C LIM A GRO
UNDERSTANDING THE ANTHROPOGENIC AND NATURAL DRIVERS OF WATER BALANCE IN CHANGING ALPINE
GRASSLANDS USING A NETWORK OF SMALL - SCALE LYSIMETERS
Georg Frenck, Klaus Obojes, Georg Leitinger, Ulrike Tappeiner & Erich Tasser
TERENO conference 29/10‐ 02/10.14 Bonn
S ETTING THE S CENE
3
T
HE HYDROLOGICAL CYCLE OF THEA
LPS
AND ITS ROLE INE
UROPE FRESHWATER SUPPLYsources:
Roder, 2009
Weingartner et al . 2007
T
HE HYDROLOGICAL CYCLE OF THEA
LPS
AND ITS VULNERABILITY TO CLIMATIC CHANGEmeteorology climate topography water use biosphere
hydrological cycle
water availability
climate warming changes in:
precipitation regimes, snow cover, glacier storage
land-use changes
5
C
LIMATEC
HANGE IN THEA
LPS
TEMPERATUREC
LIMATEC
HANGE IN THEA
LPS P
RECEPITATIONs
s
a
w
7
CLIMAGRO
T
HEL
YSIMETERA
PPROACH E
COSYSTEMW
ATERB
ALANCEprecipitation
evapotranspiration
9
T
HEL
YSIMETERA
PPROACH S
MALL-S
CALEL
YSIMETERSC
LIMA
GRO I
NSTALLATION11
C
LIMA
GRO L
OWERB
OUNDARYC
ONTROLreference lysimeter
C
LIMA
GRO E
XPERIMENTALD
ESIGNscale1:100
1/1M 2/1S
3/1I
4/1I
5/1S 6/1M
1/2S 2/2I
3/2M
4/2S
5/2I 6/2M FB1
FB2
FB5 FB3
FB4 Log1
Log2
Log3
Log4 6/3S
1/4M
1/3S 2/3M
3/3L
4/3M
5/3S
6/4S 2/4S
3/4M
4/4M
5/4I T3/3
T3/4 mc1
mc2 mc3
mc4 mc5
mc6
mc7
mc8 mc9
6 7
1 2 3 4 5
8 9
Control (shelter, percipitation) Stubai vegetation – in situ Biological manipulations
Environmental manipulations
13
2 0 2 4 km
N
3 0 3 6 km
N
Matsch Valley
dry inner alpine climate;
precipitation = 526.7 mm mean temperature = 6.6°C
Stubai Valley
northern Central-European climate precipitation = 1097 mm
mean temperature = 6.3°C
C
LIMA
GRO I
NTEGRATINGP
LANT ANDE
COSYSTEMF
UNCTIONINGPLANT
height allocation hydraulics growth
LEAF
area mass conductance
SLA [N]
life-span LDMC thickness phenology
ROOT
depth mass
CANOPY
structure: (size, denisty, diversity)
CWM & FD of height, leaf mass & area
gas exchange canopy conductance
energy balance
EVAPOTRANSPIRATION
PRODUCTIVITY
DROUGHT RESISTANCE
plant functional traits effect and response functions
15