Release of hydrates below retreating ice sheets could therefore act as a hitherto neglected positive feedback
during warming episodes.
«Ocean temperatures rose substantially
during that warming episode — as much as 7 to 9 degrees Celsius (about 12 to 16 degrees Fahrenheit) in some areas of the North Atlantic.
«Ocean temperatures rose substantially
during that warming episode — as much as 7 to 9 degrees Celsius (about 12 to 16 degrees Fahrenheit) in some areas of the North Atlantic.
Not exact matches
In addition,
during the
warmest years — particularly the record - breaking 1997 - 1998 El Nino
episode — the rain - forest trees experienced the least growth and expelled the most carbon dioxide, the scientists report.
During El Niño episodes, Montana tends to experience warmer - than - average temperatures and below - average precipitation, especially during the winter and s
During El Niño
episodes, Montana tends to experience
warmer - than - average temperatures and below - average precipitation, especially
during the winter and s
during the winter and spring.
[11] This
episode marked the close of the Precambrian eon, and was succeeded by the generally
warmer conditions of the Phanerozoic,
during which multicellular animal and plant life evolved.
These
episodes occurred toward the end of a period of hundreds of millions of years
during which
warm water interacted with subsurface rocks.
While the specific triggers for BCC
episodes may vary from one dog to another,
warm or hot environmental temperature, intensity of exercise, excitement
during exercise, an excitable disposition, or high stress levels may contribute.
Decreased sea ice area
during December preceded «94, «97, «02 and «06
warm episodes.
[Response: And note that the abstract linked says «Although the rarity of the current
episode of high average sunspot numbers may indicate that the Sun has contributed to the unusual climate change
during the twentieth century, we point out that solar variability is unlikely to have been the dominant cause of the strong
warming during the past three decades.»
One of the really troubling long - term aspects of oceanic
warming is the possibility of anoxic oceans, which have occurred in the deep past
during «hothouse Earth»
episodes.
I would like to read a book about how the rate and degree of
warming expected to take place over the next couple centuries compares with global
warming episodes in Earth's past, and how today's plants and animals might not survive climate change and heat waves more severe than experienced
during the climates in which their species evolved.
I can see how the anomalous westerlies and high surface pressure could contribute to
warmer SSTs north of 20N in the Atlantic
during El nino
episodes, but to say it weakens the trade winds in the tropical belt is incorrect, most especially
during the summer months when the Azores - Bermuda High is farther north.
Greenland has undoubtedly contributed to
episodes of accelerating and decelerating sea level changes, but the greatest rate of Greenland
warming occurred
during the 1920s and 30s.
Their reconstruction «shows a succession of
warm and cold
episodes including peak warmth
during Roman and Medieval times alternating with severe cool conditions centred in the fourth and fourteenth centuries.»
Therefore one would expect to see the rate of
warming between the late 197s and the late 1990s to be greater than the rate of
warming that occurred
during the earlier two
warming episodes.
The best way to envision the relation between ENSO and precipitation over East Africa is to regard the Indian Ocean as a mirror of the Pacific Ocean sea surface temperature anomalies [much like the Western Hemisphere
Warm Pool creates such a SST mirror with the Atlantic Ocean too]:
during a La Niña
episode, waters in the eastern Pacific are relatively cool as strong trade winds blow the tropically Sun -
warmed waters far towards the west.
However, Solanki et al made the same point as we do: «This comparison shows without requiring any recourse to modeling that since roughly 1970 the solar influence on climate (through the channels considered here) can not have been dominant» (Solanki et al., 2003), and: «Although the rarity of the current
episode of high average sunspot numbers may indicate that the Sun has contributed to the unusual climate change
during the twentieth century, we point out that solar variability is unlikely to have been the dominant cause of the strong
warming during the past three decades.»
Reconstructed Arctic SATs show
episodes of
warming during this per - iod (Fig. 3f), but according to our results the decrease in Arctic sea ice extent
during the Little Ice Age was more pronounced than
during the earlier Medieval
Warm Optimum.»
On the whole is it not true to say that
during high sunspots
episodes the equatorial areas are
warmed, and
during coronal hole events the polar regions are
warmed?
The world tends to be slightly
warmer during El Niño
episodes — 1998 is a great example of that.
Will
warmer temperatures mean more pollution
during these
episodes?
We know that tropical creatures inhabited high latitudes
during various hothouse
episodes, so the possibility exists that a large chunk of the 14 C deltaT was in temperate and higher latitudes, with the tropics only modestly
warmer.