Eddy correlation measurements of size-dependent cloud droplet turbulent fluxes to complex terrain
Autor: | Richard J. Vong, Andrew S. Kowalski |
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Jazyk: | angličtina |
Rok vydání: | 2011 |
Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences Meteorology Turbulence Evaporation Eddy covariance Magnitude (mathematics) 010501 environmental sciences Atmospheric sciences 01 natural sciences Degree (temperature) Flux (metallurgy) Liquid water content Environmental science Precipitation 0105 earth and related environmental sciences |
Zdroj: | Tellus B; Vol 47, No 3 (1995) |
ISSN: | 0280-6509 1600-0889 |
Popis: | An eddy correlation technique was used to measure the turbulent flux of cloud droplets to complex, forested terrain near the coast of Washington State during the spring of 1993. Excellent agreement was achieved for cloud liquid water content measured by two instruments. Substantial downward liquid water fluxes of ∼ 1 mm per 24 h were measured at night during “steady and continuous” cloud events, about twice the magnitude of those measured by Beswick et al. in Scotland. Cloud water chemical fluxes were estimated to represent up to 50% of the chemical deposition associated with precipitation at the site. An observed size-dependence in the turbulent liquid water fluxes suggested that both droplet impaction, which leads to downward fluxes, and phase change processes, which can lead to upward fluxes, consistently are important contributors to the eddy correlation results. The diameter below which phase change processes were important to observed fluxes was shown to depend upon σL/L̄, the relative standard deviation of the liquid water content (LWC) within a 30-min averaging period. The crossover from upward to downward LW flux occurs at 8 µm for steady and continuous cloud events but at ∼ 13 µm for events with a larger degree of LWC variability. This comparison of the two types of cloud events suggested that evaporation was the most likely cause of upward droplet fluxes for the smaller droplets (dia < 13 µm) during cloud with variable LWC (σL/L̄ > 0.3).DOI: 10.1034/j.1600-0889.47.issue3.5.x |
Databáze: | OpenAIRE |
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