Climate reconstruction since the Little Ice Age by modelling Koryto glacier, Kamchatka Peninsula, Russia

Little Ice Age climate reconstruction from ensemble reanalysis of Alpine glacier fluctuations

Mountain glaciers sample a combination of climate fields – temperature, precipitation and radiation – by accumulation and melting of ice. Flow dynamics acts as a transfer function that maps volume changes to a length response of the glacier terminus. Long histories of terminus positions have been assembled for several glaciers in the Alps. Here I analyze terminus position histories from an ense...

Little Ice Age

Volume 1, The Earth system: physical and chemical dimensions of global environmental change, pp 504–509

Kliuchevskoi Volcano, Kamchatka Peninsula

Climatic warming, glacier recession and runoff from Alpine basins after the Little Ice Age maximum

Records of discharge of rivers draining Alpine basins with between 0 and 70% ice cover, in the upper Aare and Rhône catchments, Switzerland, for the period 1894–2006 have been examined together with climatic data for 1866–2006, with a view to assessing the effects on runoff from glacierized basins of climatic warming coupled with glacier recession following the Little Ice Age maximum. Annual ru...

Evidence for external forcing of the Atlantic Multidecadal Oscillation since termination of the Little Ice Age

The Atlantic Multidecadal Oscillation (AMO) represents a significant driver of Northern Hemisphere climate, but the forcing mechanisms pacing the AMO remain poorly understood. Here we use the available proxy records to investigate the influence of solar and volcanic forcing on the AMO over the last ~450 years. The evidence suggests that external forcing played a dominant role in pacing the AMO ...