Evapotranspiration Rate during the Growing Season in Fuhrengawa Mire, Hokkaido, Japan

Yazaki, Tomotsugu; Urano, Shin-ichi; Yabe, Kazuo; Kawauchi, Kunio

doi:10.2480/agrmet.785

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2010

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“…However, fog deposition in our study was measured in a flatland mire, which has been only slightly examined. The water supply by advection fog was 20 of the daily evapotranspirative water loss from this mire (approximately 3 mm on average; Yazaki et al, 2005). Accordingly, the advection-fog water supply is not negligible to consider the water balance of the mire.…”

Section: Resultsmentioning

confidence: 95%

Fog deposition measurement in a wetland developed at a flat terrain in the Pacific coast of eastern Hokkaido, northern Japan

Yazaki¹,

Urano²,

Yabe³

2010

J. Agric. Meteorol.

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Fog might play an important role in the water balance in foggy regions. We measured the amount of fog deposition (deposition of fog and dew waters) using lysimeters in a flatland mire on the Pacific coast of eastern Hokkaido Island. During five observed nights, summer fog was observed on four nights: one night had advection fog and three nights had radiation fog. The amount of advection-fog deposition per night was 0.6 mm on average, reaching 20 of the daily evapotranspirative water loss from this mire. This value suggests that the advection-fog water supply is not negligible. In contrast, the amount of radiation-fog water supply per night was much smaller than the other terms of water balance such as rainfall and evapotranspiration, indicating that the amount of radiation-fog deposition is negligibly small.

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Section: Resultsmentioning

confidence: 95%