Not exact matches
Sunlight piped from the roof blends with fluorescent light in the fixture down below, offering a
warm glow that looks
much more natural than the harshness of conventional fluorescents.
This
warm air layer gets its heat reflected downwards during cloudy periods, especially during long night extensive cloudy periods, as a result, Arctic ocean ice doesn't thicken so
much during darkness and leaves it up to summer
sunlight (if there is some) to finish off what is left of it.
The Keto Nut Butters will either be a solid or a liquid, depending on the heat,
much the same as coconut oil and butter, if exposed to
sunlight and or
warm temperatures.
One thing I've learned from living in the Bay Area for so long... no matter how
warm it seems or how
much sunlight is out, always carry a jacket.
One of the more foreign - sounding data - gathering probes — the «Sunload Sensor» — reads incoming
sunlight so that the HVAC controller knows how
much to compensate for excess heat generated by the sun's rays
warming interior surfaces.
If vaccines are stored in areas that are too
warm, or exposed to too
much sunlight, they can loose their effectiveness.
This
warm air layer gets its heat reflected downwards during cloudy periods, especially during long night extensive cloudy periods, as a result, Arctic ocean ice doesn't thicken so
much during darkness and leaves it up to summer
sunlight (if there is some) to finish off what is left of it.
(Orbital forcing doesn't have
much of a global annual average forcing, and it's even concievable that the sensitivity to orbital forcing as measured in terms of global averages and the long - term response (temporal scale of ice sheet response) might be approaching infinity or even be negative (if more
sunlight is directed onto an ice sheet, the global average albedo might increase, but the ice sheet would be more likely to decay, with a global average albedo feedback that causes
warming).
Re 9 wili — I know of a paper suggesting, as I recall, that enhanced «backradiation» (downward radiation reaching the surface emitted by the air / clouds) contributed more to Arctic amplification specifically in the cold part of the year (just to be clear, backradiation should generally increase with any
warming (aside from greenhouse feedbacks) and more so with a
warming due to an increase in the greenhouse effect (including feedbacks like water vapor and, if positive, clouds, though regional changes in water vapor and clouds can go against the global trend); otherwise it was always my understanding that the albedo feedback was key (while sea ice decreases so far have been more a summer phenomenon (when it would be
warmer to begin with), the heat capacity of the sea prevents
much temperature response, but there is a greater build up of heat from the albedo feedback, and this is released in the cold part of the year when ice forms later or would have formed or would have been thicker; the seasonal effect of reduced winter snow cover decreasing at those latitudes which still recieve
sunlight in the winter would not be so delayed).
If you put more CO2, say, into the stratosphere then that doesn't change how
much sunlight reaches the Earth's surface
much and the surface
warms up as
much as before.
Climate models projecting that
much less
sunlight will be reflected by low clouds when the climate
warms indicate that CO2 concentrations can only reach 470 ppm before the 2 ℃
warming threshold of the Paris agreement is crossed — a CO2 concentration that will probably be reached in the 2030s.
3] on the
sunlight, CO2
warms up
much more than O&N.
get
warmed up,
much more than O&N; but only during the day b] during the day — they are 6 -7-8km high up; where cooling is
much more effective, that means: less
sunlight on the ground.
As a lay person, I asked why we can't do experiments on a replica of the atmosphere, which would include adding CO2 to it and seeing by how
much it
warmed up in
sunlight / infra red etc..
SRM describes an array of methods — all of which remain hypothetical — for artificially reducing how
much sunlight reaches the Earth's surface in order to dampen global
warming.
How
much longer are you going to try and tell is that
sunlight can not
warm us?
Which didn't answer my question, because I knew the simple answer was no - it's beyond stupid to think it could
warm a swimming pool, the question is how
much could such concentrated
sunlight have on a small quantity of water.
'' The authors attribute the cooling from 7,000 years ago until the Medieval
Warm Period to changes in Earth's orientation toward the sun, which affected how
much sunlight fell on both poles.
It absorbs 1 / 7th as
much IR, heat energy, from
sunlight as water vapor which has 188 times as many molecules capturing 1200 times as
much heat making 99.9 % of all «global
warming.»
Over the course of the twentieth century, Hansen and other climate scientists rierslot.net estimate aerosols may have offset global
warming by as
much as 50 percent by reducing the amount of
sunlight reaching the surface.
The north pole gets no
sunlight until March, but an influx of
warm air has pushed temperatures in Siberia up by as
much as 35C above historical averages this month.
When the northern oceans are
warmer than normal, they freeze later in the season, and since they emit to an almost perfect black body (deep space with no
sunlight) they release
much more heat and take up very little, esp.
The study, using complex climate modeling software to simulate changes in forest cover and then measuring the impact on global climate, found that northern forests tend to
warm the Earth because they absorb a lot of
sunlight without losing
much moisture.
Go a little deeper by saying it allows
sunlight to pass straight through to
warm the surface during the day but slows down the escape of that warmth at night and I think that's pretty
much the whole enchilada in terms the proverbial bartender can understand.
Keeping them open causes a greenhouse like effect —
sunlight and heat pour in all day and can't get out, making your home
much warmer and causing your air conditioning to work overtime, which, in turn, will spike up your power bill.
If it doesn't get
much sunlight, a creamy, soft yellow might make the room feel
warm and sunny.