Not exact matches
Its high quality and distinctive flavour, with notes of fresh basil and Mediterranean herbs finished with citrus and pepper, enables it to hold its own in a variety of cocktails — as the refreshing taste profile creates a unique drinking experience with a signature gin and tonic or all - Italian Negroni — as well as appealing to the growing
trend of enjoying super-premium spirits neat
over ice».
Signature Milkshakes — According to Datassential, the specialty
ice cream
trend is taking
over, giving rise to
over-the-top
ice cream builds that beg to be Instagrammed — including not only sundaes but also milkshakes.
The record follows a
trend over the past three years of anomalously high winter
ice extents, providing a stark contrast to the inexorable decline of Arctic sea
ice
A new NASA
ice - elevation monitoring satellite called ICESAT, scheduled for launch in 2001, will help scientists watch for climate - change
trends near the poles
over a longer time frame, he notes.
Ice all
over the world is melting, particularly in the Arctic, a
trend that will continue unabated.
Monckton says «The Antarctic, which holds 90 percent of the world's
ice and nearly all its 160,000 glaciers, has cooled and gained
ice - mass
over the past 30 years, reversing a 6,000 - year melting
trend.»
The findings suggest that Antarctic sea
ice has fluctuated substantially through the last century, rather than experiencing the sort of steady
trend seen in the Arctic
over many decades.
In addition to body changes, drastically less free time and money to spend on shopping, curating clothes, and paying attention to fashion
trends, and increased likelihood of kid staining, stretching clothes, theres also the fact that you basically put your entire wardrobe on
ice for a year or more due to pregnancy and nursing, so it doesn't really get the gradual updating
over time that people normally do, so the little wardrobe details like how pants or sweaters fit or which boots you have will just be a little more behind the fashion curve.
The downward
trend in
ice area
over 30 years is much greater in the Arctic summer than in the Arctic winter.
So it seems you have a very conservative estimate from the CMIP ensembles, which are known to suffer from various weaknesses wrt sea
ice, and which certainly don't capture the
trends over the last decade or so.
«According to a 1972 article in the Christian Science Monitor, Belchen asserted that «a general warming
trend over the North Pole is melting the polar
ice cap and may produce an
ice - free Arctic Ocean by the year 2000 ″»
Richard B. Alley of Penn State has long been a source I call on when I'm puzzling
over the latest study of
ice trends in the Arctic or Antarctica.
What about the feedbacks that are not normally well represented by ECS and normally fall into the Earth System Climate Sensitivity, stuff like the Arctic
Ice cover, which now has
trends over decades closer to what was seen on centuries in paleoclimate:
We find a consistent decreasing
trend in Arctic Ocean sea
ice thickness since 1979, and a steady decline in the Eastern Arctic Ocean
over the full 40 - year period of comparison that accelerated after 1980, but the predictions of Western Arctic Ocean sea
ice thickness between 1962 and 1980 differ substantially.
The most exciting thing is we'll get a chance to see the relative strength of all of these
over the next few years, and it will most interesting to compare the total decade of 2010 - 2019 to previous decades in terms of the
trends in Arctic Sea
ice, Global Temps, and of course, OHC.
The lower
trend found by our study is consistent with the median projected sums of thermal expansion and glacier mass loss, implying that no net contribution from polar
ice sheets is needed
over 1901 - 1990.
You can make your own list, I am sure — the retreat of the Arctic
ice last summer, Greenland melt,
trends in Atlantic hurricanes
over the past 20 years, etc..
Indeed it was Law Dome, not the Taylor Dome... I had written that from memory, but as my memory is not anymore what it was 40 years ago... What I meant was a graph on the Internet, showing the Law Dome
ice core CO2 variations, lagging the temperature variations with some 50 years (with ~ 10 ppmv / K, similar to the factor found
over the Vostok
ice core
trends).
«I wonder whether
over all the
trend towards thinner younger
ice may have resulted in a net underestimation rather than overestimation of the area of multiyear
ice.
But, he also says: «teams offering projections say
ice extent will remain well below the average for the last quarter century and a downward
trend in summer
ice around the North Pole has not abated,» and we readers are then linked to his October, 2007 article and an August, 2007 image of a «warmed
over» Artic.
Over all, the analysts as a group see no deviation from the long - term
trend toward thinning and dwindling summer sea
ice given how the Arctic tends to amplify the long - term global warming
trend.
We're not talking about day trading here, we're talking climate and long range
trends like a steady decline in sea
ice over decades, shrinking glaciers world - wide, deforestation, etc..
Over all, Dr. Rigor says, the enduring
trend is toward diminishing sea
ice in summers.
iheartheidicullen @ 162: Sorry if my tone was intemperate, but really the SH and NH sea
ice trends have been analysed at length online by Tamino and others,
over the last year or two, with the clear conclusion that the SH anomaly
trend is small (the anomaly at the maximum last year was about 1.5 % of the mean annual maximum, if I remember correctly) and not statistically significant (at the 95 % level, I think), whereas the NH
trend is large (tens of percent), long - lived, and statistically very significant indeed.
Some commentators have made much of longer - term
trends in
ice thickness, but there, too, winds and patterns of atmospheric pressure have played a powerful role
over longer time spans.
The sea
ice grows and recedes with the seasons every year and has been on the decline since spring... and the overall
trend over time is definitely downward.
Businesses, in order to plan for this, have to really see this
trend over multiple years; they are not going to make huge investment based on one or two years [of low
ice conditions].
People observed this
trend of earlier
ice - out dates by comparing to their own recollections, and all one has to do is look at the aggregated data which has been collected
over the years.
Again, the emissions
trend, be it more irregular, due to the resolution and accuracy of the
ice core measurements and emission inventories, is far superior
over the temperature - CO2
trend.
This model has been proven skillful in reproducing the monthly arctic (and Antarctic) sea
ice extent anomalies
over the last 30 years, as well as the observed long - term downward
trend.
This low - C13 carbon most certainly would have been released massively into the atmosphere
over the course of the world's warming
trend since 1850, when the Little
Ice Age ended.
«The global temperature has been rising at a steady
trend rate of 0.5 °C per century since the end of the little
ice age in the 1700s (when the Thames River would freeze
over every winter; the last time it froze
over was 1804)...
Over the long - term, melting of the West Antarctic
Ice Sheet could yield as much as 10 to 14 feet of global average sea level rise, with local sea level rise varying considerably depending on land elevation
trends, ocean currents and other factors.
This despite a cooling
trend over the last three millennia, if the Greenland
ice cores are accurate.
If
trends continue, Lake Superior, which freezes
over completely once every 20 years, could routinely be
ice - free by 2040.
Evidence suggests that the negative phase of the Arctic Oscillation was driven in part by warm air (air warmed by the dramatic seasonal loss of Arctic sea
ice) 9 as well as by changes in snow cover
over Eurasia driven by climate change.10 This event is part of an emerging
trend in which a warming climate may paradoxically bring colder, snowier winters to northern Europe and the eastern United States.11
«despite increased observational uncertainty in the pre-satellite era, the
trend in [Arctic sea
ice extent]
over this longer period [1953 — 2010] is more likely to be representative of the anthropogenically forced component.»
-- The third, being the observed destabilization of the geosphere due to both the pace of terrestrial
ice loss and relatively sudden and uneven climatic redistribution of the oceans» mass, with a consequent rise in seismic events and in volcanoes» cooling sulphate emissions, which have (according to Prof. McGuire, adviser to Munich Re on vulcanism risks) accelerated slowly on a 1.25 % / yr
trend over the last 30 years.
As of this writing, there is observational and modeling evidence that: 1) both annular modes are sensitive to month - to - month and year - to - year variability in the stratospheric flow (see section on Stratosphere / troposphere coupling, below); 2) both annular modes have exhibited long term
trends which may reflect the impact of stratospheric ozone depletion and / or increased greenhouse gases (see section on Climate Change, below); and 3) the NAM responds to changes in the distribution of sea -
ice over the North Atlantic sector.
Then it said «If the general positive
trend in Atlantic heat input remains, winter cooling will likely be insufficient to produce
ice over an increasing area, leading to further «Atlantification» of the Barents Sea.»
If you correct for the discontinuity in the way area is measured, it's undeniable that global sea
ice has
trended down
over the time span monitored by satellites.
Taken together, these changes suggest that at least part of the thinning of sea
ice recently observed
over the Arctic Ocean can be attributed to the
trend in the AO toward the high - index polarity.
This is substantially lower than the earlier estimates, reflecting both lower than average sea
ice extent used as initial conditions this summer and a persistent downward
trend in sea
ice extent
over the past decade (and longer).
Since the tropical oceans have flattened out and solar does have its largest impact on the tropical oceans, I would expect about the same possibly some increase in Arctic sea
ice over the next decade Not a consistent increase by any means, but I doubt it will make it to the 2 mkm ^ 2 and will
trend towards a 6 million km ^ 2 average which is hardly «
ice free».
I'm very convinced that the physical process of global warming is continuing, which appears as a statistically significant increase of the global surface and tropospheric temperature anomaly
over a time scale of about 20 years and longer and also as
trends in other climate variables (e.g., global ocean heat content increase, Arctic and Antarctic
ice decrease, mountain glacier decrease on average and others), and I don't see any scientific evidence according to which this
trend has been broken, recently.
The pattern of temperatures shows a rise as the world emerged from the last deglaciation, warm conditions until the middle of the Holocene, and a cooling
trend over the next 5000 years that culminated around 200 years ago in the Little
Ice Age.
Actually Fielding's use of that graph is quite informative of how denialist arguments are framed — the selected bit of a selected graph (and don't mention the fastest warming region on the planet being left out of that data set), or the complete passing
over of short term variability vs longer term
trends, or the other measures and indicators of climate change from ocean heat content and sea levels to changes in
ice sheets and minimum sea
ice levels, or the passing
over of issues like lag time between emissions and effects on temperatures... etc..
The first graph on global sea
ice area uses an expanded scale in an attempt to hide the fact that indeed, there's a declining
trend (caption «no
trend over 30 years»).
---- Cerrone and Fusco, 2017 http://journals.ametsoc.org/doi/abs/10.1175/JCLI-D-17-0184.1 Compelling evidence indicates that the large increase in the SH [Southern Hemisphere] sea
ice, recorded
over recent years, arises from the impact of climate modes and their long — term
trends.
Such models also indicate that warming would initially cause the Antarctic
ice sheet as a whole to gain mass owing to an increased accumulation of snowfall (*; some recent studies find no significant continent - wide
trends in accumulation
over the past several decades; Lemke et al., 2007 Section 4.6.3.1).