Together these influences drove exceptional moisture transports into the continent's interior (Fig. 3a) and were likely responsible for one of the wettest intervals in Australia's recorded history, the intensity and persistence of its terrestrial storage anomaly, and a considerable fraction of
the global sea level response.
Not exact matches
[this is useful, the pre-ice age era, ~ 2.5 — 3.6 million years ago, last time CO2
levels were as high as today] In
response to Pliocene climate, ice sheet models consistently produce near - complete deglaciation of the Greenland ice sheet (+7 m) and West Antarctic ice sheet (+4 m) and retreat of the marine margins of the Eastern Antarctic ice sheet (+3 m)(Lunt et al., 2008; Pollard and DeConto, 2009; Hill et al., 2010), altogether corresponding to a
global mean
sea level rise of up to 14 m.
In
response,
global sea level rises, increasing the threat of coastal inundation during storms.
Polar amplication is of
global concern due to the potential effects of future warming on ice sheet stability and, therefore,
global sea level (see Sections 5.6.1, 5.8.1 and Chapter 13) and carbon cycle feedbacks such as those linked with permafrost melting (see Chapter 6)... The magnitude of polar amplification depends on the relative strength and duration of different climate feedbacks, which determine the transient and equilibrium
response to external forcings.
The simple approach is only valid for the initial
sea level response to large and rapid rise in
global temperature, as sketched in Fig. 1 of my paper.
Regarding the «
global ice at 1980
levels», here is the canned
response we wrote in rebuttal to the astonishingly twisted piece in Daily Tech: What the graph shows is that the
global sea ice area for early January 2009 is on the long term average (zero anomaly).
Overall, the panel's reports have never focused much on research examining how humans respond (or fail to respond) to certain kinds of risk, particularly «super wicked» problems such
global warming, which is imbued with persistent uncertainty on key points (the pace of
sea -
level rise, the extent of warming from a certain buildup of greenhouse gases), dispersed and delayed risks, and a variegated menu of possible
responses.
JC comments: When I raise the issue of emphasizing adaptation over mitigation, the
response I often get is that the
sea level rise issue is so
global and overwhelming that mitigation is the only sensible way to deal with the
global sea level rise.
Projections of mean
global sea -
level (GSL) rise provide insufficient information to plan adaptive
responses; local decisions require local projections that accommodate different risk tolerances and time frames and that can be linked to storm surge projections.
Consistent with the aforementioned
sea level rise acceleration, a number of articles have projected
global sea level rise of around 1m or more by 2100, based on past estimates of
sea level rise (in
response to warming) and based on melting of land ice (with thermal expansion):
The millennial (500-2000 year) time scale of deep ocean ventilation affects the time scale for natural CO2 change and thus the time scale for paleo
global climate, ice sheet, and
sea level changes, but this paleo millennial time scale should not be misinterpreted as the time scale for ice sheet
response to a rapid large human - made climate forcing.
Tamino doesn't want to admit that there's been no detectable acceleration in the
global average rate of
sea -
level rise in
response to ~ 2/3 century of steadily increasing CO2 emissions and
levels, but that's what the data unambiguously shows.
Rather, it both offers a tool for exploring the
sea level implications of polar ice sheets» complex physical
responses to
global warming and highlights the deep uncertainty that characterizes
sea level change in a high - emissions future.
It will be the impact of
sea level rise, as a consequence of
global warming driven by ever higher greenhouse gas
levels in the atmosphere, in
response to the profligate
global consumption of fossil fuels.
Click that and within the abstract:» The new cGPS stations will, in some cases, be co-located with existing tide gauges, thus supporting studies of
sea level change in
response to current
global warming».
In the graphs above you then see the effect this has on the CO2 concentration, the
global average temperature, and the
sea level, and how this
response is damped.
The largest unknown for future
sea level rise is caused by uncertainty in the predicted
response of the Antarctic ice sheet to
global warming.
Global sea levels are on the rise, and oceans have become more acidic in
response to rising carbon dioxide
levels.
Sea level rise is happening everywhere, as ice caps and glaciers melt and the
seas rise in
response to
global warming driven by prodigal human combustion of fossil fuels, and researchers have advanced from general warning to the kind of detail that could help city and state planners prepare to cope with flood risks.
Such rates of
sea level change have occurred many times in Earth's history in
response to
global warming rates no higher than those of the past 30 years.
The FLOR model has been used extensively to understand predictability, change and mechanisms of tropical cyclones (Vecchi et al. 2014), Arctic
sea ice (Msadek et al. 2014), precipitation and temperature over land (Jia et al. 2015), drought (Delworth et al., 2015), extratropical storms (Yang et al. 2015), the Great Plains Low
Level Jet (Krishnamurthy et al. 2015), and the
global response to increasing greenhouse gases (Winton et al. 2014).
req'd] concluded, «Natural and anthropogenic aerosols have substantially delayed and lessened the total amount of
global ocean warming — and therefore of
sea level rise — that would have arisen purely in
response to increasing greenhouse gases.»
The Last Interglacial was also a period with higher
global sea -
level and a corresponding reduction in ice sheet area and volume, which are consistent with IPCC predictions for
responses to future
global warming.
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responses to climate change issues developed throughout the country, along with updates on scientific discoveries and case law addressing greenhouse gases,
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global warming and climate change.»