for article Abrupt
glacial climate shifts controlled by ice sheet changes.
Not exact matches
Climate scientists find the last
glacial period interesting because ice cores in Greenland and ocean sediment cores have shown that during this period there were sharp
shifts in global temperatures.
«Ancient Indonesian
climate shift linked to
glacial cycle.»
«Although the
climate system already was primed for the switch, we argue that these changes initiated the
shift from a largely
glacial to a largely interglacial
climate state.
It seems that after the
climate cooled during the last
glacial period, disappearing habitat inland forced brown bears toward the coasts, where they encountered polar bears
shifted there by British - Irish ice sheets.
As recently as the last
glacial period, local
climates and whole biomes
shifted substantially — and in short order, forcing many species to move, adapt or die out.
Given the number of ways that things can go wrong with continued CO2 emissions (from ocean acidfication and sea level rise to simple warming,
shifting precipitation patterns, release of buried carbon in perma - frost, and the possibility of higher
climate sensitivities — which seem to be needed to account for
glacial / inter-
glacial transitions), crossing our fingers and carrying on with BAU seems nothing short of crazy to me.
The interactions (feedbacks) between THC
shifts and sea ice and
glacial calving (as indicated by ice - rafted debris in deep sea core records) would tend to seriously magnify the
climate changes compared to what would be expected from a similar THC
shift today.
The process involves years of analyzing tens of thousands of scientific journal articles on topics ranging from sea level rise and
glacial melt to past
climate shifts.
About 14,500 years ago, the Earth's
climate began to
shift from a cold
glacial world to a warmer interglacial state.
The emergence of civilization during our current interglacial, the Holocene, has been attributed to the «relative
climate quiescence» of this period relative to the massive, abrupt
shifts in
climate that characterized
glacial periods in the form of D - O events.»
---- Mayewski, 2016 http://meetingorganizer.copernicus.org/EGU2016/EGU2016-2567.pdf «The demonstration using Greenland ice cores that abrupt
shifts in
climate, Dansgaard - Oeschger (D - O) events, existed during the last
glacial period has had a transformational impact on our understanding of
climate change in the naturally forced world.
Müller, J. & Stein, R. High - resolution record of late
glacial and deglacial sea ice changes in Fram Strait corroborates ice - ocean interactions during abrupt
climate shifts.
Paleo -
climate research suggests the position of the ASL also
shifts between
glacials and interglacials, and drove warm CDW shoreward during interglacials and accelerated glacier retreat.
«We have analyzed the transition from the last
glacial period until our present warm interglacial period, and the
climate shifts are happening suddenly, as if someone had pushed a button,» said Dahl - Jenson.
The pre-Holocene
climate shifts seem to be well accounted for by dynamics of
glacial meltoff, freshwater discharge, and the impact on the ocean circulation... all of which is less of an issue in an initially warm
climate, and the AR5 generation models give no indication that the overturning circulation will be significantly impacted over the coming century.
Ominously, data showed that sudden
climate shifts did not happen only during a
glacial period.
2.58 million years is of course the Quaternary where we have a
shift in
climate from
glacials interspersed with short interglacials.
In the past
glacial cycles organisms and ecosystems responded to
climate change by
shifting geographical ranges and when unable to
shift local populations died and at times entire species became extinct.
Higher elevation areas could experience altered water flow in some river basins if current rates of
glacial retreat continue, but
shifts in the location, intensity, and variability of rain and snow due to
climate change will likely have a greater impact on regional water supplies.