Development of a Shallow-Depth Soil Temperature Estimation Model Based on Air Temperatures and Soil Water Contents in a Permafrost Area

A model for predicting shallow depth soil temperatures is important and effective to assess the changes in soil conditions related to global climate change and local disturbances. Shallow-depth soil temperature estimation model in cold region in Alaska is developed based on thermal response using ai...

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Main Authors: Keunbo Park, Yongwon Kim, Kichoel Lee, Dongwook Kim
Format: Article
Language:English
Published: MDPI AG 2020-02-01
Series:Applied Sciences
Subjects:
Online Access:https://www.mdpi.com/2076-3417/10/3/1058
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spelling doaj-eadc3f6aee7d453197680a2500d9969f2020-11-25T01:46:20ZengMDPI AGApplied Sciences2076-34172020-02-01103105810.3390/app10031058app10031058Development of a Shallow-Depth Soil Temperature Estimation Model Based on Air Temperatures and Soil Water Contents in a Permafrost AreaKeunbo Park0Yongwon Kim1Kichoel Lee2Dongwook Kim3Division of Polar Climate Sciences, Korea Polar Research Institute, Incheon 21990, KoreaInternational Arctic Research Center (IARC), University of Alaska Fairbanks (UAF), Fairbanks, AK 99775-7340, USADepartment of Civil and Environmental Engineering, Incheon National University, Incheon 22012, KoreaDepartment of Civil and Environmental Engineering, Incheon National University, Incheon 22012, KoreaA model for predicting shallow depth soil temperatures is important and effective to assess the changes in soil conditions related to global climate change and local disturbances. Shallow-depth soil temperature estimation model in cold region in Alaska is developed based on thermal response using air temperature and shallow-depth soil water content during active layer development period of 160 days from May to October. Among the seven soil temperature measurement sites, data from four sites were used for model development, and the remaining three sites were used for model validation. Near the middle of the seven measurement sites, air temperature is monitored at one location. The proposed model implemented concepts of thermal response and cumulative temperature. Temperatures and soil water contents were measured using automated remote sensing technology. Consequently, it was confirmed that the developed model enables fast and accurate assessment of shallow-depth soil temperature during active soil layer development period.https://www.mdpi.com/2076-3417/10/3/1058air temperaturesoil temperaturesoil temperature modellingpermafrost dynamicssoil water content
collection DOAJ
language English
format Article
sources DOAJ
author Keunbo Park
Yongwon Kim
Kichoel Lee
Dongwook Kim
spellingShingle Keunbo Park
Yongwon Kim
Kichoel Lee
Dongwook Kim
Development of a Shallow-Depth Soil Temperature Estimation Model Based on Air Temperatures and Soil Water Contents in a Permafrost Area
Applied Sciences
air temperature
soil temperature
soil temperature modelling
permafrost dynamics
soil water content
author_facet Keunbo Park
Yongwon Kim
Kichoel Lee
Dongwook Kim
author_sort Keunbo Park
title Development of a Shallow-Depth Soil Temperature Estimation Model Based on Air Temperatures and Soil Water Contents in a Permafrost Area
title_short Development of a Shallow-Depth Soil Temperature Estimation Model Based on Air Temperatures and Soil Water Contents in a Permafrost Area
title_full Development of a Shallow-Depth Soil Temperature Estimation Model Based on Air Temperatures and Soil Water Contents in a Permafrost Area
title_fullStr Development of a Shallow-Depth Soil Temperature Estimation Model Based on Air Temperatures and Soil Water Contents in a Permafrost Area
title_full_unstemmed Development of a Shallow-Depth Soil Temperature Estimation Model Based on Air Temperatures and Soil Water Contents in a Permafrost Area
title_sort development of a shallow-depth soil temperature estimation model based on air temperatures and soil water contents in a permafrost area
publisher MDPI AG
series Applied Sciences
issn 2076-3417
publishDate 2020-02-01
description A model for predicting shallow depth soil temperatures is important and effective to assess the changes in soil conditions related to global climate change and local disturbances. Shallow-depth soil temperature estimation model in cold region in Alaska is developed based on thermal response using air temperature and shallow-depth soil water content during active layer development period of 160 days from May to October. Among the seven soil temperature measurement sites, data from four sites were used for model development, and the remaining three sites were used for model validation. Near the middle of the seven measurement sites, air temperature is monitored at one location. The proposed model implemented concepts of thermal response and cumulative temperature. Temperatures and soil water contents were measured using automated remote sensing technology. Consequently, it was confirmed that the developed model enables fast and accurate assessment of shallow-depth soil temperature during active soil layer development period.
topic air temperature
soil temperature
soil temperature modelling
permafrost dynamics
soil water content
url https://www.mdpi.com/2076-3417/10/3/1058
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AT kichoellee developmentofashallowdepthsoiltemperatureestimationmodelbasedonairtemperaturesandsoilwatercontentsinapermafrostarea
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