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Bendix, J.; Rollenbeck, R.; G&ouml;ttlicher, D.; Nauss, T. &amp; Fabian, P. (2008): <b>Seasonality and diurnal pattern of very low clouds in a deeply incised valley of the eastern tropical Andes (South Ecuador) as observed by a costeffective WebCam system</b>. <i>Meteorological Applications</i> <b>15</b>(2), 281-291.

Resource Description
Title: Seasonality and diurnal pattern of very low clouds in a deeply incised valley of the eastern tropical Andes (South Ecuador) as observed by a costeffective WebCam system
FOR816dw ID: 97
Publication Date: 2008-06-01
License and Usage Rights: PAK 823-825 data user agreement. (www.tropicalmountainforest.org/dataagreementp3.do)
Resource Owner(s):
Individual: Jörg Bendix
Contact:
Individual: Rütger Rollenbeck
Contact:
Individual: Dietrich Göttlicher
Contact:
Individual: Thomas Nauss
Contact:
Individual: Peter Fabian
Contact:
Abstract:
To date, the annual and diurnal pattern of low clouds touching the ground in tropical mountains is widely unknown. This holds true for the valley of the Rio San Francisco in southern Ecuador, and is mainly due to a lack of routine cloud observations, which is symptomatic for remote areas in tropical high mountains. A method to use a simple and cost-effective WebCam system for a quantitative analysis of cloud frequency as a proxy for the occurrence of low-cloud bases touching the ground is introduced. An interactive classification tool is developed, which is applied to a comprehensive dataset of 32 452 images (during the years 2002–2004) archived at 5 min intervals. The results point to a rapid increase of cloud frequency at altitudes > 2600 m asl both during the day and the year, mainly caused by advective clouds veiling the crests of the Cordillera del Consuelo. Even if the formation of radiation fog directly at the valley bottom is nearly negligible with regard to the whole dataset, scatterometer measurements suggest that valley fog formation on the slopes is a regular process during the night, causing a clear drop in the cloud base around sunrise. The interaction of low-radiative and high-advective clouds is supposed to be the driving factor for a rainfall maximum at the valley bottom around sunrise. Higher values of cloud frequency still exist at the crest level around noon: these originate from well-developed upslope-breeze systems.
Keywords:
| Ecuador | Andes | WebCam | cloud frequency |
Literature type specific fields:
ARTICLE
Journal: Meteorological Applications
Volume: 15
Issue: 2
Page Range: 281-291
Metadata Provider:
Individual: Tiziana Li Koch
Contact:
Online Distribution:
Download File: http://www.lcrs.de/publications.do?citid=97


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