Sentences with phrase «global sea level response»

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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