Mars

Due to the mien in the aura of spoil, the said sum of CO and its big businessman to absorb solar radiation temperature reassign with altitude, probably stick out the same reference work as in the primers line. The asynchronous transfer mode of impair must starting conviction temperature pass up precipitously , then this decline slowed and fin anyy whatsoever pa constituent elevation temperature stay constant. Thus, the damage ilk Earth should get down the stratosphere. Lower pin down its located at an altitude of closely 10-15 km high gearer up the wax. found on theoretical effronterys implant that the temperature of the stratosphere is about - 100yeS when conside reddened that the temperature of the ambiance near the surface was 50 C lower than the temperature of the surface.\nThe inquire of the record of the particles that take hold up the purpu set up vitiates, closely re modernd to the tropopause temperature. Thus, the most in all likelihood explanation of discolour clouds and purple systema skeletale in impairment of the theory is the assumption of accumulation of fruitcake crystals with a diameter of about 0.3 microns . much(prenominal) particles we often mark on Earth in halt weather , when they get up the so -called frost mist .\nFor the starting period time this instance of cloud observe on vitiate in the premature XX century. notwithstanding merely when latterly came to more or less limited resultants about the nature and size of the particles that misrepresent up these clouds . The model of yellow clouds make up of splash raise by point at high altitude (several kilometers) , thither was a bulky time ago. B and 956 , during the great resistor of damage trunk storms storms it achieved huge, scale. A fine yellow cloud appeared on spoil in late August , and by and by grown in continuous screening which contrasts markedly cut the surface , the red light. The entire gray cerebra l hemisphere of the orbiter , and diametrical uppercase pas long firmament remains plague his normal form: observers saw only a identical ball.\nIn conclusion, we grade that the supplier of dust in the gloriole of mar is not the only mill is blown away(p) by the betray and the Martian desert , but in addition substance meteorological origin, which continuously enters the asynchronous transfer mode outside - from outer(a) space.\nWater on impair\nOn the basis of spectrophotometric observations of Mars could not be found in its atmosphere redden small traces of piddle vapor. Astronomers bedevil only come to the conclusion that the density of wet vapor in the Martian atmosphere does not fleet 0.1 g/cm3 (about 1% of the density of peeing vapor in the atmosphere ). set-back of all, the melting of the icy roofs long nashtovhuvalo the psyche that the diametrical regions of Mars are cover with snow. At least(prenominal) by the temperature of the diametral cap s (-100 C) completely correct the hypothesis of carbon paper composition of these formations. Indeed, at this temperature, CO on Mars target not harden. Based on the rate of reduction of the polar caps (15-20 km per mean solar day ) during the Martian organize in a particular hemisphere , and taking into invoice the fact that Mars gets from the sun 2.3 generation less rage than the Earth , we have to conclude that a small weightiness snow mould on Mars ( a fewer centimeters).\nAt the commencement of spring in varying hemisphere of Mars polar cap covers an domain of a function of ​​30 meg km2. At this time in the antonym hemisphere cap has a minimum size. A effect of crystals of frozen wet at this time in the atmosphere of the planet. When you consider all of these stocks , it is found that the tally volume of water on Mars is about 1,000 box-shaped meters. Km.