The Moon / Brad Guth
This is not another effort at discrediting others, so much as it's about doing what's right with exploiting our complex mineral and raw element treasure-trove moon.
Obviously we don't have to do a damn thing about managing tidal surges, seismic issues or figuring out where our moon ever came from in the first place, as I'm certain there were any number of random happenstance events taking place at the time and especially prior to our planet getting its seasonal tilt, another ocean basin, the antipode of Antarctica and having acquired the moon kinda all at once.
Monday, June 24, 2013
Tuesday, June 18, 2013
Guth Venus / GuthVenus
GuthVenus
Focus yourself within a 10% area, situated one third up, roughly center:
-->http://docs.google.com/View?id=ddsdxhv_0hrm5bdfj
Indeed Venus is a hot planet, though not as entirely heated from the outside, but instead from the inside out.
Those extremely reflective clouds are not only thick and robust and obviously somewhat acidic, as well as getting cryogenic (worse than icy) cold above 60 km and especially getting extra cryogenic by way of their unavoidable season of nighttime, but they otherwise do tend to insulate whatever geothermal plus the little amount of solar energy that gets through, which is actually quite minimal compared to the all-inclusive 20.5 watts/m2 of global energy escaping, whereas the solar contributed factor of surface heating could be as little as a fourth or roughly an average of 5 watts/m2 because, the daytime surface simply doesn't get all that much illumination (a few percent) of the solar 2650 w/m2 spectrum to work with, and most of that cloud filtered influx isn't IR.
In other words, the vast bulk of solar energy gets reflected, and much of whatever continues inward is getting recycled within the thick layers of those clouds that continually recirculate solar energy in much the same fashion as our oceans recirculate and transport solar energy. Most of the incoming recirculation of IR energy gets moderated or diverted by the S8 layer acting somewhat like a personal protection fire blanket, below which are those mostly CO2 acidic clouds and finally a 5~10 km depth as a layer of mist or fog area of semitransparent atmosphere. Below the acidic fog and mist of micro-droplets that never reach the surface, is where the mostly buoyant and otherwise clear atmosphere as dominated by CO2 is relatively calm and basically inert, though getting hotter as you approach the active surface where that atmosphere is continually replenished and where most of the heat is coming from.
Focus yourself within a 10% area, situated one third up, roughly center:
-->http://docs.google.com/View?id=ddsdxhv_0hrm5bdfj
Indeed Venus is a hot planet, though not as entirely heated from the outside, but instead from the inside out.
Those extremely reflective clouds are not only thick and robust and obviously somewhat acidic, as well as getting cryogenic (worse than icy) cold above 60 km and especially getting extra cryogenic by way of their unavoidable season of nighttime, but they otherwise do tend to insulate whatever geothermal plus the little amount of solar energy that gets through, which is actually quite minimal compared to the all-inclusive 20.5 watts/m2 of global energy escaping, whereas the solar contributed factor of surface heating could be as little as a fourth or roughly an average of 5 watts/m2 because, the daytime surface simply doesn't get all that much illumination (a few percent) of the solar 2650 w/m2 spectrum to work with, and most of that cloud filtered influx isn't IR.
In other words, the vast bulk of solar energy gets reflected, and much of whatever continues inward is getting recycled within the thick layers of those clouds that continually recirculate solar energy in much the same fashion as our oceans recirculate and transport solar energy. Most of the incoming recirculation of IR energy gets moderated or diverted by the S8 layer acting somewhat like a personal protection fire blanket, below which are those mostly CO2 acidic clouds and finally a 5~10 km depth as a layer of mist or fog area of semitransparent atmosphere. Below the acidic fog and mist of micro-droplets that never reach the surface, is where the mostly buoyant and otherwise clear atmosphere as dominated by CO2 is relatively calm and basically inert, though getting hotter as you approach the active surface where that atmosphere is continually replenished and where most of the heat is coming from.
Just a standard 10X view of GuthVenus
The small image is extracted as a direct derivative from the GIF format of the Magellan archived image, as obtained from just one of many official radar obtained images.
If you can't identify anything unusual in this image, then the good news is that you automatically qualify for state and federal benefits for the blind/disabled.
Of course you can always go to the original image that's offering those blocky pixel resolutions of 225 meters, and not bother to enlarge/zoom-in with anything capable of delivering the best quality image, which is actually what I did at first and used such large resolution pixels in order to estimate the relative size of items.
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