Was it all mathematical models before the development of modern computers? The greenhouse effect predates the PC by about a century or so. Care to explain?
Wait... wait... let me guess. Anyone doing mathematics in the process of a scientific investigation is a useless model.
So what? Of course the atmosphere had a warming effect before we had computers and fossil fuel CO2.
For hundreds of millions of years the Greenhouse Effect was indeed keeping the planet warmer than it would have been without any greenhouse gases in the atmosphere.....but the effect was generally to moderate and stabilize temperatures in a homeostatic balance. Currently the over 46% increase in atmospheric levels of a powerful greenhouse gas, carbon dioxide, has destabilized temperatures and is having a vastly increased "
warming effect", heading towards temperatures not seen on Earth for many millions of years, when the planet was a very different place, with much, much higher sea levels.
And why would you have to "do mathematics" (now) to investigate further if as they say "the science is settled"
Too bad you are so stupid! The phrase "
the science is settled" that has been used in relation to anthropogenic global warming refers to the fact that the basic physics and processes that are causing the current abrupt and rapid global warming are well understood and are no longer in question. It doesn't mean that every aspect and part of what is happening has already been fully investigated and known. It does mean that scientists are quite certain that human activities have caused this 46% increase in CO2 levels, and that it is these highly elevated CO2 levels that are causing the rapid increase in global temperatures.
You guessed wrong, because all the models (so far) are wrong.
Too bad you're so insane, poop4brains! The climate models have proved to be fairly accurate and the predictions resulting from those models seem to be, if anything, somewhat too conservative....things are happening even faster than the models predicted.
Climate models are accurately predicting ocean and global warming
Dr John Abraham, professor of thermal sciences
27 July 2016
From your favorite "science" guru:
The albedo effect and global warming
The Unsettled Science of Albedo
The project reported a counter-intuitive finding. The Earth’s albedo was rising, even as the planet was warming. This seems contradictory, as Anthony Watts was quick to note when he voiced his sceptical argument in 2007. If higher albedo was having a cooling effect, how could global warming be taking place?
Conclusions
Albedo is a subject needing a lot more research. It’s an important feature of our climate, and a complex one. It is not yet possible to make definitive statements about what the future may hold. In fact, it is a good example of the ‘unsettled’ nature of climate change science.
Too bad you are such a braindead
LIAR, POOP4brains!
Citing something and then cherry-picking quotes to distort the meaning is fraudulent debate. Here is the whole quote, which doesn't mean what you are moronically and deceitfully trying to claim:
"Measuring Albedo
The albedo of a surface is measured on a scale from 0 to 1, where 0 is a idealised black surface with no reflection, and 1 represents a white surface that has perfect reflection.
Taking measurements of something with so many variables and influences is clearly going to be a challenge. Satellite data is constrained by the orbit of the satellite. Clouds can be hard to distinguish from white surfaces.
Indirect measurement may also be problematic. The Earthshine project investigated a phenomenon where light reflected by Earth illuminates the dark side of the moon. By measuring the brightness, the amount of albedo - reflectivity - could be estimated.
The project reported a counter-intuitive finding. The Earth’s albedo was rising, even as the planet was warming. This seems contradictory, as Anthony Watts was quick to note when he voiced his sceptical argument in 2007. If higher albedo was having a cooling effect, how could global warming be taking place?
Tricky Business
Science constantly seeks to improve itself. The first Earthshine paper (Palle 2004) claimed to have discovered a very significant cooling effect through a big increase in global albedo.
The results were problematic. They flatly contradicted the NASA CERES satellite observations, and the discrepancy became the subject of investigation. In 2004, a new telescope was installed at the Big Bear observatory, where the project was located. It became evident that the original analysis was inaccurate. Once corrected, the Earthshine project and the satellite measurements were more consistent.
Global versus Local
There are contradictory assessments of current trends in global albedo, possibly because the changes and effects are small. Research is being conducted into the role of clouds, both as forcings and feedbacks, and the role of albedo in cloud formation.
Recent research indicates that global albedo is fairly constant, and having no material effect on global temperatures. Local effects may be more pronounced. Loss of albedo in the Arctic could heat the water sufficiently to release methane stored in ice crystals called clathrates. (Methane is a greenhouse gas far more potent than CO2).
Loss of albedo in the Arctic will accelerate warming across adjacent permafrost, releasing methane. Melting permafrost may reduce its albedo, another positive feedback that will accelerate warming. Ocean warming from reduced Arctic albedo will also accelerate melting at the edges of the Greenland ice cap, speeding up sea level rise.
Conclusions
Albedo is a subject needing a lot more research. It’s an important feature of our climate, and a complex one. It is not yet possible to make definitive statements about what the future may hold. In fact, it is a good example of the ‘unsettled’ nature of climate change science.
We know the planet is warming, and that human agency is causing it. What we cannot say yet is how climate change is affecting albedo, how it might be affected in the future, and what contribution to climate change - positive or negative - it may make."
That goes to show how ignorant of physics these "climate scientists" are.
Nope! Your post once again shows how ignorant of physics and science you actually are, poop4brains......as well as completely afflicted with the
Dunning-Kruger Effect.
They state that 1120 W/m^2 sunlight hitting the ground which they said until now has an albedo of 0.3 leaves enough reflected energy to give us the daylight we have which is anywhere from 10 000 to 25 000 lux indirect sunlight.
Sooooo stupid! "
Indirect sunlight" has almost nothing to do with albedo, or the amount of reflected light from the Earth's surface.
"
Daylight", which you claim "
is anywhere from 10 000 to 25 000 lux indirect sunlight" is basically a combination of (mostly) direct sunlight and the diffuse sky radiation caused by sunlight getting scattered by striking particulates in the atmosphere or interacting with gas molecules.
Diffuse sky radiation is solar radiation reaching the Earth's surface after having been scattered from the direct solar beam by molecules or suspensoids in the atmosphere. It is also called skylight, diffuse skylight, or sky radiation and is the reason for changes in the color of the sky. Of the total light removed from the direct solar beam by scattering in the atmosphere (approximately 25% of the incident radiation when the sun is high in the sky, depending on the amount of dust and haze in the atmosphere), about two-thirds ultimately reaches the earth as diffuse sky radiation. When the sun is at the zenith in a cloudless sky, with 1361 W/m2[1] above the atmosphere, direct sunlight is about 1050 W/m2, and total insolation about 1120 W/m2.[2] This implies that under these conditions the diffuse radiation is only about 70 W/m2 out of the original 1361 W/m2.
The dominant radiative scattering processes in the atmosphere (Rayleigh scattering and Mie scattering) are elastic in nature, by which light can be deviated from its path without being absorbed and with no change in wavelength.
The sunlit sky is blue because air scatters short-wavelength light more than longer wavelengths. Since blue light is at the short-wavelength end of the visible spectrum, it is more strongly scattered in the atmosphere than long-wavelength red light. The result is that when looking toward parts of the sky other than the sun, human eye perceives them to be blue.[3] The color perceived is similar to that obtained by a monochromatic blue of a wavelength of 474–476 nm mixed with white light, i.e., an unsaturated blue light.[4]
Near sunrise and sunset, most of the sunlight arrives nearly tangentially to the Earth's surface; thus, the light's path through the atmosphere is so long that much of the blue and even green light is scattered out along the way, leaving the sun rays and the clouds it illuminates red. Therefore, when looking at the sunset and sunrise, we see the colour red more than the other colors.