For most breeds, this is
at least the second heat cycle; it may be longer in larger breed dogs.
Not exact matches
Heat another 30
seconds, and stir chocolate until completely melted, which may take
at least 30
seconds of stirring.
-- On a lower speed, add eggs one
at a time and vanilla until well incorporated — Increase mixing speed to high and let it go for 10 minutes — the mixture will become really pale and will almost double in size — In a medium sized bowl, whisk together flour, baking powder, baking soda, and salt — When 10 minutes are up, add flour mixture slowly until just combined, about 45 - 60
seconds — Chop up and mix together all of your baking and snack ingredients in a small bowl, and fold into batter with a spatula until just incorporated — Using a medium - sized ice cream scoop, portion cookie dough on parchment paper - lined cookie sheet and wrap the entire thing tightly with plastic wrap — Refrigerate for a minimum of 1 hour and up to 1 week —
Heat oven to 400F and arrange cookies on cookie sheets
at least 4 ″ apart — Bake 9 - 11 minutes, until they are golden in color and slightly brown along the edges — Cool the cookies completely on the sheet pan (or just eat them immediately...)
Next, add your oil or butter or whatever fat you're using and fully
heat it too,
at least another 30
seconds.
An utterly fearless type whose only fault is that he sometimes babies his engine, Muncey has made tentative plans to drive a
second boat, Thriftway Too, in
at least the first
heat of the Gold Cup.
It's not easy to repeat — even if your name is Trinity Wilson The nation's top 100 - meter hurdler is shutting it down until
at least May due to a big left toe injury she sustained
at the Stanford Invitational while winning her trials
heat in a national - best time of 13.41
seconds.
Only molecules made of
at least three atoms absorb
heat radiation and thus only such trace gases makes the greenhouse effect, and among these CO2 is the
second most important after water vapor.
Many of the mechanisms are like that — the tides, the direct inductive
heating, the
heating caused by the days influx of falling meteorites — which incidentally is far greater than the rate of
heat loss through outgassing, as meteoric dust and matter infalls
at an average rate of
at least millimeters per decade, from my own direct measurements — they have «impressively» large amounts of annual energy associated with them, right up to where you divide by the surface area of the earth and the number of
seconds in a year.
That's why I kept the argument in the top post above simple — limited to addressing only Jelbring and the EEJ paper so we could do adiabatic apples to apples reasoning, limited to a picture that even people who don't know much physics can understand — anybody who has tried to touch the handle of a
heating pan and found it hot to the touch has direct experience of Fourier's Law, so whether or not they fully understand the algebra they know this happens — and appealing to their intuition as much as to the letter of the various forms of the
second law (there are
at least four or five that I know of offhand).
The notion that over the longer timescales, forced responses dominated (
at least for the
second half of the past century) is reinforced by data on Ocean
Heat Uptake since 1955.
Ocean
heat content is one of the most inert components of the climate system,
second only to the huge ice sheets on Greenland and Antarctica (hopefully
at least — if the latter are not more unstable than we think).»
According to the EIA, «
Heating degree days in 2016 were the
second fewest of any year since
at least 1949, consistent with relatively warmer winter months.»