@InProceedings{DouglasMejiKill:2006:DeClCl,
author = "Douglas, Michael W. and Mejia, John F. and Killeen, Timothy J.",
affiliation = "National Severe Storms Laboratory/NOAA, Norman, Oklahoma USA
(Douglas) and CIMMS/University of Oklahoma, Norman, Oklahoma, USA
(Mejia) and Center for Applied Biodiversity Science at
Conservation International, 1919 M Street NW, Washingtion DC 20036
USA (Killeen) and {}",
title = "Developing cloudiness climatologies from satellite imagery to map
cloud forests and other vegetation features over the tropical
Americas",
booktitle = "Proceedings...",
year = "2006",
editor = "Vera, Carolina and Nobre, Carlos",
pages = "1015--1020",
organization = "International Conference on Southern Hemisphere Meteorology and
Oceanography, 8. (ICSHMO).",
publisher = "American Meteorological Society (AMS)",
address = "45 Beacon Hill Road, Boston, MA, USA",
keywords = "cloud forests, MODIS, GOES, cloudiness, vegetation.",
abstract = "Cloud forests along the eastern slopes of the tropical Andes are
associated with high cloudiness and high annual precipitation.
These regions possess very high biodiversity and as such are a
conservation priority. Detailed mapping of the cloud forests and
adjacent environments is essential for aiding conservation
strategies. Mapping is also important for studies that model
biodiversity, for interpreting both past and future climatic
scenarios, and for modeling the impact of climate change on the
vegetation distribution and associated biodiversity.
Unfortunately, mapping cloud forests is difficult. In general,
rainfall data is quite limited in the cloud forest environment,
since the eastern Andean slopes are sparsely populated and
relatively few roads cross the zone. Precipitation analyses
produced from the unevenly distributed station data do not reveal
the detailed geography of the cloud forest vegetation. Our study
has involved generating cloud climatologies from GOES and MODIS
imagery to help determine potential cloud forest environments.
MODIS imagery at 250m spatial scale provides a very high
resolution look at the distribution of cloudiness and its
relationship with topography, while GOES imagery at 1km and 4 km
(IR) scale help to define the diurnal cycle of cloudiness. In
addition to mean cloudiness patterns, we will also show the
seasonal evolution of the cloudiness and some stratifications of
cloudiness based on synoptic flow orientation. Limitations of our
procedures in identifying cloud forests will also be discussed.
Finally, some examples will be shown of the applicability of our
techniques to other regions in the tropical Americas.",
conference-location = "Foz do Igua{\c{c}}u",
conference-year = "24-28 Apr. 2006",
language = "en",
organisation = "American Meteorological Society (AMS)",
ibi = "cptec.inpe.br/adm_conf/2005/11.01.01.06",
url = "http://urlib.net/ibi/cptec.inpe.br/adm_conf/2005/11.01.01.06",
targetfile = "1015-1020.pdf",
type = "Monsoon systems and continental rainfall",
urlaccessdate = "12 maio 2024"
}