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Last modified
11/23/2009 10:50:35 AM
Creation date
10/4/2006 9:03:23 PM
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Title
Changes in the Hydrological Response of a Small Mediterranean Basin a Year After a Wildfire
Date
6/8/1992
Prepared For
Journal of Hydrology
Prepared By
Elsevier Science Publishers
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />276 <br /> <br />1. LAVABRE ET AL. <br /> <br />HYDROLOGICAL RESPONSE OF ^ MEDITERRANEAN BASIN <br /> <br />277 <br /> <br /> <br />120.0 <br /> <br />117.5 <br /> <br />~/"""__, I' <br />,- ,/ ~--- )', <br />.... '- I.... \.. ! I <br />....l..... ... / ,,;/ / <br />". ',- l ) ~ \ 't '" <br />.....___....___--1 , \ ... '.).-' \ <br />1-- , \ '. \ '__, '. J <br />I 1__ I ... \ ....-;, IC\........ <br />...~;::j--.---..-_.~.... __I -'....\ ...~-..., ',"'- " /~ <br />__....,f 'y-..._...-.... \~, ....~~- "I / <br />:; ,/" - - - \ I i-.~:)-.......... ...., s.,' <br />";~_' I ,...J~/~-I--)~,,_I .....' <br />._~_.._......_._.~/". ___. _"...--;r,:---- '. A_ A 17 <br />..- \. '.....- _. . "- ....... <br />-, (..." I, -'''''_, \ " \, <br />" /) \,\ 1 ~.......\\~'- <br />-----< J 1 \ \ /""-.1' . .. <br />....-.:.., \ I <br />\ \ ' <br />\ \--.... <br />... ....- / <br />" - <br />RIMBAUD BASIN <br /> <br />115.0 <br /> <br />112.5 <br /> <br />110.0 <br /> <br />107.5 <br /> <br />105.0 <br /> <br />910.0 <br /> <br />912.5 <br /> <br />915.0 <br /> <br />917.5 <br /> <br />920.0 <br /> <br />922.5 <br /> <br />925.0 <br /> <br />927.0 <br /> <br />930.0 <br /> <br />Fig. I (continued). <br /> <br />Km (Lambert III) <br /> <br />Fig. I. Location of the Real Collobrier experimental research basin and of the Rimbaud and Vaubarnier <br />sub-basins. <br /> <br />TABLE I <br /> <br />Summary of the main characteristics of the Rimbaud basin before the fire (1967-1989) <br /> <br />recorded during August. Thus the 1990 hydrological year can be considered <br />to be totally post-fire. <br />The data were continuously recorded during this period and only the flows <br />from 5 to 25 October were missed. In the study, the monthly total flow of <br />October was reconstituted using the next flow recorder station located in the <br />Rimbaud stream. For the precipitation data we used the values measured by <br />the pluviograph located inside the basin. Complementary data from the Real <br />Collobrier meterological station nearby were also used. <br /> <br />Surface area <br />Distance to the sea <br />Elevation range <br />Vegetation <br /> <br />l40ha <br />ISkm <br />470-670 m <br />Totally forested by maquis and degraded forest of cork <br />trees and chestnuts <br />Slightly altered gneiss <br />II64mm <br />201s-1 <br />13.7mls-1 <br />6m)s-1 <br />Marginal <br /> <br />Geology <br />Annual mean precipitation <br />Mean discharge <br />Maximal discharge <br />10 year return period f1.ow <br />Human influence <br /> <br />
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