i added the dried fruit with the nuts... since none of mine burned in the oven im wondering if
the different heating point of the oil had anything to do with it?
Not exact matches
Eleven
different Heat players scored at least two
points on Wednesday.
See you soon folks, we may differ from our opinions, argue, get
heated on debates but this what makes this community so amazing with
different points of views and very insightful analysis from our beloved club.
The battle for Premier League survival is really
heating up with just three games to go, and this weekend's match between Gus Poyet's Sunderland and Ole Gunnar Solskjaer's Cardiff City is no
different, with just one
point seperating the two sides, and Cardiff playing one more game than the Black Cats.
To generate an accurate picture of the temperature profile within the Earth's centre, scientists can look at the melting
point of iron at
different pressures in the laboratory, using a diamond anvil cell to compress speck - sized samples to pressures of several million atmospheres, and powerful laser beams to
heat them to 4000 or even 5000 degrees Celsius.
In a matter of seconds, when you put the food in the fryer, water starts evaporating, vapors form and escape the surface, oil penetration starts, and
heat begins to rise while at the same time there's evaporative cooling off at
different points in the food.
«But Waggle's low price
point and scalability make it possible to get very dense coverage throughout
different areas and ultimately a better understanding of where and how these
heat islands will occur.»
The fractionation process involves
heating then cooling the oil when it is liquid, thus separating it to «fractions» that have
different melting
points.
Different oils have different smoke points and these are often included on the product label (but not always) as «medium heat,» «medium - high heat,&raq
Different oils have
different smoke points and these are often included on the product label (but not always) as «medium heat,» «medium - high heat,&raq
different smoke
points and these are often included on the product label (but not always) as «medium
heat,» «medium - high
heat,» etc..
I love cooking with virgin olive oil, but I save the extra virgin for after
heat, and if I need to go above 200C I use a
different oil No smoke
point, no problem.
This morning's panel discussion on the importance of ebook pricing was polite but
heated as the
different panelists disagreed on the inherent built - in factors that affect ebooks and their price
points.
Sou at HotWhopper (linked above)
points out that Watts can't explain why a
heat sink or a reflective surface at a station would produce not just a
different temperature but a
different trend over time.
By the way, here is a somewhat
different view of the issue, which
points to a more dominant role for atmospheric rather than oceanic
heat transport, courtesy Richard Seagar: http://www.ldeo.columbia.edu/res/div/ocp/gs/
The
point you raise is any molecule [including gas molecules] can absorb [at certain wavelengths] and re-radiate energy [at same or
different wavelengths depending on molecule] and not
heat up a body of gas, liquid, or solid.
The
point may seem minor, but it transforms «adiabatic lapse» from a sort of «miracle
heating» that starts from an outside boundary condition and
heats to the surface via lapse into a consequence of forced convection due to the differential delivery of
heat to the surface, a dynamic process and not a static one, one that goes away if you stop actively maintaining the surface and some part of the atmosphere overhead at
different temperatures.
The
point is that when we turn to the real world, we immediately notice that the fate of
heat and number of molecules are fundamentally
different.
The blackbody temperature isn't particularly relevant at a single
point at the surface because there are lots of
different heat transport mechanisms that affect the local surface energy balance and there's lots of thermal inertia at the surface, particularly the oceans.
[Response: Your argument misses the
point in three
different and important ways, not even considering whether or not the Black Hills data have any general applicability elsewhere, which they may or may not: (1) It ignores the
point made in the post about the potential effect of previous, seasonal warming on the magnitude of an extreme event in mid summer to early fall, due to things like (especially) a depletion in soil moisture and consequent accumulation of degree days, (2) it ignores that biological sensitivity is far FAR greater during the warm season than the cold season for a whole number of crucial variables ranging from respiration and photosynthesis to transpiration rates, and (3) it ignores the potential for derivative effects, particularly fire and smoke, in radically increasing the local temperature effects of the
heat wave.
I have difficulties to understand rasmus's
point «A change in the global mean temperature is
different to, say the flow of the Nile, since the former implies a vast shift in
heat (energy), and there has to be physical explanations for this.»
Chris, my
point is that there is many many
different ways for this
heat to get distributed in the climate system.
As you
point out, there are many
different combinations of
heat transfer processes and states of the atmosphere and surface that can provide that same value of tropopause radiative fluxes.