Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China
Although deforestation affects hydrological and climatic variables over tropical regions, its actual contributions to changes in evapotranspiration (ET) over subarctic China remain unknown. To establish a quantitative relationship between deforestation and terrestrial ET variations, we estimated ET...
Published in: | Forests |
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Main Authors: | , , , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2014
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Subjects: | |
Online Access: | https://doi.org/10.3390/f5102542 |
_version_ | 1821722683296972800 |
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author | Yunjun Yao Shunlin Liang Jie Cheng Yi Lin Kun Jia Meng Liu |
author_facet | Yunjun Yao Shunlin Liang Jie Cheng Yi Lin Kun Jia Meng Liu |
author_sort | Yunjun Yao |
collection | MDPI Open Access Publishing |
container_issue | 10 |
container_start_page | 2542 |
container_title | Forests |
container_volume | 5 |
description | Although deforestation affects hydrological and climatic variables over tropical regions, its actual contributions to changes in evapotranspiration (ET) over subarctic China remain unknown. To establish a quantitative relationship between deforestation and terrestrial ET variations, we estimated ET using a semi-empirical Penman (SEMI-PM) algorithm driven by meteorological and satellite data at both local and regional scales. The results indicate that the estimated ET can be used to analyse the observed inter-annual variations. There is a statistically significant positive relationship between local-scale forest cover changes (∆F) and annual ET variations (∆ET) of the following form: ∆ET = 0.0377∆F – 2.11 (R2 = 0.43, p < 0.05). This relationship may be due to deforestation-induced increases in surface albedo and a reduction in the fractional vegetation cover (FVC). However, the El Niño/Southern Oscillation (ENSO), rather than deforestation, dominates the multi-decadal ET variability due to regional-scale wind speed changes, but the exact effects of deforestation and ENSO on ET are challenging to quantify. |
format | Text |
genre | Subarctic |
genre_facet | Subarctic |
id | ftmdpi:oai:mdpi.com:/1999-4907/5/10/2542/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_container_end_page | 2560 |
op_coverage | agris |
op_doi | https://doi.org/10.3390/f5102542 |
op_relation | https://dx.doi.org/10.3390/f5102542 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Forests; Volume 5; Issue 10; Pages: 2542-2560 |
publishDate | 2014 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/1999-4907/5/10/2542/ 2025-01-17T01:00:03+00:00 Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China Yunjun Yao Shunlin Liang Jie Cheng Yi Lin Kun Jia Meng Liu agris 2014-10-23 application/pdf https://doi.org/10.3390/f5102542 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/f5102542 https://creativecommons.org/licenses/by/4.0/ Forests; Volume 5; Issue 10; Pages: 2542-2560 deforestation evapotranspiration subarctic China climate variability Text 2014 ftmdpi https://doi.org/10.3390/f5102542 2023-07-31T20:39:53Z Although deforestation affects hydrological and climatic variables over tropical regions, its actual contributions to changes in evapotranspiration (ET) over subarctic China remain unknown. To establish a quantitative relationship between deforestation and terrestrial ET variations, we estimated ET using a semi-empirical Penman (SEMI-PM) algorithm driven by meteorological and satellite data at both local and regional scales. The results indicate that the estimated ET can be used to analyse the observed inter-annual variations. There is a statistically significant positive relationship between local-scale forest cover changes (∆F) and annual ET variations (∆ET) of the following form: ∆ET = 0.0377∆F – 2.11 (R2 = 0.43, p < 0.05). This relationship may be due to deforestation-induced increases in surface albedo and a reduction in the fractional vegetation cover (FVC). However, the El Niño/Southern Oscillation (ENSO), rather than deforestation, dominates the multi-decadal ET variability due to regional-scale wind speed changes, but the exact effects of deforestation and ENSO on ET are challenging to quantify. Text Subarctic MDPI Open Access Publishing Forests 5 10 2542 2560 |
spellingShingle | deforestation evapotranspiration subarctic China climate variability Yunjun Yao Shunlin Liang Jie Cheng Yi Lin Kun Jia Meng Liu Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China |
title | Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China |
title_full | Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China |
title_fullStr | Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China |
title_full_unstemmed | Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China |
title_short | Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China |
title_sort | impacts of deforestation and climate variability on terrestrial evapotranspiration in subarctic china |
topic | deforestation evapotranspiration subarctic China climate variability |
topic_facet | deforestation evapotranspiration subarctic China climate variability |
url | https://doi.org/10.3390/f5102542 |