I used to illicit gales of laughter when I quoted (in translation, and in my best Sesame Street Swedish Chef voice) dated documents about destitute farmers overwhelmed
by the glacial advance who were seeking parish aid.
Not exact matches
Dating the phases of
glacial advance requires to analyze moraines, rocky debris carried along
by the glacier.
However, until now, it was thought that the glaciers were only affected
by events in the northern hemisphere, based on the dating of past
glacial advances.
Evidence from
glacial advance / retreat (e.g. the evidence from tropical Andean glaciers you cite above) is often difficult to interpret, because
glacial mass balance represents in general a subtle competition between the influences of ablation (determined
by changes in temperature thresholds reached) and accumulation (determined
by changes in humidity and precipitation).
This is because terrestrial deposits of ancient
glacial and interglacial periods1 — 3 are overrun and eroded
by more recent
glacial advances, and are therefore usually rare, isolated and poorly dated.
The
glacial retreat induced
by this or any other process can be amplified
by similar inverse positive feedbacks as for
glacial advances.
Term originally introduced in the late 1930s
by Matthes (1939) to describe a broad interval of the late Holocene during which significant
glacial advances were observed.
If water (rain, clouds, oceans) is the stabilizer, then it should overwhelm any warming
by trace gases, albedo effects of
glacial advances and retreats, etc..
By around 2013 computer models had finally
advanced to the point where modelers could get convincing
glacial cycles.
In the higher altitudes old mines were covered up
by advancing glacial ice.
The observed effects of cryosphere reduction include modification of river regimes due to enhanced
glacial melt, snowmelt
advance and enhanced winter base flow; formation of thermokarst terrain and disappearance of surface lakes in thawing permafrost; decrease in potential travel days of vehicles over frozen roads in the Arctic; enhanced potential for glacier hazards and slope instability due to mechanical weakening driven
by ice and permafrost melting; regional ocean freshening; sea - level rise due to glacier and ice sheet shrinkage; biotic colonisation and faunal changes in deglaciated terrain; changes in freshwater and marine ecosystems affected
by lake - ice and sea - ice reduction; changes in livelihoods; reduced tourism activities related to skiing, ice climbing and scenic activities in cryospheric areas affected
by degradation; and increased ease of ship transportation in the Arctic.