«Even accounting for the uncertainties of the age of CO2, the deep
sea warmed substantially before the CO2 began to rise,» Stott says.
Not exact matches
One of the most worrisome consequences of global
warming is that
sea levels could rise
substantially this century and beyond.
Contemporary global mean
sea level rise will continue over many centuries as a consequence of anthropogenic climate
warming, with the detailed pace and final amount of rise depending
substantially on future greenhouse gas emissions.
This isn't news to top climate scientists around the world (see Hadley Center: «Catastrophic» 5 — 7 °C
warming by 2100 on current emissions path) or even to top climate scientists in this country (see US Geological Survey stunner:
Sea - level rise in 2100 will likely «
substantially exceed» IPCC projections, SW faces «permanent drying») and certainly not to people who follow the scientific literature, like Climate Progress readers (see Study: Water - vapor feedback is «strong and positive,» so we face «
warming of several degrees Celsius»).
In the first comprehensive international report on Antarctica's climate, there was strong agreement that the West Antarctic Ice Sheet will contribute
substantially to the ongoing rise in
sea levels in a
warming world, while increased snowfall in the interior could offset the contribution somewhat.
As I've written before, while 20 years of intensifying inquiry has greatly reinforced confidence that humans are influencing climate in ways that could profoundly disrupt human and natural affairs, it has not
substantially clarified climate outcomes that matter most: how fast and far temperatures and
seas will rise in the next 100 years, how hurricanes will respond to
warming, how regional conditions will change.
Research indicates that the Arctic had
substantially less
sea ice during this period compared to present Current desert regions of Central Asia were extensively forested due to higher rainfall, and the
warm temperate forest belts in China and Japan were extended northwards West African sediments additionally record the «African Humid Period», an interval between 16,000 and 6,000 years ago when Africa was much wetter due to a strengthening of the African monsoon While there do not appear to have been significant temperature changes at most low latitude sites, other climate changes have been reported.
Contemporary global mean
sea level rise will continue over many centuries as a consequence of anthropogenic climate
warming, with the detailed pace and final amount of rise depending
substantially on future greenhouse gas emissions.
Um... while the oceans as a whole would have to cool, the
sea surface would have to
warm up
substantially in order to transfer lots of heat to the air (and in order to
warm up
substantially, I suppose there would have to be reduced circulation with cold deeper waters).
There are, however, caveats: (1) multidecadal fluctuations in Arctic — subarctic climate and
sea ice appear most pronounced in the Atlantic sector, such that the pan-Arctic signal may be
substantially smaller [e.g., Polyakov et al., 2003; Mahajan et al., 2011]; (2) the
sea - ice records synthesized here represent primarily the cold season (winter — spring), whereas the satellite record clearly shows losses primarily in summer, suggesting that other processes and feedback are important; (3) observations show that while recent
sea - ice losses in winter are most pronounced in the Greenland and Barents
Seas, the largest reductions in summer are remote from the Atlantic, e.g., Beaufort, Chukchi, and Siberian seas (National Snow and Ice Data Center, 2012, http://nsidc.org/Arcticseaicenews/); and (4) the recent reductions in sea ice should not be considered merely the latest in a sequence of AMOrelated multidecadal fluctuations but rather the first one to be superposed upon an anthropogenic GHG warming background signal that is emerging strongly in the Arctic [Kaufmann et al., 2009; Serreze et al., 20
Seas, the largest reductions in summer are remote from the Atlantic, e.g., Beaufort, Chukchi, and Siberian
seas (National Snow and Ice Data Center, 2012, http://nsidc.org/Arcticseaicenews/); and (4) the recent reductions in sea ice should not be considered merely the latest in a sequence of AMOrelated multidecadal fluctuations but rather the first one to be superposed upon an anthropogenic GHG warming background signal that is emerging strongly in the Arctic [Kaufmann et al., 2009; Serreze et al., 20
seas (National Snow and Ice Data Center, 2012, http://nsidc.org/Arcticseaicenews/); and (4) the recent reductions in
sea ice should not be considered merely the latest in a sequence of AMOrelated multidecadal fluctuations but rather the first one to be superposed upon an anthropogenic GHG
warming background signal that is emerging strongly in the Arctic [Kaufmann et al., 2009; Serreze et al., 2009].
The cities» lawsuits allege — supported by modern climate science — that major oil and natural gas companies contribute
substantially to global
warming by extracting and using fossil fuels, which emit massive quantities of heat - trapping greenhouse gases into the atmosphere, causing ocean waters to
warm and ice sheets to melt, and thus,
sea levels to rise, endangering coastal communities.
But a new study published in the journal Science Advances has concluded that another impact of global climate change might help coral reefs survive increasing
sea temperatures: «even a modest
sea level rise can
substantially reduce temperature extremes within tide - dominated reefs, thereby partially offsetting the local effects of future ocean
warming,» the authors of the study write.
During the last interglacial about 125,000 years ago, when global average temperatures were not
substantially warmer than at present,
sea level was 4 - 6 meters (about 13 to 20 feet) higher than at present.
When the climate was much
warmer,
sea levels would have been
substantially higher, because less water would've been locked up as ice.
For example, the argument that follows very
substantially from the extent of continental shelf that there is within the Arctic Basin and, therefore, the particular relationship that
warming on that relatively shallow
sea has on trapped methane - for example, the emergence of methane plumes in that continental shelf, apparently in quite an anomalous way - leading possibly to the idea that there may be either tipping points there or catastrophic feedback mechanisms there, which could then have other effects on things, such as more stabilised caps like the Greenland ice cap and so on.
NOAA has now «decided that the
sea dataset will have to be replaced and
substantially revised just 18 months after it was issued, because it used unreliable methods which overstated the speed of
warming,» The Daily Mail learned.
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.»
[A] nthropogenic climate change is expected to lead to a greater incidence of high - intensity hurricanes, which together with rising
sea level, will produce increased risk of storm surge flooding, while hurricanes are projected to produce
substantially more precipitation as the atmosphere and oceans
warm.