alpine scenario: la fouly susana fernandez vidal epfl - eflum
Post on 20-Dec-2015
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Alpine scenario:
La Fouly
Susana Fernandez VidalEPFL - EFLUM
Rationales and Goals of the monitoring1. Generation and acquisition of data which describes hazardous scenarios in the Swiss Alps
2. Studying and analyzing environmental processes that might trigger hazardous scenarios, such as floods, debris-flows and landslides
3. Assessing the impact of spatial variability related to meteorological and soil characteristics, on catchment hydrology
4. Characterizing the soil more in detail to improve soil moisture modeling
5. Hydrograph separation: snow and ice melt, rainfall-runoff, groundwater drainage
6. Improve hydrological modeling using a 3D-physically based model
7. Study of the slope winds
La Fouly Catchment area = 20 Km2
Zmin = 1785 m , Zmax = 3238 m
Gd ST-BernardItaly N
LAYOUT OF THE STATIONS 2010
16 SENSORSCOPE STATIONSMaster station
Master station
MAXBOTIX: Water levelhttp://sensorscope.epfl.ch/climaps/
EACH STATION MEASURES:
• ACCUMULATED RAIN• WIND SPEED & WIND DIRECTION• INCOMING SHORTWAVE RADIATION• SKIN TEMPERATURE• AIR TEMPERATURE• RELATIVE HUMIDITY• SOIL MOISTURE • SOIL TEMPERATURE• SOIL SUCTION
Water level :• Pressure transducer• Maxbotix (ultrasound)
WATER LEVEL & DISCHARGE
Discharge measurements: •Salt dilution method (Sommer)
STAGE-DISCHARGE RELATION
~ 1 km
~ 10 m
Surface energy balance
Profiles of turbulent fluxes
Atmospheric profiles
Sensorscope stations
Slope Winds at La Fouly
ISOTOPE APPLICATIONS IN CATCHMENT HYDROLOGY
• To answer to questions like: - Where water goes when it rains? - What pathways it takes to the stream? - How long water resides in the catchment?
• Isotope information may be used to calibrate and test distributed rainfall-runoff models (GEOtop, ALpine3D)
STABLE ISOTOPE ANALYSER(CAVITY RING DOWN)FOR 18O/16O & 2H/1H
Some results of La Fouly 2009
Discharge components:Stream Hydrograph separation
Samples
-River-Snow melt-Snow/ice from the glacier-Streams-Springs-Rain-Soil
Catchment area = 20 Km2
Zmin = 1785 m , Zmax = 3238 m
Baseflow : The glacier
La Fouly – field campaign 2009Soil Data (18th June – 29th October)
-20 cm-40 cm-60 cm
-60 cm-20 cm
1036
20 cm
20 cm
20 cm
Slope Winds at La Fouly
Slope Winds at La Fouly
Dayslo
pe w
inds
valley winds
Night
Katabatic Winds Anabatic Winds