smitha,a+2

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**Rain is liquid precipitation that reaches the surface in the form of drops that are greater than 0.5 millimeters in diameter. The intensity of rain is determined by the accumulation over a given time. Categories of rain are light, moderate and heavy.**


 * [[image:http://t0.gstatic.com/images?q=tbn:vQNQt4SYnVH1fM:http://www.photohowto.info/files/images/story/2008/04/108/Image1_Snow_Mountains.jpg width="150" height="113" link="http://images.google.com/imgres?imgurl=http://www.photohowto.info/files/images/story/2008/04/108/Image1_Snow_Mountains.jpg&imgrefurl=http://www.photohowto.info/how-take-photos-snow&usg=__n9OevhPBTMZENgKpyk-d8s7Gios=&h=768&w=1024&sz=322&hl=en&start=50&tbnid=vQNQt4SYnVH1fM:&tbnh=113&tbnw=150&prev=/images%3Fq%3Dsnow%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D36"]] [[image:http://t3.gstatic.com/images?q=tbn:EAxrfqzEt2th3M:http://www.richbrenner.com/gallery/d/95-2/Snow.jpg width="137" height="91" link="http://images.google.com/imgres?imgurl=http://www.richbrenner.com/gallery/d/95-2/Snow.jpg&imgrefurl=http://www.richbrenner.com/gallery/v/upclose/&usg=__UOhzS65JrgHWLMiDSbCz8VP_UVE=&h=427&w=640&sz=123&hl=en&start=71&tbnid=EAxrfqzEt2th3M:&tbnh=91&tbnw=137&prev=/images%3Fq%3Dsnow%2Bup%2Bclose%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D54"]] [[image:http://t1.gstatic.com/images?q=tbn:3s6FR77Vqn5OIM:http://www.robertwstarkey.com/images/paintings/winter/large/Snow%2520Stream,%2520(close-up%25201).jpg width="149" height="112" link="http://images.google.com/imgres?imgurl=http://www.robertwstarkey.com/images/paintings/winter/large/Snow%2520Stream,%2520(close-up%25201).jpg&imgrefurl=http://www.robertwstarkey.com/winter_2.htm&usg=__YgWjvbs7mULT_SbRl9twqiptYdA=&h=750&w=1000&sz=272&hl=en&start=179&tbnid=3s6FR77Vqn5OIM:&tbnh=112&tbnw=149&prev=/images%3Fq%3Dsnow%2Bup%2Bclose%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D162"]] [[image:http://t1.gstatic.com/images?q=tbn:N6Bh8JK7EibXzM:http://www.robertwstarkey.com/images/paintings/winter/large/Midnight%2520Snow,%2520(close-up%25201)%2520Winter.JPG width="149" height="63" link="http://images.google.com/imgres?imgurl=http://www.robertwstarkey.com/images/paintings/winter/large/Midnight%2520Snow,%2520(close-up%25201)%2520Winter.JPG&imgrefurl=http://www.robertwstarkey.com/winter_1.htm&usg=__i3XVpyPxFyTv0YtROOtXA-zs2n8=&h=425&w=1000&sz=116&hl=en&start=195&tbnid=N6Bh8JK7EibXzM:&tbnh=63&tbnw=149&prev=/images%3Fq%3Dsnow%2Bup%2Bclose%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D180"]]

Snow is an aggregate of ice crystals that form into flakes. Snow forms at temperatures below freezing. For snow to reach the earth's surface the entire temperature profile in the troposphere needs to be at or below freezing. It can be slightly above freezing in some layers if the layer is not warm or deep enough the melt the snow flakes much. The intensity of snow is determined by the accumulation over a given time. Categories of snow are light, moderate and heavy. **


 * [[image:http://t2.gstatic.com/images?q=tbn:UV7-B3ptojF2BM:http://media-2.web.britannica.com/eb-media/67/123867-004-B8C2F31F.jpg width="133" height="100" link="http://images.google.com/imgres?imgurl=http://media-2.web.britannica.com/eb-media/67/123867-004-B8C2F31F.jpg&imgrefurl=http://www.britannica.com/EBchecked/topic-art/548629/118052/Sleet-on-the-ground&usg=__f9VL3q9xXZkpSj6BHauYSGZrVEo=&h=413&w=550&sz=43&hl=en&start=25&tbnid=UV7-B3ptojF2BM:&tbnh=100&tbnw=133&prev=/images%3Fq%3Dsleet%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D18"]] [[image:http://t1.gstatic.com/images?q=tbn:TZ7BCqxcQxti0M:http://www.zianet.com/msaxton/TX/arcticblast07/sleet9-15Am.JPG width="131" height="98" link="http://images.google.com/imgres?imgurl=http://www.zianet.com/msaxton/TX/arcticblast07/sleet9-15Am.JPG&imgrefurl=http://www.zianet.com/msaxton/TX/arcticblast07/index.html&usg=__z8h8FvIGMbT55WBdgc5BoodmwQA=&h=384&w=512&sz=119&hl=en&start=3&tbnid=TZ7BCqxcQxti0M:&tbnh=98&tbnw=131&prev=/images%3Fq%3Dsleet%26gbv%3D2%26hl%3Den"]] [[image:http://t2.gstatic.com/images?q=tbn:JNJCpfGUcL_mTM:http://image24.webshots.com/25/7/53/83/287075383YnWMMx_ph.jpg width="136" height="125" link="http://images.google.com/imgres?imgurl=http://image24.webshots.com/25/7/53/83/287075383YnWMMx_ph.jpg&imgrefurl=http://outdoors.webshots.com/photo/1287075383026337972YnWMMx&usg=__s5xkTweKfZbmYbNO4VwGTnUOiHQ=&h=562&w=613&sz=42&hl=en&start=51&tbnid=JNJCpfGUcL_mTM:&tbnh=125&tbnw=136&prev=/images%3Fq%3Dsleet%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D36"]] [[image:http://t1.gstatic.com/images?q=tbn:3SS54Oa8nCofUM:http://img.chinaa2z.com/uploadpic/news/2009/20090114/20090114095225949876/1231898000.jpg width="130" height="86" link="http://images.google.com/imgres?imgurl=http://img.chinaa2z.com/uploadpic/news/2009/20090114/20090114095225949876/1231898000.jpg&imgrefurl=http://news.chinaa2z.com/news/html/2009/20090114/20090114095225949876/20090114095337183210.html&usg=__xHgpGlnF8txS71dfAKCBNTgOndY=&h=332&w=500&sz=63&hl=en&start=66&tbnid=3SS54Oa8nCofUM:&tbnh=86&tbnw=130&prev=/images%3Fq%3Dsleet%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D54"]]

Sleet (Ice Pellets) are frozen raindrops that strike the earth's surface. In a sleet situation the precipitation aloft when it is first generated will be snow. The snow falls through a layer that is a little above freezing and the snow partially melts. If the snow completely melts it will be more likely to reach the earth's surface as supercooled water instead of sleet. If the snow partially melts there will still be ice within the falling drop for water to freeze on when the drop falls into a subfreezing layer. The lowest layer of the troposphere will be below freezing in a sleet situation and deep enough to freeze drops completely. The lower boundary layer can be above freezing and sleet occur if the sleet does not have time to melt before reaching the surface. **


 * [[image:http://t3.gstatic.com/images?q=tbn:ARxP24_G2AcYBM:http://justinsomnia.org/images/san-francisco-hail-2.jpg width="123" height="92" link="http://images.google.com/imgres?imgurl=http://justinsomnia.org/images/san-francisco-hail-2.jpg&imgrefurl=http://justinsomnia.org/2007/02/hail-attacks-san-francisco/&usg=__MNGFoBnZ8cMkWBksS6s3j8j__4s=&h=285&w=380&sz=65&hl=en&start=7&tbnid=ARxP24_G2AcYBM:&tbnh=92&tbnw=123&prev=/images%3Fq%3Dhail%26gbv%3D2%26hl%3Den"]] [[image:http://t2.gstatic.com/images?q=tbn:7wA637DggwTnOM:http://pasc.met.psu.edu/PA_Climatologist/extreme/Hail/hail%2520damage.bmp width="142" height="90" link="http://images.google.com/imgres?imgurl=http://pasc.met.psu.edu/PA_Climatologist/extreme/Hail/hail%2520damage.bmp&imgrefurl=http://pasc.met.psu.edu/PA_Climatologist/extreme/Hail/PEMA_hail.html&usg=__ii0p9PX0n9gHx4gA1e5FfMnABSo=&h=488&w=770&sz=1102&hl=en&start=2&tbnid=7wA637DggwTnOM:&tbnh=90&tbnw=142&prev=/images%3Fq%3Dhail%26gbv%3D2%26hl%3Den"]] [[image:http://t0.gstatic.com/images?q=tbn:NGXY3NgQYelUQM:http://blogs.warwick.ac.uk/images/jjaiston/2006/06/12/hail.jpg width="143" height="107" link="http://images.google.com/imgres?imgurl=http://blogs.warwick.ac.uk/images/jjaiston/2006/06/12/hail.jpg&imgrefurl=http://blogs.warwick.ac.uk/jjaiston/entry/wow&usg=__MRQIgEdt84c_eMERnDqVTvp_JHw=&h=600&w=800&sz=129&hl=en&start=22&tbnid=NGXY3NgQYelUQM:&tbnh=107&tbnw=143&prev=/images%3Fq%3Dhail%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D18"]] [[image:http://t0.gstatic.com/images?q=tbn:UWjcxPrvV5Eh0M:http://nimg.sulekha.com/Business/original700/hail-edmond-oklahoma-tornado-2009-2-10-21-4-12.jpg width="106" height="129" link="http://images.google.com/imgres?imgurl=http://nimg.sulekha.com/Business/original700/hail-edmond-oklahoma-tornado-2009-2-10-21-4-12.jpg&imgrefurl=http://newshopper.sulekha.com/topic/slideshow/industries/667850.htm&usg=__qzt5NCvltwF4b209Ndj2PiCEWEk=&h=480&w=394&sz=38&hl=en&start=34&tbnid=UWjcxPrvV5Eh0M:&tbnh=129&tbnw=106&prev=/images%3Fq%3Dhail%26gbv%3D2%26ndsp%3D18%26hl%3Den%26sa%3DN%26start%3D18"]]

Hail is dense precipitation ice that is that least 5 millimeters in diameter. It forms due to ice crystals and supercooled water that freeze or stick to the embryo hail stone. Soft hail is more white and less dense since it has air bubbles. Soft hail occurs when hail grows at a temperature below freezing by ice crystals and small supercooled water and cloud droplets merging onto the hail. Hard hail occurs when liquid water drops freeze on the outer edges of the hailstone after the outer edge is above freezing. The freezing of supercooled water releases latent heat and this can result in the outer edge of the hail stone warming above freezing. Then the water refreezes creating solid ice. Hail will commonly have soft ice and hard ice layers when it is sliced open. **