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TALLER DE GESTION INTEGRADA DE RECURSOS HÍDRICOS
QUITO19 Junio 2006
Vicente Barros
LAS PREVISIONES PARA LA GESTILAS PREVISIONES PARA LA GESTIÓÓN DE LOS RECURSOS N DE LOS RECURSOS HHÍÍDRICOS EN RELACIDRICOS EN RELACIÓÓN CON N CON
LA VARIABILIDAD Y EL CAMBIO CLIMLA VARIABILIDAD Y EL CAMBIO CLIMÁÁTICO TICO EN LA CUENCA DEL PLATAEN LA CUENCA DEL PLATA
PROGRAMA MARCO PARA LA GESTION PROGRAMA MARCO PARA LA GESTION SOSTENIBLE DE LOS RECURSOS HIDRICODS SOSTENIBLE DE LOS RECURSOS HIDRICODS
DE LA CUENCA DEL PLATA EN RELACION DE LA CUENCA DEL PLATA EN RELACION CON LOS EFECTOS HIDROLOGICOS DE LA CON LOS EFECTOS HIDROLOGICOS DE LA VARIABILIDAD Y EL CAMBIO CLIMATICOVARIABILIDAD Y EL CAMBIO CLIMATICO
ComitComitéé Intergubernamental de la Cuenca del PlataIntergubernamental de la Cuenca del Plata
WHY WHY INTEGRATE CLIMATE CHANGEINTEGRATE CLIMATE CHANGE
IN THE PLATA BASIN PROGRAME?IN THE PLATA BASIN PROGRAME?
12
3
4
5
6
1: Chaco
2: Pantanal
3: Middle Paraguay
4: Upper Paraná
5: Middle Paraná
6: Upper Uruguay
Changes in river dischargesChanges in river dischargesRío de la Plata basin
Paraná River - Corrientes
annu
al d
isch
arge
(m3 /s
)
0
5000
10000
15000
20000
25000
30000
35000
40000
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000
Uruguay River- Paso de los Libres
annu
al d
isch
arge
(m3 /s
)
0
2000
4000
6000
8000
10000
12000
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000
Salado River - RP 70
annu
al d
isch
arge
(m3 /s
)
0
100
200
300
400
500
600
700
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000
Paraguay River - Puerto Bermejo
annu
al d
isch
arge
(m3 /s
)
0
2000
4000
6000
8000
10000
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000
•• Are the river flow changes Are the river flow changes resulting from precipitation resulting from precipitation changes or from the land use changes or from the land use change?change?
Land surface effects
Land cover / Land use
¿ How much of the changeshould be attributed
to precipitation changeand how much to land use change?
Precipitation en the Plata basin (m3 s-1)
Streamflow(m3 s-1)
Evaporation +Infiltration (m3 s-1)
1998 107000 36600 70400
1999 81600 20440 61600
Difference 23 % 44 % 13 %
El Niño 76000 25250 50750
La Niña 71000 21640 49360
Difference 7 % 17 % 3 %
1951-1970 72000 19300 52700
1980-1999 83500 26000 56500
Difference 16 % 35 % 9 %
AMPLIFICATION OF THE PRECIPITATION VARIABILITY IN THE RIVER FLOWS
PRECIPITATION CHANGES
Annual precipitation trends 1900-2000
IPCC (2001)
SE South America: 23%Chile: 40%
pm
m
600
800
1000
1200
1400
1600
1800
2000
2200
2400
1940 1950 1960 1970 1980 1990 2000
Monte Caseros: Annual Precipitation
Annual rainfall trends (mm/year): 1960-2000
The region hasincrements in the annual rainfallbetween 10% and 40%.
The increments in some regions of the Plata basinwere 200 m or more in 40 years.
IMPACTS-70 -65 -60 -55 -50 -45 -40-40
-35
-30
-25
-20
-15
Isohyets in Isohyets in mmmm
black : black : 19501950--19691969
Red:Red:19801980--19991999
Extreme events
Number of cases with Precipitation> 100 mm/(2 days) for 16 gauging stations over
central and northeastern Argentina
0
5
10
15
20
25
30
35
40
59/ 62 63/ 66 67/ 70 71/ 74 75/ 78 79/ 82 83/ 86 87/ 90 91/ 94 95/ 98 99/ 02
AÑOS
Precipitation over 150 mm: rate between the annual frequency of the 1983/2002 and the 1959/1978 periods
Impacts in the HydrologyImpacts in the Hydrology
Annual maximum, mean and minimum daily discharge of the Paraná river at Santa Fe-Paraná
period 1902-2000
0
10000
20000
30000
40000
50000
60000
Cau
dal (
m3/
s)
1910 1940 1970 2000
1997/98 Flood of the Paraná River(Satellite images from CONAE)Normal conditions
TEMPERATURE
Global annual temperature trends: 1976-2000
IPCC (2001)
CLIMATE CHANGE CLIMATE CHANGE SCENARIOSSCENARIOS
Average of various models: Mean annual temperature difference 2071/ 2100 minus 1961/ 1990 (colors),range (blue lines) (in °C). (IPCC, 2001)
-80 -75 -70 -65 -60 -55 -50 -45-60
-55
-50
-45
-40
-35
-30
-25
-20
-80 -75 -70 -65 -60 -55 -50 -45-60
-55
-50
-45
-40
-35
-30
-25
-20
-80 -75 -70 -65 -60 -55 -50 -45-60
-55
-50
-45
-40
-35
-30
-25
-20
HADCM3 model HADCM3 model Scenario A2 :Scenario A2 :Difference of Difference of temperature (temperature (°°K) K) with present with present (1961(1961--90)90)
2020/2030 2050/2060
2070/2080
In the La Plata Basin, temperatures will be higher and rainfall will tend to be above normal or not as projected by all IPCC models, especially for the time slices between 2050 and 2080. Courtesy of Marengo
PrecipitationTemperature
LPB temperature and precipitation scenarios for 2050-2080
Hydrologic modeling
Discharge Scenarios: Plata Basin
-5112,627-2120,31126,012Total
-472,836-194,2935,329UpperUruguay
-564,541-237,99310,435MiddleParaná
-364,230-155,6526,614UpperParaná
-72691-341,5122,435Paraguay
-73329-377601,202Pantanal
+ 5° CPercent change
+ 5° CEstimated
m3/s
+ 2° CPercent change
+ 2° CEstimated
m3/sPresent
dischargem3/s
IN THE PLATA BASIN75 % OF PRECIPITATION EVAPORATES
ONLY 25 % REACH the RIVERS
RELATIVELY MODEST CHANGES IN PRECIPITATION OR IN EVAPORATION MAY LEAD
TO GREAT PERCENT CHANGES IN THE RUNOFF
IN THE CONTEXT OF CLIMATE CHANGE THIS MEANS THAT THE
HIDROPOWER (BRASIL 90 %)NAVEGATIONWATER SUPPYARE HIGHLY VULNERABLE
Hay Cambio Climatico?THE BEST GLOBAL CLIMATE MODELS DO NOT
REPRODUCE THE MAIN FEATURES OF
PRECIPITATION AND TEMPERATURE OVER THE
PLATA BASIN
Verification of rainfall fields
-65 -60 -55 -50 -45
-45
-40
-35
-30
-25
-20
-15
-10PP HADCM3-UDEL - ANNUAL (1961-1999) (mm/dy)
Difference between observed annual precipitation and
simulated by the HADCM3 model (mm/day)
~ 35 % lower than observed
PART OF THE PROJECTED CLIMATE CHANGE IS PART OF THE PROJECTED CLIMATE CHANGE IS UNAVOIDABLEUNAVOIDABLE
IT IS ALREADY TAKEN PLACEIT IS ALREADY TAKEN PLACE
REGIONAL CLIMATE PROJECTIONS HAVE LARGEREGIONAL CLIMATE PROJECTIONS HAVE LARGEUNCERTAINTIESUNCERTAINTIES
SOCIETY NEEDS BETTER PROJECTIONS TO START SOCIETY NEEDS BETTER PROJECTIONS TO START ADAPTATIONADAPTATION
GOVERMENTS NEED BETTER PROJECTIONS TO ASSESS GOVERMENTS NEED BETTER PROJECTIONS TO ASSESS THEIR NATIONAL INTERESTSTHEIR NATIONAL INTERESTS
Land surface effects
Land surface effects
Climate changescenarios
Climate changescenarios
Extreme eventsExtreme events
Hydro-climatePrediction
Hydro-climatePrediction
La Plata Basin Priority areas
Variability and trends
Variability and trends
Planned activities
• Climate change scenarios, vulnerability and adaptation
. Land use change
. Improvement of the diagnostic and prediction system (weather and climate)
• Improvement of the diagnostic and prediction system (hydrology)
• Enhanced monitoring
• Field experiment
Thank you!...