Investigation of the Soil Depths Temperature Trend Using Parametric and Non-Parametric Methods (Shahrud Station)

The effects of climate change can be released from the surface to the soil depth, thereby affecting soil thermal regime. Thermal energy in the soil plays a very important role in causing climate changes. In this study, for the assessment and detection of  the climate changes, soil depths temperature...

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Main Authors: S. Shiukhy Soqanloo, S. Golshan, M. Khoshravesh
Format: Article
Language:fas
Published: Isfahan University of Technology 2019-03-01
Series:علوم آب و خاک
Subjects:
Online Access:http://jstnar.iut.ac.ir/article-1-3456-en.html
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author S. Shiukhy Soqanloo
S. Golshan
M. Khoshravesh
author_facet S. Shiukhy Soqanloo
S. Golshan
M. Khoshravesh
author_sort S. Shiukhy Soqanloo
collection DOAJ
description The effects of climate change can be released from the surface to the soil depth, thereby affecting soil thermal regime. Thermal energy in the soil plays a very important role in causing climate changes. In this study, for the assessment and detection of  the climate changes, soil depths temperature, the measured data related to the  daily air temperature at a height of 2 meters (screen) during the years (1951-2014), and the soil depths daily temperature (5-10-20-30-50 to 100 cm), for 3, 9 and 15 hours, were obtained during a period (1992-2014) in Shahrud station. The climate change detection was employed to compare the treatment mean. As well, for detection of trends related to the annual, seasonal and monthly time series and their relation to the soil depths temperature, parametric methods (regression analysis and Pearson) and nonparametric (Mann-Kendall, Spearman) were applied. The results showed that the soil temperature was increased in all months except January, February and March. Also, in the seasonal time series, the soil depths temperature was increased in all seasons except winter. In fact, based on the results, the soil temperature in spring, summer and autumn was increased. Detection trends of the annual soil depths temperature showed that, except for the Pearson correlation coefficient method, soil temperature was increased at all soil depths.
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spelling doaj.art-72d87ee5cabc42a8a2578f3b7a204a7b2022-12-21T23:51:08ZfasIsfahan University of Technologyعلوم آب و خاک2476-35942476-55542019-03-012242939Investigation of the Soil Depths Temperature Trend Using Parametric and Non-Parametric Methods (Shahrud Station)S. Shiukhy Soqanloo0S. Golshan1M. Khoshravesh2 1. Department of Water Engineering, Faculty of Agricultural Engineering, Sari Agricultural Sciences and Natural Resources University, Sari, Iran. 1. Department of Water Engineering, Faculty of Agricultural Engineering, Sari Agricultural Sciences and Natural Resources University, Sari, Iran. 1. Department of Water Engineering, Faculty of Agricultural Engineering, Sari Agricultural Sciences and Natural Resources University, Sari, Iran. The effects of climate change can be released from the surface to the soil depth, thereby affecting soil thermal regime. Thermal energy in the soil plays a very important role in causing climate changes. In this study, for the assessment and detection of  the climate changes, soil depths temperature, the measured data related to the  daily air temperature at a height of 2 meters (screen) during the years (1951-2014), and the soil depths daily temperature (5-10-20-30-50 to 100 cm), for 3, 9 and 15 hours, were obtained during a period (1992-2014) in Shahrud station. The climate change detection was employed to compare the treatment mean. As well, for detection of trends related to the annual, seasonal and monthly time series and their relation to the soil depths temperature, parametric methods (regression analysis and Pearson) and nonparametric (Mann-Kendall, Spearman) were applied. The results showed that the soil temperature was increased in all months except January, February and March. Also, in the seasonal time series, the soil depths temperature was increased in all seasons except winter. In fact, based on the results, the soil temperature in spring, summer and autumn was increased. Detection trends of the annual soil depths temperature showed that, except for the Pearson correlation coefficient method, soil temperature was increased at all soil depths.http://jstnar.iut.ac.ir/article-1-3456-en.htmlaverage of annual temperaturedaily temperaturetime seriesthermal energy
spellingShingle S. Shiukhy Soqanloo
S. Golshan
M. Khoshravesh
Investigation of the Soil Depths Temperature Trend Using Parametric and Non-Parametric Methods (Shahrud Station)
علوم آب و خاک
average of annual temperature
daily temperature
time series
thermal energy
title Investigation of the Soil Depths Temperature Trend Using Parametric and Non-Parametric Methods (Shahrud Station)
title_full Investigation of the Soil Depths Temperature Trend Using Parametric and Non-Parametric Methods (Shahrud Station)
title_fullStr Investigation of the Soil Depths Temperature Trend Using Parametric and Non-Parametric Methods (Shahrud Station)
title_full_unstemmed Investigation of the Soil Depths Temperature Trend Using Parametric and Non-Parametric Methods (Shahrud Station)
title_short Investigation of the Soil Depths Temperature Trend Using Parametric and Non-Parametric Methods (Shahrud Station)
title_sort investigation of the soil depths temperature trend using parametric and non parametric methods shahrud station
topic average of annual temperature
daily temperature
time series
thermal energy
url http://jstnar.iut.ac.ir/article-1-3456-en.html
work_keys_str_mv AT sshiukhysoqanloo investigationofthesoildepthstemperaturetrendusingparametricandnonparametricmethodsshahrudstation
AT sgolshan investigationofthesoildepthstemperaturetrendusingparametricandnonparametricmethodsshahrudstation
AT mkhoshravesh investigationofthesoildepthstemperaturetrendusingparametricandnonparametricmethodsshahrudstation