Another amusing demonstration of your profound ignorance, wiredwrong. Scientists use the 'global mean temperature' to refer to temperatures at the surface of the Earth. Jupiter has no detectable surface, it is a gas giant planet with a diameter of about 143,000 miles compared to the Earth's diameter of 8000 miles. On Earth, 99.99997% of the atmosphere by mass is below 100 km (62 mi; 330,000 ft) but Jupiter's atmosphere just keeps going down. Five thousand miles deep the pressure is ten times Earth's surface pressure.
Total bullshit, wiredwrong. Climate models are very much based on the laws of physics but you're just too ignorant and retarded to understand that.
More total bullshit based only on your denier cult myths. Astrophysicists studying exoplanets use the same General Climate Models as on Earth and they definitely do incorporate the very real and well verified greenhouse effect. The main difference is that scientists have enormously more direct measurements of conditions on Earth to work with than the very limited measurements they can get for other planets at astronomical distances.
Climate modelling of an Earth-like extrasolar planet orbiting a K-type star (pdf)
(excerpts)
Modelling details
To improve the understanding of the interaction between stellar radiation characteristics, atmospheric dynamics and local planetary conditions, we make use of the 3D general circulation model EMAC (ECHAM/MESSy Atmospheric Chemistry model, [1]), which has been developed for Earth climate studies, to calculate the climate of an Earth-like extrasolar planet around a K-type star.
LOLOLOL....jeez, are you really
that stupid? LOL. You talk about "
the temperature on earth increases with atmospheric pressure as well", which is wrong to begin with, and then cite an upper figure based on the core temperature of the planet. LOL. That's not "
atmospheric pressure", dimwit, it is the pressure of 4000 miles of solid (or molten) rock, not gas.
Atmospheric pressure on Earth has very little to do with the temperature at the surface, nor does ""
the temperature on earth increases with atmospheric pressure" in some linear fashion. Your knowledge of the atmosphere is as minimal and deficient as your knowledge of most everything else, you poor retard. Let me educate you.
Atmosphere of Earth
From Wikipedia, the free encyclopedia
Structure of the atmosphere
Principal layers
In general, air pressure and density decrease in the atmosphere as height increases. However, temperature has a more complicated profile with altitude. Because the general pattern of this profile is constant and recognizable through means such as balloon soundings, temperature provides a useful metric to distinguish between atmospheric layers. In this way, Earth's atmosphere can be divided into five main layers. From highest to lowest, these layers are:
Exosphere
The outermost layer of Earth's atmosphere extends from the exobase upward. It is mainly composed of hydrogen and helium. The particles are so far apart that they can travel hundreds of kilometers without colliding with one another. Since the particles rarely collide, the atmosphere no longer behaves like a fluid. These free-moving particles follow ballistic trajectories and may migrate into and out of the magnetosphere or the solar wind.
Thermosphere
Temperature increases with height in the thermosphere from the mesopause up to the thermopause, then is constant with height. Unlike in the stratosphere, where the inversion is caused by absorption of radiation by ozone, in the thermosphere the inversion is a result of the extremely low density of molecules. The temperature of this layer can rise to 1,500 °C (2,700 °F), though the gas molecules are so far apart that temperature in the usual sense is not well defined. The air is so rarefied, that an individual molecule (of oxygen, for example) travels an average of 1 kilometer between collisions with other molecules.[3] The International Space Station orbits in this layer, between 320 and 380 km (200 and 240 mi). Because of the relative infrequency of molecular collisions, air above the mesopause is poorly mixed compared to air below. While the composition from the troposphere to the mesosphere is fairly constant, above a certain point, air is poorly mixed and becomes compositionally stratified. The point dividing these two regions is known as the turbopause. The region below is the homosphere, and the region above is the heterosphere. The top of the thermosphere is the bottom of the exosphere, called the exobase. Its height varies with solar activity and ranges from about 350–800 km (220–500 mi; 1,100,000–2,600,000 ft).
Mesosphere
The mesosphere extends from the stratopause to 80–85 km (50–53 mi; 260,000–280,000 ft). It is the layer where most meteors burn up upon entering the atmosphere. Temperature decreases with height in the mesosphere. The mesopause, the temperature minimum that marks the top of the mesosphere, is the coldest place on Earth and has an average temperature around −85 °C (−120 °F; 190 K).[4] At the mesopause, temperatures may drop to −100 °C (−150 °F; 170 K).[5] Due to the cold temperature of the mesosphere, water vapor is frozen, forming ice clouds (or Noctilucent clouds). A type of lightning referred to as either sprites or ELVES, form many miles above thunderclouds in the troposphere.
Stratosphere
The stratosphere extends from the tropopause to about 51 km (32 mi; 170,000 ft). Temperature increases with height due to increased absorption of ultraviolet radiation by the ozone layer, which restricts turbulence and mixing. While the temperature may be −60 °C (−76 °F; 210 K) at the tropopause, the top of the stratosphere is much warmer, and may be near freezing. The stratopause, which is the boundary between the stratosphere and mesosphere, typically is at 50 to 55 km (31 to 34 mi; 160,000 to 180,000 ft). The pressure here is 1/1000 sea level.
Troposphere
The troposphere begins at the surface and extends to between 9 km (30,000 ft) at the poles and 17 km (56,000 ft) at the equator,[6] with some variation due to weather. The troposphere is mostly heated by transfer of energy from the surface, so on average the lowest part of the troposphere is warmest and temperature decreases with altitude. This promotes vertical mixing (hence the origin of its name in the Greek word "τροπή", trope, meaning turn or overturn). The troposphere contains roughly 80% of the mass of the atmosphere.[7] The tropopause is the boundary between the troposphere and stratosphere.
More nonsense based only on your own abject ignorance of physics (and everything else, for that matter). Repeating your denier cult myths over and over won't make them become real.
So speaks the ignorant retard who denies the basic laws of science and foolishly imagines that he understands climate science better than the actual climate scientists. You are a silly and very sad joke, wiredwrong, and you'll probably never get your head out of your ass and wake up to reality.