616228 | 2023-07-195120 x 3290 | 6458.2 KbDownloads: 0|2|500
616212 | 2023-07-155120 x 3415 | 4975.2 KbDownloads: 1|3|532
616205 | 2023-07-156144 x 4096 | 6828.2 KbDownloads: 2|0|813
616202 | 2023-07-135120 x 3414 | 4766.9 KbDownloads: 1|1|935
616182 | 2023-07-106144 x 4096 | 8935.2 KbDownloads: 1|3|751
616172 | 2023-07-093871 x 2582 | 3420.4 KbDownloads: 1|4|788
616159 | 2023-07-075120 x 3417 | 5007.5 KbDownloads: 1|1|849
616144 | 2023-07-045120 x 3414 | 4980.1 Kb | 2|0|776
616124 | 2023-07-015120 x 3413 | 3316.4 KbDownloads: 0|5|553
616106 | 2023-06-305120 x 3417 | 5857.5 KbDownloads: 1|1|881
616098 | 2023-06-295120 x 3413 | 5687.7 KbDownloads: 0|2|1313
616094 | 2023-06-295120 x 3413 | 5837.4 KbDownloads: 0|2|774
616083 | 2023-06-275120 x 3200 | 7833.4 KbDownloads: 1|4|1167
616068 | 2023-06-195120 x 3415 | 4976.9 KbDownloads: 1|2|603
616066 | 2023-06-193840 x 2560 | 3286.3 KbDownloads: 0|3|1742
616063 | 2023-06-183840 x 2560 | 5083.7 KbDownloads: 0|8|1018
616062 | 2023-06-186144 x 4098 | 5748.2 KbDownloads: 0|4|987
616038 | 2023-06-153840 x 2560 | 3448.6 Kb | 1|2|772
616008 | 2023-06-125120 x 3413 | 5282.7 Kb | 0|0|661
615965 | 2023-06-086144 x 4096 | 7392.8 KbDownloads: 0|1|645
615959 | 2023-06-085120 x 3280 | 5735.6 KbDownloads: 3|4|711
615951 | 2023-06-075120 x 3413 | 4172.9 Kb | 0|2|909
615896 | 2023-06-023840 x 2555 | 3743.3 KbDownloads: 0|5|680
615891 | 2023-06-023840 x 2555 | 4259.2 KbDownloads: 0|2|546
615846 | 2023-05-295120 x 3413 | 4625.5 Kb | 0|2|777
615845 | 2023-05-293840 x 2297 | 4319.4 KbDownloads: 1|0|635
615843 | 2023-05-283840 x 2563 | 4198.3 KbDownloads: 0|1|883
615820 | 2023-05-265120 x 3201 | 5814.6 KbDownloads: 0|1|701
615770 | 2023-05-113840 x 2561 | 3924.4 KbDownloads: 2|2|448
615756 | 2023-05-105120 x 3417 | 5992.4 Kb | 2|4|1099
In meteorology, a cloud is an aerosol comprising a visible mass of minute liquid droplets, frozen crystals, or particles suspended in the atmosphere above the surface of a planetary body.[1] The droplets and crystals may be made of water or various chemicals. On Earth, clouds are formed as a result of saturation of the air when it is cooled to its dew point, or when it gains sufficient moisture (usually in the form of water vapor) from an adjacent source to raise the dew point to the ambient temperature. They are seen in the Earth's homosphere (which includes the troposphere, stratosphere, and mesosphere). Nephology is the science of clouds which is undertaken in the cloud physics branch of meteorology.
2017-05-28See the
Wikipedia page for more information.
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