Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Leila M.V. Carvalho"'
Autor:
Alan T. Murray, Jiwon Baik, Vanessa Echeverri Figueroa, Darlene Rini, Max A. Moritz, Dar A. Roberts, Stuart H. Sweeney, Leila M.V. Carvalho, Charles Jones
Publikováno v:
International Journal of Applied Earth Observations and Geoinformation, Vol 124, Iss , Pp 103531- (2023)
The wildland urban interface (WUI) is a transition zone between mostly undeveloped, vegetated lands and more densely populated areas with buildings and other infrastructure. This interface is of great interest and concern in wildfire prone areas like
Externí odkaz:
https://doaj.org/article/f34bda455ac147be873706f092ba8c07
Publikováno v:
Weather and Climate Extremes, Vol 37, Iss , Pp 100482- (2022)
This study investigates mesoscale mechanisms associated with two extreme heatwaves affecting Santa Barbara County (SBC), southern California, and their implication for severe fire weather. We examine these issues using a database consisting of surfac
Externí odkaz:
https://doaj.org/article/b68429d16ef04af2ba7f9fca16db0fdf
Autor:
Danlu Cai, Klaus Fraedrich, Yanning Guan, Shan Guo, Chunyan Zhang, Leila M.V. Carvalho, Xiuhua Zhu
Publikováno v:
Sensors, Vol 19, Iss 20, p 4499 (2019)
Essential for directing conservation resources is to identify threatened vertebrate regions and diagnose the underlying causalities. Through relating vertebrates and threatened vertebrates to the rainfall-runoff chain, to the food chain, and to the h
Externí odkaz:
https://doaj.org/article/308417c89b224751b61e0870734a31c6
Publikováno v:
Atmosphere, Vol 10, Iss 3, p 155 (2019)
This study investigates the influence of planetary boundary layer (PBL) schemes and land surface models (LSMs) on the performance of the Weather Research & Forecasting model in simulating the development of downslope windstorms in the lee of the Sant
Externí odkaz:
https://doaj.org/article/867a084a32d34a43a0d389e43ca19c05
Atmospheric rivers (ARs) reach High Mountain Asia (HMA) about 10 days per month during the winter and spring, resulting in about 20 mm day-1 of precipitation. However, a few events may exceed 100 mm day-1, providing most of the total winter precipita
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d86bf4efb3adc3f7bb1d3312c799aff0
https://doi.org/10.21203/rs.3.rs-2787173/v1
https://doi.org/10.21203/rs.3.rs-2787173/v1