Indicators of present global warming through changes in active layer-thickness,estimation of thermal diffusivity and geomorphological observations in the Morenas Coloradas rockglacier, Central Andes of Mendoza, Argentina

D. TROMBOTTO; E. BORZOTTA

COLD REGIONS SCIENCE AND TECHNOLOGY

ELSEVIER SCIENCE BV

Año: 2009 vol. 55 p. 321 - 330

0165-232X

Temperature profiles from the active layer have been analysed for 2 sites on the composed rockglacier Morenas Coloradas, Cord¨®n del Plata, Mendoza, Argentina, using monitoring data collected between 1989 and 2008 in order to characterize the impact of global warming in the cryolithozone of the Dry Andes at these latitudes (32¡ã¨C33¡ã S). Asignificant change in the active layer and suprapermafrost of this rockglacier of the Cord¨®n del Plata is registered at themonitoring sites. The observed changes imply direct consequences for the cryogenic environment and the Andean creeping permafrost. The nose of the Morenas Coloradas rockglacier for example (Balc¨®n I, 3560 m a.s.l.), already expresses inactivity; the permafrost table is found at great depth (7.5¨C9 m). Data collected at Balc¨®n I and II allow to estimate the theoretical thermal diffusivity ¦Á at the active layer of Morenas Coloradas. Thermal diffusivitymay be decisive for the study of cryogenic dynamics at other altitudes and latitudes in the region where data are still scarce. Low ¦Á values (b0.2¡Á10− 6m2/s) correlate with occurrence of freezing and ice at low altitudes. While the glaciers are turning into small insignificant bodies in the high mountains, the periglacial level withfiles from the active layer have been analysed for 2 sites on the composed rockglacier Morenas Coloradas, Cord¨®n del Plata, Mendoza, Argentina, using monitoring data collected between 1989 and 2008 in order to characterize the impact of global warming in the cryolithozone of the Dry Andes at these latitudes (32¡ã¨C33¡ã S). Asignificant change in the active layer and suprapermafrost of this rockglacier of the Cord¨®n del Plata is registered at themonitoring sites. The observed changes imply direct consequences for the cryogenic environment and the Andean creeping permafrost. The nose of the Morenas Coloradas rockglacier for example (Balc¨®n I, 3560 m a.s.l.), already expresses inactivity; the permafrost table is found at great depth (7.5¨C9 m). Data collected at Balc¨®n I and II allow to estimate the theoretical thermal diffusivity ¦Á at the active layer of Morenas Coloradas. Thermal diffusivitymay be decisive for the study of cryogenic dynamics at other altitudes and latitudes in the region where data are still scarce. Low ¦Á values (b0.2¡Á10− 6m2/s) correlate with occurrence of freezing and ice at low altitudes. While the glaciers are turning into small insignificant bodies in the high mountains, the periglacial level with¨C33¡ã S). Asignificant change in the active layer and suprapermafrost of this rockglacier of the Cord¨®n del Plata is registered at themonitoring sites. The observed changes imply direct consequences for the cryogenic environment and the Andean creeping permafrost. The nose of the Morenas Coloradas rockglacier for example (Balc¨®n I, 3560 m a.s.l.), already expresses inactivity; the permafrost table is found at great depth (7.5¨C9 m). Data collected at Balc¨®n I and II allow to estimate the theoretical thermal diffusivity ¦Á at the active layer of Morenas Coloradas. Thermal diffusivitymay be decisive for the study of cryogenic dynamics at other altitudes and latitudes in the region where data are still scarce. Low ¦Á values (b0.2¡Á10− 6m2/s) correlate with occurrence of freezing and ice at low altitudes. While the glaciers are turning into small insignificant bodies in the high mountains, the periglacial level withficant change in the active layer and suprapermafrost of this rockglacier of the Cord¨®n del Plata is registered at themonitoring sites. The observed changes imply direct consequences for the cryogenic environment and the Andean creeping permafrost. The nose of the Morenas Coloradas rockglacier for example (Balc¨®n I, 3560 m a.s.l.), already expresses inactivity; the permafrost table is found at great depth (7.5¨C9 m). Data collected at Balc¨®n I and II allow to estimate the theoretical thermal diffusivity ¦Á at the active layer of Morenas Coloradas. Thermal diffusivitymay be decisive for the study of cryogenic dynamics at other altitudes and latitudes in the region where data are still scarce. Low ¦Á values (b0.2¡Á10− 6m2/s) correlate with occurrence of freezing and ice at low altitudes. While the glaciers are turning into small insignificant bodies in the high mountains, the periglacial level withcreeping permafrost. The nose of the Morenas Coloradas rockglacier for example (Balc¨®n I, 3560 m a.s.l.), already expresses inactivity; the permafrost table is found at great depth (7.5¨C9 m). Data collected at Balc¨®n I and II allow to estimate the theoretical thermal diffusivity ¦Á at the active layer of Morenas Coloradas. Thermal diffusivitymay be decisive for the study of cryogenic dynamics at other altitudes and latitudes in the region where data are still scarce. Low ¦Á values (b0.2¡Á10− 6m2/s) correlate with occurrence of freezing and ice at low altitudes. While the glaciers are turning into small insignificant bodies in the high mountains, the periglacial level with¨C9 m). Data collected at Balc¨®n I and II allow to estimate the theoretical thermal diffusivity ¦Á at the active layer of Morenas Coloradas. Thermal diffusivitymay be decisive for the study of cryogenic dynamics at other altitudes and latitudes in the region where data are still scarce. Low ¦Á values (b0.2¡Á10− 6m2/s) correlate with occurrence of freezing and ice at low altitudes. While the glaciers are turning into small insignificant bodies in the high mountains, the periglacial level with¦Á at the active layer of Morenas Coloradas. Thermal diffusivitymay be decisive for the study of cryogenic dynamics at other altitudes and latitudes in the region where data are still scarce. Low ¦Á values (b0.2¡Á10− 6m2/s) correlate with occurrence of freezing and ice at low altitudes. While the glaciers are turning into small insignificant bodies in the high mountains, the periglacial level with¦Á values (b0.2¡Á10− 6m2/s) correlate with occurrence of freezing and ice at low altitudes. While the glaciers are turning into small insignificant bodies in the high mountains, the periglacial level withficant bodies in the high mountains, the periglacial level with creeping permafrost and linked with rockglaciers is expanding altitudinally, passing a transitional ¡°rooting¡± area which is indirectly feeding the rockglaciers with their covered or ¡°dead ice¡±. The ice of glacigenic origin contributes to the genesis of this type of permafrost. As the permafrost table is found at greater depths, the rockglaciers need to be monitored in order to define a balance between the upper periglacial level (in terms of altitude) with mountain continuous¨Cquasi continuous permafrost and the lower periglacial level to where the lowest fronts of creeping permafrost are reaching. The variations of the cryogenic structure of the rockglaciers of the Cord¨®n del Plata caused bywarming processes, will have direct consequences for the volume of frozen sediments and therefore for the hydrology of the entire region, a fact that has to be taken into account for future socio-economic programs of the respective provincial governments.and linked with rockglaciers is expanding altitudinally, passing a transitional ¡°rooting¡± area which is indirectly feeding the rockglaciers with their covered or ¡°dead ice¡±. The ice of glacigenic origin contributes to the genesis of this type of permafrost. As the permafrost table is found at greater depths, the rockglaciers need to be monitored in order to define a balance between the upper periglacial level (in terms of altitude) with mountain continuous¨Cquasi continuous permafrost and the lower periglacial level to where the lowest fronts of creeping permafrost are reaching. The variations of the cryogenic structure of the rockglaciers of the Cord¨®n del Plata caused bywarming processes, will have direct consequences for the volume of frozen sediments and therefore for the hydrology of the entire region, a fact that has to be taken into account for future socio-economic programs of the respective provincial governments.¡°dead ice¡±. The ice of glacigenic origin contributes to the genesis of this type of permafrost. As the permafrost table is found at greater depths, the rockglaciers need to be monitored in order to define a balance between the upper periglacial level (in terms of altitude) with mountain continuous¨Cquasi continuous permafrost and the lower periglacial level to where the lowest fronts of creeping permafrost are reaching. The variations of the cryogenic structure of the rockglaciers of the Cord¨®n del Plata caused bywarming processes, will have direct consequences for the volume of frozen sediments and therefore for the hydrology of the entire region, a fact that has to be taken into account for future socio-economic programs of the respective provincial governments.fine a balance between the upper periglacial level (in terms of altitude) with mountain continuous¨Cquasi continuous permafrost and the lower periglacial level to where the lowest fronts of creeping permafrost are reaching. The variations of the cryogenic structure of the rockglaciers of the Cord¨®n del Plata caused bywarming processes, will have direct consequences for the volume of frozen sediments and therefore for the hydrology of the entire region, a fact that has to be taken into account for future socio-economic programs of the respective provincial governments.¨Cquasi continuous permafrost and the lower periglacial level to where the lowest fronts of creeping permafrost are reaching. The variations of the cryogenic structure of the rockglaciers of the Cord¨®n del Plata caused bywarming processes, will have direct consequences for the volume of frozen sediments and therefore for the hydrology of the entire region, a fact that has to be taken into account for future socio-economic programs of the respective provincial governments.creeping permafrost are reaching. The variations of the cryogenic structure of the rockglaciers of the Cord¨®n del Plata caused bywarming processes, will have direct consequences for the volume of frozen sediments and therefore for the hydrology of the entire region, a fact that has to be taken into account for future socio-economic programs of the respective provincial governments.