Not exact matches
When
measuring flour or
icing sugar by volume (cup) never scoop the flour /
icing sugar up with the cup otherwise you compress the contents and this can make a big difference in the
amount you're using.
Only a very small
amount is needed to color the
icing, and I
measure it out using the end of a toothpick.
Measure the water in a 2 - cup
measuring cup, adding
ice until the total
amount equals 1 1/2 cups.
Or, you can do what I do and
measure out tablespoon
amounts, put them into
ice cube trays, freeze them, and then dump them out into a bag to stash in the freezer for whenever you need just a bit.
Take approximately 1/4 of the original
amount of honeycomb (this
measure should be mostly crumbs and tiny pieces) and mix it into the
ice cream while it churns.
To that end, they will observe the weather on these
ice shelves,
measure the
amount of surface melt from the ground and from satellites, and analyse how snow characteristics change in response to melt.
Using its three main science instruments, Odyssey has mapped the global distribution of many minerals and chemical elements across the Martian surface, found evidence of large
amounts of buried water
ice near the planet's poles and
measured the radiation environment in low Mars orbit, which could help NASA plan out future manned missions to the Red Planet.
We know the the areal extent of sea
ice is an important
measure of the degree of cold in the Arctic Ocean / sea
ice subsystem of Earth's climate but is it not true that even if areal extent was to increase the
amount of
ice could still be much decreased?
Ice volume, the product of sea ice area and thickness, is a measure for the total loss in sea ice and the total amount of energy involved in melting the i
Ice volume, the product of sea
ice area and thickness, is a measure for the total loss in sea ice and the total amount of energy involved in melting the i
ice area and thickness, is a
measure for the total loss in sea
ice and the total amount of energy involved in melting the i
ice and the total
amount of energy involved in melting the
iceice.
Ice mass loss in Greenland 2003 - 2009 as
measured by GRACE
amounts to 223 + / - 29 Gt / yr.
Researchers
measured variations in the composition of fossilized plankton to gauge the
amount of
ice flowing into the sea over the last 12,000 years.
There are two ways to categorize the
amount of
ice: by
measuring the extent (essentially the area of the ocean covered by
ice, though in detail it's a little more complicated) or using volume, which includes the thickness of the
ice.
Sea
ice can be
measured in square miles, essentially the
amount of area covered by
ice.
http://www.nationalgeographic.com/magazine/2017/07/antarctica-sea-level-rise-climate-change/ By
measuring the
amount of this freshwater, the researchers could estimate how much
ice was being lost.
«New calculations show that the
amount of melted inland
ice in Greenland is 25 - 50 % higher in 2010 than normally -LSB-...] «It is my assessment that we have had the strongest melting since they started
measuring the temperature in Greenland in 1873,» he said.»
The figure below shows the total
amount of surface (red) and bottom (yellow) melt through 1 August 2008
measured at seven sea
ice mass balance buoys.
For instance the Vostok
ice - core data over 415,000 years has an average measurement - spacing of 756 years, meaning that the likelihood of
measuring an increase in atmospheric CO2 as the one
measured at Mauna Loa over the last 50 years, if one existed in the Vostok
ice - core samples,
amounts to 6.6 % (i.e. 50/756).
They are limited only by the
amount of water the glaciers themselves release —
ice masses that hold volumes of water often
measured in cubic kilometers.
Arctic sea
ice reached its maximum annual extent on March 21, and the
amount measured was the fifth - lowest level ever recorded.
As explained in the press release, the scientists began with the
measure of sea level rise between 2005 and 2013, then deducted the
amount of rise due to meltwater (e.g., melting
ice sheets and loss of glacier mass worldwide) and then the
amount of rise due to the expansion of water from the warming in the upper portion of the world's oceans (which scientists have good data on).
Ablation stakes are used to
measure the
amount of firn and
ice lost beneath the previous winter's snowpack.
For average absolute error, or the
amount of
ice that the sensor
measures compared to actual
ice on the ground, the error is approximately 50 thousand to 1 million square kilometers (19,300 to 386,100 square miles), varying over the year.
However, they're not
measuring ice thickness but
ice draft, the
amount of
ice below the water line.
They
measured soot concentrations in
ice cores from five Tibetan glaciers, and found radiatively significant
amounts in all but one, with evidence for recent increases in at least two.
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