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ANALYSEN & KONZEPTE, 8404-WINTERTHUR Seasonal variations of evapoTRANSPIRATION Olivier Liechti, A&K OSTIV Meteorological Panel Antalya, September 2011

Seasonal variations of evapoTRANSPIRATION · evapoTRANSPIRATION Olivier Liechti, A&K OSTIV Meteorological Panel Antalya, September 2011. ANALYSEN & KONZEPTE, 8404-WINTERTHUR Surface

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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