Difference in snowmelt processes between an opening and three Japanese cedar stands

Snowmelt was measured on a daily basis for 17 days at the open site and 18 days at three Japanese cedar sites with canopy closure of 17.8% (cedar stand A), 5.2% (B) and 2.4% (C) in April. Measured daily snowmelt at each site was reproduced by heat-balance calculation with an accuracy of <±1 mm w....

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Main Authors: Shigeki Murakami, Yukari Takeuchi
Format: Article
Language:English
Published: Cambridge University Press 2018-12-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0260305518000216/type/journal_article
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author Shigeki Murakami
Yukari Takeuchi
author_facet Shigeki Murakami
Yukari Takeuchi
author_sort Shigeki Murakami
collection DOAJ
description Snowmelt was measured on a daily basis for 17 days at the open site and 18 days at three Japanese cedar sites with canopy closure of 17.8% (cedar stand A), 5.2% (B) and 2.4% (C) in April. Measured daily snowmelt at each site was reproduced by heat-balance calculation with an accuracy of <±1 mm w.e. From 1st April to the date of snow disappearance net radiation accounted for 88.4, 43.0, 32.7 and 34.2% of total snowmelt energy at the open site, the cedar stands A, B and C, respectively. The ratio of sensible and latent heat to total snowmelt was 33.1–37.9 and 25.9–29.4%, respectively, at three cedar stands. The ratios of sensible and latent heat increased over time in accordance with the rise in temperature at all cedar sites. They became large on a daily basis when air temperature and/or wind speed were high. Wind speed is dependent on morphology around each site that also dictated snowmelt.
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spelling doaj.art-a910f72eb06b4235ace363df4a49db0e2023-03-09T12:27:35ZengCambridge University PressAnnals of Glaciology0260-30551727-56442018-12-0159414910.1017/aog.2018.21Difference in snowmelt processes between an opening and three Japanese cedar standsShigeki Murakami0Yukari Takeuchi1Kyushu Research Center, Forestry and Forest Products Research Institute, 4-11-16 Kurokami, Chuo, Kumamoto, 860-0862, Japan. Email:Tohkamachi Experimental Station, Forestry and Forest Products Research Institute, 614-9 Kawahara-cho, Tokamachi-shi, Niigata, 948-0013, JapanSnowmelt was measured on a daily basis for 17 days at the open site and 18 days at three Japanese cedar sites with canopy closure of 17.8% (cedar stand A), 5.2% (B) and 2.4% (C) in April. Measured daily snowmelt at each site was reproduced by heat-balance calculation with an accuracy of <±1 mm w.e. From 1st April to the date of snow disappearance net radiation accounted for 88.4, 43.0, 32.7 and 34.2% of total snowmelt energy at the open site, the cedar stands A, B and C, respectively. The ratio of sensible and latent heat to total snowmelt was 33.1–37.9 and 25.9–29.4%, respectively, at three cedar stands. The ratios of sensible and latent heat increased over time in accordance with the rise in temperature at all cedar sites. They became large on a daily basis when air temperature and/or wind speed were high. Wind speed is dependent on morphology around each site that also dictated snowmelt.https://www.cambridge.org/core/product/identifier/S0260305518000216/type/journal_articleforestheat balancesnowmeltsnow water equivalent
spellingShingle Shigeki Murakami
Yukari Takeuchi
Difference in snowmelt processes between an opening and three Japanese cedar stands
Annals of Glaciology
forest
heat balance
snowmelt
snow water equivalent
title Difference in snowmelt processes between an opening and three Japanese cedar stands
title_full Difference in snowmelt processes between an opening and three Japanese cedar stands
title_fullStr Difference in snowmelt processes between an opening and three Japanese cedar stands
title_full_unstemmed Difference in snowmelt processes between an opening and three Japanese cedar stands
title_short Difference in snowmelt processes between an opening and three Japanese cedar stands
title_sort difference in snowmelt processes between an opening and three japanese cedar stands
topic forest
heat balance
snowmelt
snow water equivalent
url https://www.cambridge.org/core/product/identifier/S0260305518000216/type/journal_article
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