THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION
Autor(a) principal: | |
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Data de Publicação: | 2023 |
Outros Autores: | |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Ra'e Ga (Online) |
Texto Completo: | https://revistas.ufpr.br/raega/article/view/93530 |
Resumo: | Cloud water interception (CWI) occurs when water contained in fog and wind-driven rain collides with vegetation, merges into larger droplets, and precipitates to the ground. CWI has an important function as an additional source of water and its relationships with tropical cloud forests have often been emphasized. Despite its importance, there is no standardization of measurement methods, nor of the terms that designate the process in Portuguese. Therefore, a systematic analysis of research on CWI is necessary. To this end, the present study carried out a review of the theoretical and methodological aspects of CWI through description and analysis of terminology; history and chronology of studies on the topic; survey of the environmental conditions necessary for the CWI process to occur; analysis of methodological aspects relating to the measurement of CWI; and synthesis and discussion of magnitudes described in scientific literature. As a result, of the 31 publications reviewed, 14 different words were found, the most common being “Cloud Water Interception” (19.4%) and “Fog Drip” (16.1%). In general, CWI is more common in places such as continental edges and islands that are constantly subject to sea breezes. In most cases, the below-canopy measurement approach can be considered more accurate than those obtained by fog collectors. CWI is on average responsible for 42% of effective precipitation (n:41). The values listed show a large variation, between 0.5% and 462%, probably due to the different environmental characteristics of the sampled locations as well as variations in sample sizes. |
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THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTIONPhysical Geography, Hidrology, Mountain HydrologyHydrological monitoring, Tropical Cloud Forests, Stemflow.Cloud water interception (CWI) occurs when water contained in fog and wind-driven rain collides with vegetation, merges into larger droplets, and precipitates to the ground. CWI has an important function as an additional source of water and its relationships with tropical cloud forests have often been emphasized. Despite its importance, there is no standardization of measurement methods, nor of the terms that designate the process in Portuguese. Therefore, a systematic analysis of research on CWI is necessary. To this end, the present study carried out a review of the theoretical and methodological aspects of CWI through description and analysis of terminology; history and chronology of studies on the topic; survey of the environmental conditions necessary for the CWI process to occur; analysis of methodological aspects relating to the measurement of CWI; and synthesis and discussion of magnitudes described in scientific literature. As a result, of the 31 publications reviewed, 14 different words were found, the most common being “Cloud Water Interception” (19.4%) and “Fog Drip” (16.1%). In general, CWI is more common in places such as continental edges and islands that are constantly subject to sea breezes. In most cases, the below-canopy measurement approach can be considered more accurate than those obtained by fog collectors. CWI is on average responsible for 42% of effective precipitation (n:41). The values listed show a large variation, between 0.5% and 462%, probably due to the different environmental characteristics of the sampled locations as well as variations in sample sizes.UFPRCoordenação de Aperfeiçoamento de Pessoal de Nível SuperiorLange, Daniel RibeiroSantos, Irani dos2023-12-23info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufpr.br/raega/article/view/9353010.5380/raega.v58i0.93530RA'E GA Journal - The Geographic Space in Analysis; v. 58 (2023); 63-92RAEGA - O Espaço Geográfico em Análise; v. 58 (2023); 63-922177-27381516-413610.5380/raega.v58i0reponame:Ra'e Ga (Online)instname:Universidade Federal do Paraná (UFPR)instacron:UFPRenghttps://revistas.ufpr.br/raega/article/view/93530/51123https://revistas.ufpr.br/raega/article/downloadSuppFile/93530/60475https://revistas.ufpr.br/raega/article/downloadSuppFile/93530/60765https://revistas.ufpr.br/raega/article/downloadSuppFile/93530/60766Direitos autorais 2023 RAEGA - O Espaço Geográfico em Análiseinfo:eu-repo/semantics/openAccess2023-12-29T18:43:40Zoai:revistas.ufpr.br:article/93530Revistahttps://revistas.ufpr.br/raegaPUBhttps://revistas.ufpr.br/raega/oai||raega@ufpr.br2177-27382177-2738opendoar:2023-12-29T18:43:40Ra'e Ga (Online) - Universidade Federal do Paraná (UFPR)false |
dc.title.none.fl_str_mv |
THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION |
title |
THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION |
spellingShingle |
THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION Lange, Daniel Ribeiro Physical Geography, Hidrology, Mountain Hydrology Hydrological monitoring, Tropical Cloud Forests, Stemflow. |
title_short |
THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION |
title_full |
THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION |
title_fullStr |
THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION |
title_full_unstemmed |
THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION |
title_sort |
THEORETICAL AND METHODOLOGICAL ASPECTS OF CLOUD WATER INTERCEPTION |
author |
Lange, Daniel Ribeiro |
author_facet |
Lange, Daniel Ribeiro Santos, Irani dos |
author_role |
author |
author2 |
Santos, Irani dos |
author2_role |
author |
dc.contributor.none.fl_str_mv |
Coordenação de Aperfeiçoamento de Pessoal de Nível Superior |
dc.contributor.author.fl_str_mv |
Lange, Daniel Ribeiro Santos, Irani dos |
dc.subject.por.fl_str_mv |
Physical Geography, Hidrology, Mountain Hydrology Hydrological monitoring, Tropical Cloud Forests, Stemflow. |
topic |
Physical Geography, Hidrology, Mountain Hydrology Hydrological monitoring, Tropical Cloud Forests, Stemflow. |
description |
Cloud water interception (CWI) occurs when water contained in fog and wind-driven rain collides with vegetation, merges into larger droplets, and precipitates to the ground. CWI has an important function as an additional source of water and its relationships with tropical cloud forests have often been emphasized. Despite its importance, there is no standardization of measurement methods, nor of the terms that designate the process in Portuguese. Therefore, a systematic analysis of research on CWI is necessary. To this end, the present study carried out a review of the theoretical and methodological aspects of CWI through description and analysis of terminology; history and chronology of studies on the topic; survey of the environmental conditions necessary for the CWI process to occur; analysis of methodological aspects relating to the measurement of CWI; and synthesis and discussion of magnitudes described in scientific literature. As a result, of the 31 publications reviewed, 14 different words were found, the most common being “Cloud Water Interception” (19.4%) and “Fog Drip” (16.1%). In general, CWI is more common in places such as continental edges and islands that are constantly subject to sea breezes. In most cases, the below-canopy measurement approach can be considered more accurate than those obtained by fog collectors. CWI is on average responsible for 42% of effective precipitation (n:41). The values listed show a large variation, between 0.5% and 462%, probably due to the different environmental characteristics of the sampled locations as well as variations in sample sizes. |
publishDate |
2023 |
dc.date.none.fl_str_mv |
2023-12-23 |
dc.type.none.fl_str_mv |
|
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://revistas.ufpr.br/raega/article/view/93530 10.5380/raega.v58i0.93530 |
url |
https://revistas.ufpr.br/raega/article/view/93530 |
identifier_str_mv |
10.5380/raega.v58i0.93530 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
https://revistas.ufpr.br/raega/article/view/93530/51123 https://revistas.ufpr.br/raega/article/downloadSuppFile/93530/60475 https://revistas.ufpr.br/raega/article/downloadSuppFile/93530/60765 https://revistas.ufpr.br/raega/article/downloadSuppFile/93530/60766 |
dc.rights.driver.fl_str_mv |
Direitos autorais 2023 RAEGA - O Espaço Geográfico em Análise info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Direitos autorais 2023 RAEGA - O Espaço Geográfico em Análise |
eu_rights_str_mv |
openAccess |
dc.format.none.fl_str_mv |
application/pdf |
dc.publisher.none.fl_str_mv |
UFPR |
publisher.none.fl_str_mv |
UFPR |
dc.source.none.fl_str_mv |
RA'E GA Journal - The Geographic Space in Analysis; v. 58 (2023); 63-92 RAEGA - O Espaço Geográfico em Análise; v. 58 (2023); 63-92 2177-2738 1516-4136 10.5380/raega.v58i0 reponame:Ra'e Ga (Online) instname:Universidade Federal do Paraná (UFPR) instacron:UFPR |
instname_str |
Universidade Federal do Paraná (UFPR) |
instacron_str |
UFPR |
institution |
UFPR |
reponame_str |
Ra'e Ga (Online) |
collection |
Ra'e Ga (Online) |
repository.name.fl_str_mv |
Ra'e Ga (Online) - Universidade Federal do Paraná (UFPR) |
repository.mail.fl_str_mv |
||raega@ufpr.br |
_version_ |
1799712043532550144 |