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ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Seasonal variations of evapoTRANSPIRATION
Olivier Liechti, A&K
OSTIV Meteorological PanelAntalya, September 2011
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Surface energy flux
3 6 9 12 15 180
100
200
300
400
500
600
700
800
900
1000
[h]
[W/m2]
VIS
IR
GH
SH
LH
3 6 9 12 15 180
100
200
300
400
500
600
700
800
900
1000
[h]
[W/m2]
VIS
IR
GH
SH
LH
• CBL depth• glider flight level
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Seasonal variation
-10
-5
0
5
10
15
20
25
30
T (C)
2007 20082006 20092005
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Seasonal variation
-5
0
5
10
15
20
T(C)
J F M A M J J A S O N D
increased albedo
inactive vegetation
active vegetation
inactive vegetation
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Complex topography
1000 2000 3000
1000
2000
3000
1000 2000 3000
1000
2000
3000
1000 2000 3000
1000
2000
3000
Surface area [km2]
A
A
B
B
C
D D
1000 2000 3000
1000
2000
3000
[m M
SL]
[m M
SL]
[m M
SL]
C
River Adda
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Elevation dependence of seasonal temperature
-10 -5 0 5 10 15 200
400
800
1200
1600
2000
2400
2800
3200
3600
4000
T (C)
z (mMSL)
April, October July January
increased albedo minimum
transpiration transpiration maximum
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Seasonal variation in elevated terrain
-5
0
5
10
15
20
T(C)
J F M A M J J A S O N D
increased albedo
reduced transpiration
full transpiration
reduced transpiration
3200 mMSL
sea level
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Seasonal variation of transpiration in complex terrain
-5
0
5
10
15
20
T(�C)
J F M A M J J A S O N D
increased albedo
minimum transpiration
transpiration maximum
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
CBL predictions for the Rhone valley in April
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
CBL predictions for the Rhone valley in August
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
CBL predictions for the Alps in April
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Glider flight in April
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
CBL predictions for the Alps in August
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Glider flight in August
ANALYSEN & KONZEPTE, 8404-WINTERTHUR
Summary
• seasonal variations of surface characteristics(transpiration, albedo) affect the depth of the convectiveboundary layer significantly
• glider flight data has been used for the development of seasonal parameterisations
• summertime convective mixing in deep valleys withelevation dependent transpiration tends to form twomixed layers