Controls on open water evaporation

Abstract

The paper presents the initial results of a field study of boundary layer behaviour and open water evaporation carried out on two small- to medium-sized lakes in Western and Northern Canada. Meteorological and boundary layer measurements were made over the water surfaces and over the upwind land surface, allowing for an examination of the effect of lake-land contrasts of temperature on the wind speed over the open water and on the evaporation rates. Lake evaporation was measured directly using eddy covariance equipment. <br><br> The study showed that, for time periods shorter than daily, the open water evaporation bears no relationship to the net radiation. The wind speed is the most significant factor governing the evaporation rates, followed by the land-water temperature contrast and the land-water vapour pressure contrast. The effect of the stability on the wind field is demonstrated; stability over the water and adjacent land surfaces are, for the most part, out of phase. The derived relationships will be used to develop a model for estimating the hourly evaporation rates from open water. <br><br> Examination of the seasonal trends shows that the open water period can be separated into two distinct evaporative regimes: the warming period in the Spring, when the land temperature is greater than the water temperature, the turbulent fluxes over water are suppressed; and the cooling period, when the water temperature is greater than the air temperature, and the turbulent fluxes over water are enhanced

Connectivity and runoff dynamics in heterogeneous basins

“…Lake outflow, Q o (mm · d −1 ), was taken to be the Δ S det , l remaining after losses to lake evaporation E l (mm·d −1 ). The latter was estimated from daily measurements from an eddy covariance system on a rock outcrop in Landing Lake (Granger and Hedstrom, 2010).…”

Refining understanding of hydrological connectivity in a boreal catchment

“…Additionally, there were losses from lake evaporation. Granger and Hedstrom () estimated summer rates from lakes in the Baker Creek watershed of approximately 3 mm/day. In concert with outflow, these losses can rapidly deplete lake detention storage, which would not have been large because 25% of the snowmelt inputs went into addressing lake storage deficits.…”

Aplikasi Satelit Dalam Mengestimasi Evaporasi Di Daerah Waduk (Studi Kasus: Waduk Saguling-Jawa Barat)

“…Proses evaporasi menentukan kadar uap air di atmosfer yang merupakan salah satu faktor penting untuk keberlangsungan proses pembentukan awan dan presipitasi. Evaporasi badan air adalah komponen penting dari siklus energi dan hidrologi untuk waduk (Granger & Hedstrom, 2010). Evaporasi air terbuka seperti penguapan waduk dapat menunjukkan evaporasi potensial regional (Vercauteren et al, 2009).…”