Jultime 2005 vs watertemp -1m Jultime 2005 vs soiltemp-50cm Jultime 2005 vs soiltemp-10cm Jultime 2005 vs airtemp+10cm
3
No data
0.1
Water level change (cm)
0.01 40 35 30 25 20 15 10 240
245
250
255
260
265
270
275
280
285
290
295
300
305
310
Day of Year 2005
Source: Horna, Zimmerman, Kuppers 2006
4 100
Rain (mm/h)
10
Puddles Filling
1
1
Jultime 2005 vs watertemp -1m Jultime 2005 vs soiltemp-50cm Jultime 2005 vs soiltemp-10cm Jultime 2005 vs airtemp+10cm
No data
0.1
Water level change (cm)
0.01 40 35 30 25 20 15 10 240
245
250
255
260
265
270
275
280
285
290
295
300
305
310
Day of Year 2005
Source: Horna, Zimmerman, Kuppers 2006
Runoff
- Gradient towards basins - Increased Storage in basins ET
Subsurface Flow
Impermeable layer
- No change in center
45
Jultime 2005 vs watertemp -1m Jultime 2005 vs soiltemp-50cm Jultime 2005 vs soiltemp-10cm Jultime 2005 vs airtemp+10cm
Puddles forming
2
No data
250
255
260
265
270
275
280
285
290
295
300
305
310
Day of Year 2005
Source: Horna, Zimmerman, Kuppers 2006
- Puddles independent
ET
- Local ET rates
Runoff
- Decrease in Center - Large Decrease in Storage Subsurface Flow Impermeable layer
45
Jultime 2005 vs watertemp -1m Jultime 2005 vs soiltemp-50cm Jultime 2005 vs soiltemp-10cm Jultime 2005 vs airtemp+10cm
Puddles forming
2
No data
250
255
260
265
270
275
280
285
290
295
300
305
310
Day of Year 2005
Source: Horna, Zimmerman, Kuppers 2006
- Puddles independent
ET
- Local ET rates
Runoff
- Decrease in Center - Large Decrease in Storage Subsurface Flow Impermeable layer
45
Jultime 2005 vs watertemp -1m Jultime 2005 vs soiltemp-50cm Jultime 2005 vs soiltemp-10cm Jultime 2005 vs airtemp+10cm
Puddles forming
2
No data
250
255
260
265
270
275
280
285
290
295
300
305
310
Day of Year 2005
Source: Horna, Zimmerman, Kuppers 2006
- Puddles independent
ET
- Local ET rates
Runoff
- Decrease in Center - Large Decrease in Storage Subsurface Flow Impermeable layer
60
Jultime 2005 vs watertemp -1m Jultime 2005 vs soiltemp-50cm Jultime 2005 vs soiltemp-10cm Jultime 2005 vs airtemp+10cm
Pooling
3
No data
265
270
275
280
285
290
295
300
305
310
Day of Year 2005
Source: Horna, Zimmerman, Kuppers 2006
Runoff
- Maximum Storage ET + outflow
- Basins act as single unit - Pulses in center
Subsurface Flow
Impermeable layer
4 100
Rain (mm/h)
10
1
1
2
Jultime 2005 vs watertemp -1m Jultime 2005 vs soiltemp-50cm Jultime 2005 vs soiltemp-10cm Jultime 2005 vs airtemp+10cm
3
No data
0.1
Water level change (cm)
0.01 40 35 30 25 20 15 10 240
245
250
255
260
265
270
275
280
285
290
295
300
305
310
Day of Year 2005
Source: Horna, Zimmerman, Kuppers 2006
Puddle-Pool Dynamics
Runoff
Subsurface Flow
Impermeable layer
-
Uplands are critical
-
Control on Vegetation
Summary - Important aspect of landscape - Conglomeration of multiple meander scars - Puddle-pool dynamics - Dependence on terrace and upland forests
Acknowledgements John Janovec Mathias Tobler Viviana Horna Reiner Zimmerman Dario Cruz Javier Huinga Moore Foundation ACA/ACCA More Info: www.andesamazon.org Coming soon: