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Record #82320:

Changes in soil temperature caused by infiltration of snowmelt water / M. Taniguchi, I. Kayane.

Title: Changes in soil temperature caused by infiltration of snowmelt water / M. Taniguchi, I. Kayane.
Author(s): Taniguchi, M.
Kayane, I.
Date: 1986.
Publisher: Wallingford, Oxfordshire: International Association of Hydrological Sciences
In: Modelling snowmelt-induced processes. Proceedings of a Symposium held during the 2nd Scientific Assembly of the International Association of Hydrological Sciences at Budapest, Hungary, July 1986. .... (1986.),
Abstract: In order to clarify effects of infiltrating meltwater on soil temperature, thermal and hydrological conditions during snowmelt season in Nagaoka, Japan, were examined and numerical simulations of soil temperature performed. Soil temperatures at all depths in capillary zone fall in day during snowmelt season, caused by movement of soil water, pushed down by infiltrating meltwater.
Notes:

In: Modelling snowmelt-induced processes. Proceedings of a Symposium held during the 2nd Scientific Assembly of the International Association of Hydrological Sciences at Budapest, Hungary, July 1986. ... / Elizabeth M. Morris, ed.

Keywords: 631.436 -- Soils, thermal properties.
556 -- Hydrology.
551.579.2 -- Water supply from snow.
E11 -- Glaciology: glaciohydrology.
(520) -- Japan.
SPRI record no.: 82320

MARCXML

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245 10 ‡aChanges in soil temperature caused by infiltration of snowmelt water /‡cM. Taniguchi, I. Kayane.
260 ## ‡aWallingford, Oxfordshire :‡bInternational Association of Hydrological Sciences,‡c1986.
300 ## ‡ap. 93-101 :‡bdiags., table.
490 0# ‡aIAHS Publication ;‡v155
500 ## ‡aIn: Modelling snowmelt-induced processes. Proceedings of a Symposium held during the 2nd Scientific Assembly of the International Association of Hydrological Sciences at Budapest, Hungary, July 1986. ... / Elizabeth M. Morris, ed.
520 3# ‡aIn order to clarify effects of infiltrating meltwater on soil temperature, thermal and hydrological conditions during snowmelt season in Nagaoka, Japan, were examined and numerical simulations of soil temperature performed. Soil temperatures at all depths in capillary zone fall in day during snowmelt season, caused by movement of soil water, pushed down by infiltrating meltwater.
650 07 ‡a631.436 -- Soils, thermal properties.‡2udc
650 07 ‡a556 -- Hydrology.‡2udc
650 07 ‡a551.579.2 -- Water supply from snow.‡2udc
650 07 ‡aE11 -- Glaciology: glaciohydrology.‡2local
651 #7 ‡a(520) -- Japan.‡2udc
700 1# ‡aKayane, I.
773 0# ‡7nnam ‡aElizabeth M. Morris, ed. ‡tModelling snowmelt-induced processes. Proceedings of a Symposium held during the 2nd Scientific Assembly of the International Association of Hydrological Sciences at Budapest, Hungary, July 1986. .... ‡dWallingford, Oxfordshire : International Association of Hydrological Sciences, 1986. ‡wSPRI-82312
917 ## ‡aUnenhanced record from Muscat, imported 2019
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