The concentration of continents in one hemisphere would allow Milankovitch cycles to induce
glacial cycles in Westeros - world.
The clincher I understand was the good correlation in the timing of
Glacial cycles in the cores with the peaks & troughs of Milankovitch.
Glacial cycles in the past have been observed on a 41kyr timescale which corresponds to the variation of the Earth's axial tilt.
And another thing coby why doesn't the scientific evidence that i gave you say anything about Co2 setting
glacial cycles in motion?
«The Polar Ocean and
Glacial Cycles in Atmospheric CO2 Concentration.»
There's never been a study that has comprehensively analyzed whether vertebrate communities responded to
the glacial cycles in a uniform way.»
Those cycles operate on much longer timescales than humans tend to worry about and regardless they would have the earth very slowly cooling with a new
glacial cycle in 30 to 50 thousand years.
Not exact matches
Human history is
in grand
cycles parallel to
glacial floods starting
in about 63000 BC from which Puranic records are available.
what is necessary and a very important change for us today and the future is our conscience, and this requires global consciousness necessary for our long term needs and survival, we need a faith that will compel us to unite to address the problems of survival,
in the future, a few thousand years from now the
glacial period
cycle is due, earth will no longer be hospitable and we either have to immigrate to other planets or, develope a system that will protect us, the natural calamities like floods, typhoons, sub zero temperatures, will become our big problem
in the future, so we need a religion that will guide our conscience from simplistic self survival towards a more holistic view of reality.Our oneness with ourselves and Him is the primary tenets or doctrines of this religion.
«Recurrent
glacial cycles have probably selected for a highly mobile arctic flora,» the researchers report
in Science.
Bay mud consists of thick deposits of soft, unconsolidated silty clay, which is saturated with water; these soil layers are situated at the bottom of certain estuaries, which are normally
in temperate regions that have experienced cyclical
glacial cycles.
Now, using two deep cores collected at two Ocean Drilling Program sites
in the Southern Ocean, Jaccard and colleagues have reconstructed ocean records of productivity and vertical overturning reaching back a million years, through multiple
glacial - interglacial
cycles.
But for the other half of the picture — what happened
in the oceans during that time — there is only a relatively short record extending back about 20,000 years to the last
glacial cycle.
The next step for Russell and his colleagues is to see if this pattern is repeated
in multiple
glacial cycles.
So the fact that we have this very strong drying
in the tropics during glaciation would argue for a strong feedback of water vapor concentration to the global climate during
glacial - interglacial
cycles.»
The timing of this decline correlates with environmental changes associated with the onset of the last
glacial cycle, the team reports, whereas archaeological evidence does not support the presence of large populations of humans
in eastern Beringia until more than 15,000 years later.
The sediment cores used
in this study cover a period when the planet went through many climate
cycles driven by variations
in Earth's orbit, from extreme
glacial periods such as the Last Glacial Maximum about 20,000 years ago, when massive ice sheets covered the northern parts of Europe and North America, to relatively warm interglacial periods with climates more like t
glacial periods such as the Last
Glacial Maximum about 20,000 years ago, when massive ice sheets covered the northern parts of Europe and North America, to relatively warm interglacial periods with climates more like t
Glacial Maximum about 20,000 years ago, when massive ice sheets covered the northern parts of Europe and North America, to relatively warm interglacial periods with climates more like today's.
«The meltwater feedback
cycle under the ice shelf will only slow down once the shelf has collapsed, or no more
glacial ice flows
in from inland to take its place.
Patrick Crill, an American biogeochemist at Stockholm University, says ice core data from the past 800,000 years, covering about eight
glacial and interglacial
cycles, show atmospheric methane concentrations between 350 and 800 parts per billion
in glacial and interglacial periods, respectively.
The research team also assessed whether climate sensitivity was different
in warmer times, like the Pliocene, than
in colder times, like the
glacial cycles of the last 800,000 years.
Climate scientists have long suspected that these
glacial cycles are triggered by changes
in our planet's orbit.
The cool reception to the suggestion that GCR's are involved
in glacial - interglacial
cycles comes because there is overwhelming evidence that Milankovic is the basic pacemaker, which needs to be supplemented with an amplifying feedback (certainly involving CO2) and some kind of rectifier of the seasonal
cycle.
In some sense, the search for a theory of glacial - interglacial cycles amounts to a search for the «rectifier» which turns the modulation of the amplitude of the seasonal forcing into a rectified signal in global ice volum
In some sense, the search for a theory of
glacial - interglacial
cycles amounts to a search for the «rectifier» which turns the modulation of the amplitude of the seasonal forcing into a rectified signal
in global ice volum
in global ice volume.
Ecological niche models supported inference of drastic changes
in the extent of its breeding range over the last
glacial — interglacial
cycle.
Timescales covered encompass the last 130 ka,
in particular the time streams of the last
glacial - interglacial
cycle, the Holocene, and the last 2 ka.
We recently extended this record to approximately 120,000 years BP
in order to track vegetation change over a full
glacial cycle at millennial to orbital timescales.
(Top left) Global annual mean radiative influences (W m — 2) of LGM climate change agents, generally feedbacks
in glacial - interglacial
cycles, but also specified
in most Atmosphere - Ocean General Circulation Model (AOGCM) simulations for the LGM.
Ice core records show that atmospheric CO2 varied
in the range of 180 to 300 ppm over the
glacial - interglacial
cycles of the last 650 kyr (Figure 6.3; Petit et al., 1999; Siegenthaler et al., 2005a).
Predicted changes
in orbital forcing suggest that the next
glacial period would begin at least 50,000 years from now, even
in absence of human - made global warming (see Milankovitch
cycles).
While Milankovitch forcing predicts that cyclic changes
in the Earth's orbital parameters can be expressed
in the glaciation record, additional explanations are necessary to explain which
cycles are observed to be most important
in the timing of
glacial — interglacial periods.
We also know humans were pretty much only
in Africa for most of the
glacial cycles and was highly mobile during the most recent.
Changes
in the mode of Southern Ocean circulation over the last
glacial cycle revealed by foraminiferal stale isotopic variability.
a) a
glacial cycle over 100,000 years with warm interglacial periods
in red and the long
glacial period
in between.
The archaeological record suggested that very roughly 150,000 individuals spanned Europe and Asia, living
in small groups of 15 to 25 — and that their total numbers fluctuated greatly during the several climate
cycles (which included harsh
glacial periods) that occurred during the half a million years they inhabited Earth, before going extinct 40,000 years ago.
If you believe that, try the «Rimu», an exploration of the South Island that includes backpacking through national parks, sea kayaking Milford Sound,
cycling the Hollyford Valley and
glacial hiking
in the southern Alps.
This could be explained by the role of the greenhouse gas CO2, which varies
in abundance
in the atmosphere
in sync with the
glacial cycles and thus acts as a «globaliser» of
glacial cycles, as it is well - mixed throughout the atmosphere.
You don't get the minor changes
in insolation from Milankovitch
cycles causing
glacial - interglacial
cycles.
Raymo and Paillard have a good story about the 100KYr
cycle arising from the modulation of the precessional
cycle by the changes
in the Earth's orbital eccentricity, coupled with some
glacial dynamical effects which «rectify» the high frequency precessional signal.
Re # 8, any changes
in climate over
glacial - interglacial timescales have to take into account an additional component: the biogeochemical
cycling of atmospheric gases.
The
glacial interglacial
cycle is like a sine wave and the only possible explanation is
in our perambulations around our galaxy and the effect on our solar system.
Specifically, changes
in the Earth's tilt / seasonality that pace the
glacial process and the carbon
cycle feedbacks that change CO2 by ~ 100 ppm.
Although the primary driver of
glacial — interglacial
cycles lies
in the seasonal and latitudinal distribution of incoming solar energy driven by changes
in the geometry of the Earth's orbit around the Sun («orbital forcing»), reconstructions and simulations together show that the full magnitude of
glacial — interglacial temperature and ice volume changes can not be explained without accounting for changes
in atmospheric CO2 content and the associated climate feedbacks.
There is high confidence that changes
in atmospheric CO2 concentration play an important role
in glacial — interglacial
cycles.
And perhaps you can explain how tiny changes
in insolation
in the course of Milankovitch
cycles give rise to
glacial / interglacial
cycles without significant positive feedback.
Glacial - interglacial cycles are an unfinished story, however, held up primarily by the lack of a good theory for the glacial / interglacial CO2 fluctuations, and a number of uncertainties in ice dy
Glacial - interglacial
cycles are an unfinished story, however, held up primarily by the lack of a good theory for the
glacial / interglacial CO2 fluctuations, and a number of uncertainties in ice dy
glacial / interglacial CO2 fluctuations, and a number of uncertainties
in ice dynamics.
However, if CO2 plays this role it is surprising that climatic proxies indicate that Antarctica seems to have warmed prior to the Northern Hemisphere, yet
glacial cycles follow
in phase with Northern insolation («INcoming SOLar radiATION») patterns, raising questions as to what communication mechanism links the hemispheres.
Instead, it appears that the shift between
glacials and interglacials is a change from one attractor to another, with the
glacial attractor exhibiting (possibly) chaotic oscillations
in the DO
cycles.
So to be safe, use a prior distribution with support the entire real line; afterall the
glacial cycles might be due to something else completely un-understood
in 1959.
Dr. Archer has worked on the ongoing mystery of the low atmospheric CO2 concentration during
glacial time 20,000 years ago, and on the fate of fossil fuel CO2 on geologic time scales
in the future, and its impact on future ice age
cycles, ocean methane hydrate decomposition, and coral reefs.
The conclusion that they survived over at least two
glacial cycles, where the amplitude of environmental change
in the Arctic is quite large, suggests they have under natural conditions the ability to adapt / survive such changes.