2. El Nexo Agua-Energia-Desarollo:
riesgos naturales y interacciones entre
infraestrutura, clima y paisaje en
un marco de adaptación
a multiples escalas
Ana P. Barros
Duke University
Lima, March 22, 2013
3. Pilares de Adaptación
Observaciones - Rigorosas, Consistentes, Dense, Extensas
Analísis y Interpretación – Representación y modelos
Descoberta
Ciencia
Integración de datos e física >>> Contexto de riesgo
Evaluar Vulnerabilidades , “Breaking Points”
4. Ciclos Climáticos…
Dos series con Nilometer 622-1284 A.D.
media y variancia H=0.91
estadísticas iguales
The idea that
persistent
(0.5<H<1.0)
H=0.5 “Ruído Blanco”
movements in a
time series tend to
be part of larger
trends and cycles
more often than they
are completely
random.
From Koutsoyannis, 2004
(Mandelbrot and Wallis 1977, Hurst 1951, Barros and Evans 1996)
5. Renaissance
Y de un punto de vista regional,
local que significa? Revolución
Industrial
6. Analísis de Riesgo – Infraestrutura
Presa
Construída
?
Note la influencia de la duración del periodo de observación
7. Green, Renewable Energy
“Gran Muralla Andina”
India: Plans to build 292 hydroelectric dams in the
Himalayas
Environmental Services
Conectividad Hidrologica
Conectividad Ecologica
Material (Sedimentos, Nutrientes)
Sustainability /Climate
Finer and Jenkins, 2012
8. Endicamientos Naturales : Formación y Falla
Penna e al. 2012) HidroAgoyan Dam,
Pastaza River, Ecuador
9. Changing Mix of Stations: Raingauge Stations Over Time
(NOAA GHCN Dataset)
New et al. 2001
Courtesy David Easterling, NOAA- NCDC
10. GHCN-Monthly Version 3.0
• The dataset for global climate monitoring and assessment
– 7280 mean temperature stations; >20,000 precipitation stations
– Global coverage from 1880 to present
– GHCN-M Version 3 released in 2010 (temperature only)
Courtesy David Easterling, NOAA- NCDC
12. Estaciones hydrométricas
b)
1 – Africa
2 – Asia
3 – South America
4 – North America,
Central America,
and the Caribbean
5 – Europe
Elevation H [m]
6 – South-West Pacific
WMO Region
Barros 2012
13. Hydrometeorology of Mountainous Regions
Maritime vs Continental Tropical Monsoon Regimes
Mid-Latitude Seasonal Regimes
Global to Regional Scale Controls
Summit to Sea and Sea To Summit
14. From Clouds to River Networks
1st Principal Component of Cloudiness (IR Brightness)
Giovannetone and Barros 2008 and 2009
15. Warm Rain
Daytime
“Deep”
TRMM Central Andes
Convection
Giovannettone and Barros, 2009
Figure 19 – Global distribution of streamgauges: a) as a function of elevation; b) for each elevation as a function of WMO (World Meteorological Organization) regions. [Source: http://www.bafg.de/GRDC/EN]