A characteristic feature of diurnal air temperature variation in the upper Yellow River valley in a semi-arid region

Hisashi Yoshikoshi, Tetsuo Kobayashi, Weizhen Wang, Daisuke Yasutake

研究成果: ジャーナルへの寄稿記事

2 引用 (Scopus)

抄録

In the upper Yellow River valley in a semi-arid region, the surface air temperature is high in the late afternoon and often peaking after 16:30 local time, and then decreasing rapidly during the growing season. To investigate this characteristic phenomenon, an intensive measurement of the heat budget of bare-soil surfaces was carried out at a field in the upper Yellow River valley in April 2008. Consequently, this phenomenon was found to occur at this field in the spring. The wind strengthened in the late afternoon, which was a valley breeze, and subsided after sunset, meanwhile the sensible heat flux was positive and remained considerable until sunset. Furthermore, the specific humidity decreased to minimal values when the air temperature approached its maximum for the day. These results suggest that the wind caused the vertical transport of the hot and dry air from the upper air advected from the surrounding desert, and maintained higher surface air temperatures, along with the large flux of sensible heat in the late afternoon. After sunset, however, the radiative cooling dominated the heat budget of the surface air layer and the air temperature decreased rapidly.

元の言語英語
ページ(範囲)215-219
ページ数5
ジャーナルjournal of agricultural meteorology
65
発行部数2
DOI
出版物ステータス出版済み - 1 1 2009

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Yellow River
semiarid region
arid zones
air temperature
valleys
heat
valley
heat budget
river
air
surface temperature
sensible heat flux
bare soil
deserts
humidity
soil surface
growing season
cooling
desert
soil

All Science Journal Classification (ASJC) codes

  • Agronomy and Crop Science
  • Atmospheric Science

これを引用

A characteristic feature of diurnal air temperature variation in the upper Yellow River valley in a semi-arid region. / Yoshikoshi, Hisashi; Kobayashi, Tetsuo; Wang, Weizhen; Yasutake, Daisuke.

:: journal of agricultural meteorology, 巻 65, 番号 2, 01.01.2009, p. 215-219.

研究成果: ジャーナルへの寄稿記事

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abstract = "In the upper Yellow River valley in a semi-arid region, the surface air temperature is high in the late afternoon and often peaking after 16:30 local time, and then decreasing rapidly during the growing season. To investigate this characteristic phenomenon, an intensive measurement of the heat budget of bare-soil surfaces was carried out at a field in the upper Yellow River valley in April 2008. Consequently, this phenomenon was found to occur at this field in the spring. The wind strengthened in the late afternoon, which was a valley breeze, and subsided after sunset, meanwhile the sensible heat flux was positive and remained considerable until sunset. Furthermore, the specific humidity decreased to minimal values when the air temperature approached its maximum for the day. These results suggest that the wind caused the vertical transport of the hot and dry air from the upper air advected from the surrounding desert, and maintained higher surface air temperatures, along with the large flux of sensible heat in the late afternoon. After sunset, however, the radiative cooling dominated the heat budget of the surface air layer and the air temperature decreased rapidly.",
author = "Hisashi Yoshikoshi and Tetsuo Kobayashi and Weizhen Wang and Daisuke Yasutake",
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AU - Wang, Weizhen

AU - Yasutake, Daisuke

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N2 - In the upper Yellow River valley in a semi-arid region, the surface air temperature is high in the late afternoon and often peaking after 16:30 local time, and then decreasing rapidly during the growing season. To investigate this characteristic phenomenon, an intensive measurement of the heat budget of bare-soil surfaces was carried out at a field in the upper Yellow River valley in April 2008. Consequently, this phenomenon was found to occur at this field in the spring. The wind strengthened in the late afternoon, which was a valley breeze, and subsided after sunset, meanwhile the sensible heat flux was positive and remained considerable until sunset. Furthermore, the specific humidity decreased to minimal values when the air temperature approached its maximum for the day. These results suggest that the wind caused the vertical transport of the hot and dry air from the upper air advected from the surrounding desert, and maintained higher surface air temperatures, along with the large flux of sensible heat in the late afternoon. After sunset, however, the radiative cooling dominated the heat budget of the surface air layer and the air temperature decreased rapidly.

AB - In the upper Yellow River valley in a semi-arid region, the surface air temperature is high in the late afternoon and often peaking after 16:30 local time, and then decreasing rapidly during the growing season. To investigate this characteristic phenomenon, an intensive measurement of the heat budget of bare-soil surfaces was carried out at a field in the upper Yellow River valley in April 2008. Consequently, this phenomenon was found to occur at this field in the spring. The wind strengthened in the late afternoon, which was a valley breeze, and subsided after sunset, meanwhile the sensible heat flux was positive and remained considerable until sunset. Furthermore, the specific humidity decreased to minimal values when the air temperature approached its maximum for the day. These results suggest that the wind caused the vertical transport of the hot and dry air from the upper air advected from the surrounding desert, and maintained higher surface air temperatures, along with the large flux of sensible heat in the late afternoon. After sunset, however, the radiative cooling dominated the heat budget of the surface air layer and the air temperature decreased rapidly.

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