Figure 2: DMI summer
melt season temperatures and annual DMI temperature anomaly as well as five year running averages
Not exact matches
1) Pre-heat oven to 300 deg Fahrenheit (150 deg cel) 2) Line one large baking sheet (0r two medium baking sheets) with parchment paper 3) In a large bowl, combine the oats, chia seeds, flax seeds, raisins, almonds and other nuts, and mix well 4) In a smaller bowl, whisk together the honey, light brown sugar,
melted butter and cinnamon until smooth and sugar has dissolved 5) Pour the honey mixture over the dry ingredients and stir well until you get a homogeneous mixture 6) Pour the mixture over the baking sheets and spread evenly with a spatula, then
season lightly with sea salt 7) Bake for 15 minutes, then stir the granola gently (to make sure all sides are cooked) 8) At this point, you may need to switch the baking sheets (if you are using 2) so the granola cooks evenly 9) Bake for another 15 minutes, then stir again, before cooking for a final 15 minutes or until golden brown 10) Remove granola from the oven and place on cooking racks until completely cool and crisp 11) Store granola in air - tight containers at room
temperature.
4 large eggs at room
temperature (this is a must) 1.5 c of low fat milk 1/2 tsp of salt 1.5 c of all purpose flour 1 tsp of Italian
seasoning (you can use whatever
seasonings you would like) 3 tbl of
melted I Can't Believe It's Not Butter or regular butter
Warmer local
temperatures make the snow
melt earlier in the spring, shifting flood
season up, too.
The reason: until the end of the
melting season the fate of the ice is ultimately determined by the wind conditions and air and water
temperatures during the summer months.
Its minimum summertime extent, which occurs at the end of the
melt season, has been decreasing since the late 1970s in response to warming
temperatures.
Climate change is pushing
temperatures up most rapidly in the polar regions and left the extent of Arctic sea ice at 1.79 million square miles at the end of the summer
melt season.
Even so much that there is a cooling
temperature trend in winter, large enough to refreeze almost all ice that was
melted in the other
seasons.
Thursday's toasty reading in Nuuk marks the second exceptionally warm
temperature recorded in southwest Greenland since April, when the ice
melt season began about a month prematurely.
High
temperatures also meant that any snow that did fall
melted very early in the
season, leaving only a smattering come spring.
Emerging from a winter that has had staggeringly warm Arctic
temperatures, scientists monitoring the vast Greenland ice sheet announced Tuesday that it is experiencing a record - breaking level of
melt for so early in the
season.
Last year, the
melt season started two months early thanks to high
temperatures across parts of the island.
In contrast to the midlatitude case, tropical glaciers do not have summertime
melt seasons characterized by above - freezing air
temperature.
BTW, my fearless «denialism forecast» for the next month is for declining mentions of surface
temperature trends, 30 - 50 % chance of more scientist bashing, and sporadic outbreaks of «Arctic sea ice recovery» — at least until the
melting season gathers some steam.
Furiously destructive Hurricanes are not the only indicator of AGW, in context of those Hurricanes cycles in the past, or rather in contrast with past high intensity hurricane
seasons, we now experience all time high
temperatures raging everywhere in the world, 1 meter a day rainfalls, severe droughts on 4 distinct continents, many glaciers going or gone everywhere, and a good chunk of the Arctic Ocean permanent ice
melted.
And the levels of SIE through the coming
melt season will probably reflect those record
temperatures.
Glaciers and ice caps in Arctic Canada are continuing to lose mass at a rate that has been increasing since 1987, reflecting a trend towards warmer summer air
temperatures and longer
melt seasons.
Even so much that there is a cooling
temperature trend in winter, large enough to refreeze almost all ice that was
melted in the other
seasons.
What's been published correlating summer and winter Siberian
temperature with river runoff
temperature and the following
seasons» Arctic ice
melt?
Temperatures on the Greenland ice sheet are well below freezing, and this is peak
melt season.
This causes increased erosion due to permafrost
melt, increased flooding due to the warmer
temperatures, and intensified storms because the sea ice forms later in the
season and is unable to provide a natural barrier for our coastal communities.
But with several factors combining to increase
temperatures in Greenland and reduce the reflectivity of the snow and ice cover, the ice sheet is becoming less efficient at reflecting that heat energy, and as a consequence
melt seasons are becoming more severe.
And, by comparing the DMI 80 north daily
temperature presentation from 1959 - 2014 for the summer
melt season (mid-June to late August when the arctic is above 0.0 Tave), you see very clearly that there has NO warming over the actual arctic ocean.
That is, I expect to go from a sea ice area of 2 or 3 million km ^ 2 to almost nothing in one
melt season as a result of a storm driven by the
temperature differential between the sea ice and the surrounding environment.
After a weeklong delay in data availability from a 61st satellite maneuver in 13 years to makeup low earth orbit drag, we find Greenland ice reflectivity (a.k.a. albedo) returning toward higher values, evidence of fresh snowfall accumulation and accompanying lower
temperatures now as the
melt season approaches its end.
Since the spectacularly pronounced
melting of 2007, a greater proportion of the Arctic Ocean has been covered by thin ice that is formed in a single
season and is more vulnerable to slight
temperature increases than older, thicker ice.
Over the past quarter - century, both the extent of
melting and the length of the
melt season on the Greenland ice sheet have been growing, as local
temperatures have risen.6 Satellites measure the extent of
melting by differentiating between areas of the ice mass that are fully frozen and those with surface meltwater.
Climate change is pushing
temperatures up most rapidly in the polar regions and left the extent of Arctic sea ice at 1.79 million square miles at the end of the summer
melt season.
Higher spring and summer
temperatures, along with an earlier spring
melt, are also the primary factors driving the increasing frequency of large wildfires and lengthening the fire
season in the western U.S. over recent decades.13 The record - breaking fires this year in the Southwest and Rocky Mountain Region are consistent with these trends.
Every element of the hydrologic cycle, to some degree, is
temperature dependent: when it snows versus when it rains; when it
melts, how much evaporates; how much water the plants use; the length of the growing
seasons.
Biologists found plants that provide food for caribou calves in Greenland were starting their growing
seasons earlier, due to a rise in
temperatures linked to
melting Arctic sea ice.
However, at the border of the sea ice minimum, during the only
melting season that exists, air
temperatures have remained steady.
Increased surface
melting, loss of ice shelves, and reduction of summer and autumn sea ice around the Antarctic and Greenland continents during the warmest interglacials would have a year - round effect on
temperature, because the increased area of open water has its largest impact on surface air
temperature in the cool
seasons.
Its minimum summertime extent, which occurs at the end of the
melt season, has been decreasing since the late 1970s in response to warming
temperatures.
When summer
temperatures rise in Greenland and the
melt season begins, water pools on the surface, and sometimes disappears down holes in the ice.