User:Brardino: Difference between revisions
From CSDMS
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|Website member=http://www.geo.unimib.it/staff/dipartimento.html?sobi2Task=sobi2Details&catid=13&sobi2Id=6 | |Website member=http://www.geo.unimib.it/staff/dipartimento.html?sobi2Task=sobi2Details&catid=13&sobi2Id=6 | ||
|Working group member=Terrestrial Working Group | |Working group member=Terrestrial Working Group | ||
|Emaillist group member=yes | |||
|Description of your CSDMS-related interests member=So far I have taken an empirical (field-based) approach to geomorphology. This approach has clear spatial and temporal limitations. I'd hope to see field data (perhaps coming from different regions) contributing to the development/fine tuning of landscape evolution/sediment flux models to examine how site-specific data will scale up at regional spatial scales and possibly at longer (> 100 yrs)time scales. | |Description of your CSDMS-related interests member=So far I have taken an empirical (field-based) approach to geomorphology. This approach has clear spatial and temporal limitations. I'd hope to see field data (perhaps coming from different regions) contributing to the development/fine tuning of landscape evolution/sediment flux models to examine how site-specific data will scale up at regional spatial scales and possibly at longer (> 100 yrs)time scales. | ||
|How did you learn about CSDMS member=through geomorph-list announcement | |How did you learn about CSDMS member=through geomorph-list announcement | ||
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Revision as of 11:33, 2 August 2013
Francesco Brardinoni, website username login: Brardino
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Member of the following CSDMS groups
- Terrestrial Working Group
Signed up for the mailing list: yes
So far I have taken an empirical (field-based) approach to geomorphology. This approach has clear spatial and temporal limitations. I'd hope to see field data (perhaps coming from different regions) contributing to the development/fine tuning of landscape evolution/sediment flux models to examine how site-specific data will scale up at regional spatial scales and possibly at longer (> 100 yrs)time scales.
