Estimating Meltwater Drainage Onset Timing and Duration of Landfast Ice in the Canadian Arctic Archipelago Using AMSR-E Passive Microwave Data

Meltwater drainage onset (DO) timing and drainage duration (DD) related to snowmelt-water redistribution are both important for understanding not only the Arctic energy and heat budgets but also the salt/heat balance of the mixed layer in the ocean and sea-ice ecosystem. We present DO and DD as dete...

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Main Author: Yasuhiro Tanaka
Format: Article
Language:English
Published: MDPI AG 2020-03-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/6/1033
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spelling doaj-e9d5d0b3d9014b0a9d131fea39d24cd42020-11-25T00:44:43ZengMDPI AGRemote Sensing2072-42922020-03-01126103310.3390/rs12061033rs12061033Estimating Meltwater Drainage Onset Timing and Duration of Landfast Ice in the Canadian Arctic Archipelago Using AMSR-E Passive Microwave DataYasuhiro Tanaka0Earth Observation Research Center, Tsukuba Space Center, Japan Aerospace Exploration Agency, Tsukuba, Ibaraki 305-8505, JapanMeltwater drainage onset (DO) timing and drainage duration (DD) related to snowmelt-water redistribution are both important for understanding not only the Arctic energy and heat budgets but also the salt/heat balance of the mixed layer in the ocean and sea-ice ecosystem. We present DO and DD as determined from the time series of Advanced Microwave Scanning Radiometer-Earth observing system (AMSR-E) melt pond fraction (MPF) estimates in an area with Canadian landfast ice. To address the lack of evaluation on a day-by-day basis for the AMSR-E MPF estimate, we first compared AMSR-E MPF with the daily Medium Resolution Imaging Spectrometer (MERIS) MPF. The AMSR-E MPF estimate correlates significantly with the MERIS MPF (<i>r</i> = 0.73&#8722;0.83). The estimate has a product quality similar to the MERIS MPF only when the albedo is around 0.5&#8722;0.7 and a positive bias of up to 10% in areas with an albedo of 0.7&#8722;0.9, including melting snow. The DO/DD estimates are determined by using a polynomial regression curve fitted on the time series of the AMSR-E MPF. The DOs/DDs from time series of the AMSR-E and MERIS MPFs are compared, revealing consistency in both DD and DO. The DO timing from 2006 to 2011 is correlated with melt onset timing. To the best of our knowledge, our study provides the first large-scale information on both DO timing and DD.https://www.mdpi.com/2072-4292/12/6/1033sea icemelt pondlandfast icemeltwater drainagearcticpassive microwaveamsr-e
collection DOAJ
language English
format Article
sources DOAJ
author Yasuhiro Tanaka
spellingShingle Yasuhiro Tanaka
Estimating Meltwater Drainage Onset Timing and Duration of Landfast Ice in the Canadian Arctic Archipelago Using AMSR-E Passive Microwave Data
Remote Sensing
sea ice
melt pond
landfast ice
meltwater drainage
arctic
passive microwave
amsr-e
author_facet Yasuhiro Tanaka
author_sort Yasuhiro Tanaka
title Estimating Meltwater Drainage Onset Timing and Duration of Landfast Ice in the Canadian Arctic Archipelago Using AMSR-E Passive Microwave Data
title_short Estimating Meltwater Drainage Onset Timing and Duration of Landfast Ice in the Canadian Arctic Archipelago Using AMSR-E Passive Microwave Data
title_full Estimating Meltwater Drainage Onset Timing and Duration of Landfast Ice in the Canadian Arctic Archipelago Using AMSR-E Passive Microwave Data
title_fullStr Estimating Meltwater Drainage Onset Timing and Duration of Landfast Ice in the Canadian Arctic Archipelago Using AMSR-E Passive Microwave Data
title_full_unstemmed Estimating Meltwater Drainage Onset Timing and Duration of Landfast Ice in the Canadian Arctic Archipelago Using AMSR-E Passive Microwave Data
title_sort estimating meltwater drainage onset timing and duration of landfast ice in the canadian arctic archipelago using amsr-e passive microwave data
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-03-01
description Meltwater drainage onset (DO) timing and drainage duration (DD) related to snowmelt-water redistribution are both important for understanding not only the Arctic energy and heat budgets but also the salt/heat balance of the mixed layer in the ocean and sea-ice ecosystem. We present DO and DD as determined from the time series of Advanced Microwave Scanning Radiometer-Earth observing system (AMSR-E) melt pond fraction (MPF) estimates in an area with Canadian landfast ice. To address the lack of evaluation on a day-by-day basis for the AMSR-E MPF estimate, we first compared AMSR-E MPF with the daily Medium Resolution Imaging Spectrometer (MERIS) MPF. The AMSR-E MPF estimate correlates significantly with the MERIS MPF (<i>r</i> = 0.73&#8722;0.83). The estimate has a product quality similar to the MERIS MPF only when the albedo is around 0.5&#8722;0.7 and a positive bias of up to 10% in areas with an albedo of 0.7&#8722;0.9, including melting snow. The DO/DD estimates are determined by using a polynomial regression curve fitted on the time series of the AMSR-E MPF. The DOs/DDs from time series of the AMSR-E and MERIS MPFs are compared, revealing consistency in both DD and DO. The DO timing from 2006 to 2011 is correlated with melt onset timing. To the best of our knowledge, our study provides the first large-scale information on both DO timing and DD.
topic sea ice
melt pond
landfast ice
meltwater drainage
arctic
passive microwave
amsr-e
url https://www.mdpi.com/2072-4292/12/6/1033
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