The very POWERFUL the Solar Irradiated planet surface Rotational Warming Phenomenon: ( N*cp )^1/16

Written by Christos I. Vournas,

M.sc. mechanical engineer

We do planets and moons surface temperatures comparison.

The presence of atmosphere doesn't  warm Earth's surface.

It is the other reasons, not the presence of atmosphere, that make Earth warmer than the Moon by +68°C.

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Key words:

Specular Reflection

Φ - Solar Irradiation Accepting Factor (spherical shape and surface roughness coefficient), for smooth bodies Φ = 0,47 and for rough / porous Φ = 1

Immediate IR Emission

Rotational Warming Phenomenon ( N*cp )^1/16

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Comments

Yes, and thank you. So once L cools to planet H temperature, it continues to emit more radiation, even when it is cooler.

IR emission = σTΛ4.
Planet LTday =200K, LTnight =100K
To balance the same energy in = out
Planet HTnight grows higher (100+7,5) K, than HTday goes down (200-1) K.
So the HTmean > LTmean
Thanks ask

Important - Rough example:

LTday>HTday
LTday - HTday = 20 oC

But
HTnight - LTnight = 50 oC

So HTmean>LTmean

Thanks

Important topic H on average is always warmer than L because L lit surface emits more intense24/7
For L Tmean=(Tnight+Tday)/2
For H the Tnight↑↑→T↑mean ←T↓day
(Tnight↑↑+T↓day)/2>(Tnight+Tday)/2 Thanks

Once the warmer planet L emitted adequet radiation to reach the same T as planet H, would not any further emissions then be equal?

Yes, and thank you. Just trying to understand. I should have specified planet L as sunlight side being warmer. Can you be more specific as to your answer. Once planet L cools to planet H temperatur

Table of contents - Links

0). Explain Rotational Warming Model.

Demonstrate the Initial PREMISE, Links: (1) and (2)

1). The first steps.

2). The Initial PREMISE.

3).The Planetary Temperatures Comparison Criteria.

4). "The total amount of the specularly reflected portion of solar flux"

Link: Φ = 0,47 and FRESNEL

5). How A Planet Retains The Solar Energy - the role of the Immediate IR emission.

6). Φ -Factor is an analogue of the well known Drag Coefficient Cd=0,47

7). “What ‘portion’ of ‘sunlight’ reaches surface of Earth?”

8). The satellites do not measure Bond Albedo.

9). Stefan-Boltzmann formula J = σ T⁴ W/m² doesn't apply to terrestrial temperatures.

10). The Theoretical Equation.

11). The First Conclusions.

12). The actual reason of the observed Global Warming.

13). The Axial Precession's role in Global Warming.

14). The Original Milankovitch cycle.

15). The Reversed Milankovitch cycle.

16). The higher CO2 content in ice core samples relates to colder periods.

17). Sensible Heat /Latent Heat ratio.

18). The conventional greenhouses, and the role of immediate IR emission.

19). NASA Technical Memorandum An Earth Albedo Model

20). The yearly total Immediate IR Emitted solar energy - in our times - is lower.

21). The yearly total reflected solar energy - in our times - is lower.

Appendix - Links

1). Earth's Corrected Effective Temperature (210 K ) calculation.

2). Earth's Average Surface Temperature (288 K ) calculation.

3). Moon's Corrected Effective Temperature (224 K ) calculation.

4). Moon's Average Surface Temperature (220 K ) calculation.

5). Mars' Corrected Effective Temperature (174 K ) calculation.

6). Mars' Average Surface Temperature (210 K ) calculation.

7). Mercury's Corrected Effective Temperature (364 K ) calculation.

8). Mercury's Average Surface Temperature (340 K ) calculation.

9). Titan's Average Surface Temperature (93,7 K ) calculation.

10). Earth / Mars satellite measured mean surface temperatures 288 K and 210 K comparison.

11). Earth's /Moon's temps 288K /220K comparison.

12). Completed DeepSearch.

13). Blog.

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The table of contents will be completed some time soon. For more pages view the menu at the top.

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