical signal reflected by a pond is defined by the scattering characteristics of the underlying ice. Without knowing the influence of meltwater on the reflected signal, the water depth cannot be determined. To solve the problem, we simulated the way meltwater changes the reflected spectra of bare ice. We developed a model based on the slope of the log-scaled remote sensing reflectance at 710 nm as a function of depth that is widely independent from the bottom albedo and accounts for the influence of varying solar zenith angles. We validated the model using 49 in situ melt pond spectra and corresponding depths from shallow ponds on dark and bright ice. Retrieved pond depths are accurate (root mean square error, RMSE=2.81 cm n RMSE=16 %) and highly correlated with in situ measurements ( r =0.89 <math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>p</mi><mo>=</mo><mn mathvariant="normal">4.34</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">17</mn></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="81pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="e889bc451f3575818ff1fb9c7014edd0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-14-2567-2020-ie00001.svg" width="81pt" height="15pt" src="tc-14-2567-2020-ie00001.png"/></svg:svg> ). The model further explains a large portion of the variation in pond depth ( R 2 =0.74 ). Our results ... Article in Journal/Newspaper albedo Arctic Sea ice The Cryosphere Directory of Open Access Journals: DOAJ Articles Arctic The Cryosphere 14 8 2567 2579
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
M. König
N. Oppelt
A linear model to derive melt pond depth on Arctic sea ice from hyperspectral data
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description Melt ponds are key elements in the energy balance of Arctic sea ice. Observing their temporal evolution is crucial for understanding melt processes and predicting sea ice evolution. Remote sensing is the only technique that enables large-scale observations of Arctic sea ice. However, monitoring melt pond deepening in this way is challenging because most of the optical signal reflected by a pond is defined by the scattering characteristics of the underlying ice. Without knowing the influence of meltwater on the reflected signal, the water depth cannot be determined. To solve the problem, we simulated the way meltwater changes the reflected spectra of bare ice. We developed a model based on the slope of the log-scaled remote sensing reflectance at 710 nm as a function of depth that is widely independent from the bottom albedo and accounts for the influence of varying solar zenith angles. We validated the model using 49 in situ melt pond spectra and corresponding depths from shallow ponds on dark and bright ice. Retrieved pond depths are accurate (root mean square error, RMSE=2.81 cm n RMSE=16 %) and highly correlated with in situ measurements ( r =0.89 <math xmlns="http://www.w3.org/1998/Math/MathML" id="M6" display="inline" overflow="scroll" dspmath="mathml"><mrow><mi>p</mi><mo>=</mo><mn mathvariant="normal">4.34</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mrow><mo>-</mo><mn mathvariant="normal">17</mn></mrow></msup></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="81pt" height="15pt" class="svg-formula" dspmath="mathimg" md5hash="e889bc451f3575818ff1fb9c7014edd0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-14-2567-2020-ie00001.svg" width="81pt" height="15pt" src="tc-14-2567-2020-ie00001.png"/></svg:svg> ). The model further explains a large portion of the variation in pond depth ( R 2 =0.74 ). Our results ...
format Article in Journal/Newspaper
author M. König
N. Oppelt
author_facet M. König
N. Oppelt
author_sort M. König
title A linear model to derive melt pond depth on Arctic sea ice from hyperspectral data
title_short A linear model to derive melt pond depth on Arctic sea ice from hyperspectral data
title_full A linear model to derive melt pond depth on Arctic sea ice from hyperspectral data
title_fullStr A linear model to derive melt pond depth on Arctic sea ice from hyperspectral data
title_full_unstemmed A linear model to derive melt pond depth on Arctic sea ice from hyperspectral data
title_sort linear model to derive melt pond depth on arctic sea ice from hyperspectral data
publisher Copernicus Publications
publishDate 2020
url https://doi.org/10.5194/tc-14-2567-2020
https://doaj.org/article/49d417fc272b4f61b4268a6bba87e6a0
geographic Arctic
geographic_facet Arctic
genre albedo
Arctic
Sea ice
The Cryosphere
genre_facet albedo
Arctic
Sea ice
The Cryosphere
op_source The Cryosphere, Vol 14, Pp 2567-2579 (2020)
op_relation https://tc.copernicus.org/articles/14/2567/2020/tc-14-2567-2020.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-14-2567-2020
1994-0416
1994-0424
https://doaj.org/article/49d417fc272b4f61b4268a6bba87e6a0
op_doi https://doi.org/10.5194/tc-14-2567-2020
container_title The Cryosphere
container_volume 14
container_issue 8
container_start_page 2567
op_container_end_page 2579
_version_ 1766248479281119232