Aerosol Deposition and Behavior on Leaves in Cool-temperate Deciduous Forests. Part 3: Estimation of Fog Deposition onto Cool-temperate Deciduous Forest by the Inferential Method
Fog deposition onto the cool-temperate deciduous forest around Lake Mashu in northern Japan was estimated by the inferential method using the parameterizations of deposition velocity and liquid water content of fog (LWC). Two parameterizations of fog deposition velocity derived from field experiment...
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doaj-df59876281634acd82647e0155abd87f2020-11-25T03:31:50ZengAsian Association for Atmospheric EnvironmentAsian Journal of Atmospheric Environment1976-69122287-11602013-03-0171172410.5572/ajae.2013.7.1.017Aerosol Deposition and Behavior on Leaves in Cool-temperate Deciduous Forests. Part 3: Estimation of Fog Deposition onto Cool-temperate Deciduous Forest by the Inferential MethodGenki Katata0Takashi Yamaguchi1Haruna Sato2Yoko Watanabe3Izumi Noguchi4Hiroshi Hara5Haruyasu Nagai6Research Group for Environmental Science, Japan Atomic Energy Agency, Ibaraki 319-1195, JapanEnvironmental Conservation Division, Hokkaido Research Organization, Sapporo 060-0819, JapanField Science Center, Tokyo University of Agriculture and Technology, Tokyo 183-8538, JapanField Science Center for Northern Biosphere, Hokkaido University, Sapporo 060-0809, JapanEnvironmental Conservation Division, Hokkaido Research Organization, Sapporo 060-0819, JapanField Science Center, Tokyo University of Agriculture and Technology, Tokyo 183-8538, JapanResearch Group for Environmental Science, Japan Atomic Energy Agency, Ibaraki 319-1195, JapanFog deposition onto the cool-temperate deciduous forest around Lake Mashu in northern Japan was estimated by the inferential method using the parameterizations of deposition velocity and liquid water content of fog (LWC). Two parameterizations of fog deposition velocity derived from field experiments in Europe and numerical simulations using a detailed multi-layer atmosphere-vegetation-soil model were tested. The empirical function between horizontal visibility (VIS) and LWC was applied to produce hourly LWC as an input data for the inferential method. Weekly mean LWC computed from VIS had a good correlation with LWC sampled by an active string-fog collector. By considering the enhancement of fog deposition due to the edge effect, fog deposition calculated by the inferential method using two parameterizations of deposition velocity agreed with that computed from throughfall data. The results indicated that the inferential method using the current parameterizations of deposition velocity and LWC can provide a rough estimation of water input due to fog deposition onto cool-temperature deciduous forests. Limitations of current parameterizations of deposition velocity related to wind speed, evaporation loss of rain and fog droplets intercepted by tree canopies, and leaf area index were discussed.http://asianjae.org/_common/do.php?a=full&b=11&bidx=1567&aidx=19764fog depositioninferential methodparameterizationvisibilityliquid water contentdeposition velocitydeciduous forestleaf area index |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Genki Katata Takashi Yamaguchi Haruna Sato Yoko Watanabe Izumi Noguchi Hiroshi Hara Haruyasu Nagai |
spellingShingle |
Genki Katata Takashi Yamaguchi Haruna Sato Yoko Watanabe Izumi Noguchi Hiroshi Hara Haruyasu Nagai Aerosol Deposition and Behavior on Leaves in Cool-temperate Deciduous Forests. Part 3: Estimation of Fog Deposition onto Cool-temperate Deciduous Forest by the Inferential Method Asian Journal of Atmospheric Environment fog deposition inferential method parameterization visibility liquid water content deposition velocity deciduous forest leaf area index |
author_facet |
Genki Katata Takashi Yamaguchi Haruna Sato Yoko Watanabe Izumi Noguchi Hiroshi Hara Haruyasu Nagai |
author_sort |
Genki Katata |
title |
Aerosol Deposition and Behavior on Leaves in Cool-temperate Deciduous Forests. Part 3: Estimation of Fog Deposition onto Cool-temperate Deciduous Forest by the Inferential Method |
title_short |
Aerosol Deposition and Behavior on Leaves in Cool-temperate Deciduous Forests. Part 3: Estimation of Fog Deposition onto Cool-temperate Deciduous Forest by the Inferential Method |
title_full |
Aerosol Deposition and Behavior on Leaves in Cool-temperate Deciduous Forests. Part 3: Estimation of Fog Deposition onto Cool-temperate Deciduous Forest by the Inferential Method |
title_fullStr |
Aerosol Deposition and Behavior on Leaves in Cool-temperate Deciduous Forests. Part 3: Estimation of Fog Deposition onto Cool-temperate Deciduous Forest by the Inferential Method |
title_full_unstemmed |
Aerosol Deposition and Behavior on Leaves in Cool-temperate Deciduous Forests. Part 3: Estimation of Fog Deposition onto Cool-temperate Deciduous Forest by the Inferential Method |
title_sort |
aerosol deposition and behavior on leaves in cool-temperate deciduous forests. part 3: estimation of fog deposition onto cool-temperate deciduous forest by the inferential method |
publisher |
Asian Association for Atmospheric Environment |
series |
Asian Journal of Atmospheric Environment |
issn |
1976-6912 2287-1160 |
publishDate |
2013-03-01 |
description |
Fog deposition onto the cool-temperate deciduous forest around Lake Mashu in northern Japan was estimated by the inferential method using the parameterizations of deposition velocity and liquid water content of fog (LWC). Two parameterizations of fog deposition velocity derived from field experiments in Europe and numerical simulations using a detailed multi-layer atmosphere-vegetation-soil model were tested. The empirical function between horizontal visibility (VIS) and LWC was applied to produce hourly LWC as an input data for the inferential method. Weekly mean LWC computed from VIS had a good correlation with LWC sampled by an active string-fog collector. By considering the enhancement of fog deposition due to the edge effect, fog deposition calculated by the inferential method using two parameterizations of deposition velocity agreed with that computed from throughfall data. The results indicated that the inferential method using the current parameterizations of deposition velocity and LWC can provide a rough estimation of water input due to fog deposition onto cool-temperature deciduous forests. Limitations of current parameterizations of deposition velocity related to wind speed, evaporation loss of rain and fog droplets intercepted by tree canopies, and leaf area index were discussed. |
topic |
fog deposition inferential method parameterization visibility liquid water content deposition velocity deciduous forest leaf area index |
url |
http://asianjae.org/_common/do.php?a=full&b=11&bidx=1567&aidx=19764 |
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