IANIGLA   20881
INSTITUTO ARGENTINO DE NIVOLOGIA, GLACIOLOGIA Y CIENCIAS AMBIENTALES
Unidad Ejecutora - UE
congresos y reuniones científicas
Título:
New evidence of surge-type glaciers in the Central Andes of Argentina and Chile
Autor/es:
MARIA GABRIELA LENZANO; DANIEL FALASCHI; TAKEO TADONO; TOBIAS BOLCH; LUIS LENZANO
Lugar:
New Orleans
Reunión:
Encuentro; AGU Fall Meeting; 2017
Institución organizadora:
American Geophysical Union
Resumen:
In contrast to the large surge-type glacier clusters widely known for several mountain ranges around the world, the presence of surging glaciers in the Andes has been historically seen as marginal. Based on the analysis of satellite imagery and DEM differencing, coupled with aerial archival data, we identified 21 surge-type glaciers in the Central Andes, out of which four of them are confirmed surge-type, six are very-probable surge-type, and eleven are possible surge-type. The geodetic mass balance estimation of 12 glaciers for the 2000-2011 period, which encompasses the latest surge events, mostly showed either moderately negative or positive patterns (-0.5 to 0.3 m w.e. a-1). Additionally, we calculated maximum surface velocities of ~6.3 ±1.9 m d-1 and ~3.5 ±1.2 m d-1 for the Piuquenes and Noreste del Cerro Alto glaciers during the latest two identifiable surge events (1985-1987 and 2003-2007), and preliminarily determined surge cycles of ~10 and ~20 years for these two glaciers, respectively. The synchronicity of recent and past glacier surges and the coincidence with anomalously cold, snowy periods point out to a common climatic control over glacier surges in this region.