INVESTIGADORES
MOREIRAS Stella Maris
congresos y reuniones científicas
Título:
Climatic role in landslide occurrence in the Central Andes, Argentina
Autor/es:
MOREIRAS S.M.
Lugar:
Mendoza
Reunión:
Simposio; Symposium on Climate Change: Organizing the Science in the American Cordillera; 2006
Institución organizadora:
IAI (Inter American Institute for Global Climatic Change) - IANIGLA
Resumen:
Identification of landslides triggering mechanisms is a key for the prediction of
these natural hazardous events. Although landslides are triggered by several
causes; summer rainstorm is one of a major factor in their distribution and
frequency in this arid region (200 mm mean annual precipitation). More than 200
historical rockfall and debris flows happened during the 1902-2002 period could be
correlated with rainfall. The precipitation threshold value established from daily
meteorological records was 6.5-12.9 mm, even though the net of meteorological
stations is not dense enough in the region. What is more, the antecedent
precipitation is important to be taken into account as 60% of these events showed
previous rainfall. Total amount of rainfall increases notably and the mean value
increases by 56% if antecedent rainfall is considered.
Furthermore, climatic phenomena are forcing landslide occurrence in the Central
Andes. Given that the ENSO warm episodes (El Niño) (Díaz and Kiladis, 1992) are
characterised by major precipitation events; greater number of landslides has been
recorded during these periods in Cordillera Frontal; whereas a decreasing number
happened during cold episodes (La Niña). However, the slope instability in the
Precordillera, located east of the Cordillera Frontal, seems to be mainly influenced
by wet-cold periods linked to the Atlantic Anticyclone behaviour (Compagnucci et
al. (2002). A higher number of landslides were recorded in years linked to wet
periods than during dry periods. Moreover, the analysis of variance shows that
there is no significant difference between landslide records and cold-warm
episodes.
The mean interval of landslide recurrence is 4 and 15 years in Cordillera Frontal and
Precordillera, respectively (Moreiras, 2006). However, we suspect that this
frequency may be higher in the future as climate models suggest an increase in
both precipitation and temperature in the region. In addition, El Niño climatic
phenomenon may be more frequent and severe in the future as a consequence of
global climatic change. Likewise, the end of the present wet period starting in 1972
is yet unknown. Hence the importance of considering the climatic role in temporal
distribution of landslides related to hazard and risk scenarios.