11/16/11

StudyBlue printing of 11/16/11 html, body, div, span, applet, object, iframe, h1, h2, h3, h4, h5, h6, p, blockquote, pre, a, abbr, acronym, address, big, cite, code, del, dfn, em, font, img, ins, kbd, q, s, samp, small, strike, strong, sub, sup, tt, var, b, u, i, center, fieldset, form, label, legend, table, caption, tbody, tfoot, thead, tr, th, td { margin: 0; padding: 0; border: 0; outline: 0; font-size: 100%; background: transparent; } body { line-height: 1; } blockquote, q { quotes: none; } blockquote:before, blockquote:after, q:before, q:after { content: ''; content: none; } /* remember to define focus styles! */ :focus { outline: 0; } /* remember to highlight inserts somehow! */ ins { text-decoration: none; } del { text-decoration: line-through; } /* tables still need 'cellspacing="0"' in the markup */ table { border-collapse: collapse; border-spacing: 0; } /* end RESET */ .header { min-width:800px; } .logo { padding:6px 20px 2px 20px; margin:0; font-size:25px; font-weight:bold; color:#808285; position:relative; border-bottom: 1px solid #c5c5c5; } .logo-blue { color:#70adc4; } .logo-desc { font-weight:normal; font-size:19px; color:#cccccc; margin-top:50px; position:absolute; display: none; } .back-button { position:absolute; top:20px; right:20px; font-size:13px; line-height:25px; color:rgb(0,175,225); font-weight:normal; } .back-button a { color:rgb(0,175,225); } .instructions { padding:0; margin:0; width:100%; position:relative; color:rgb(100,100,100); } .step-holder { border-left:1px solid #ededed; margin-left:20px; } .steps { padding:15px 0; float:left; width:24%; border-right:1px solid #ededed; text-align:center; } .steps-01 { } .steps-02 { } .steps-03 { } .steps-04 { } .label { padding:5px 10px; } .print-button { } .print-button a { background-color:rgb(0,175,225); color:white; line-height: 19px; padding:9px 8px 5px 30px; font-size:14px; text-decoration:none; background-image: url(images/printer.png); background-repeat: no-repeat; background-position: 7px 50%; -moz-border-radius: 5px; -webkit-border-radius: 5px; } .print-button a:hover { background-color:black; } .theNote .content { width: 8.0in !important; margin: 5px auto; padding:20px; background-color:white; } .theNote .header { border-bottom: 1px dashed #C8C8C8; font-size: 17px; padding: 0 0 10px; line-height: 19px; color: #00ADE1; min-width:500px; } .theNote .body { font-size: 14px; line-height: 19px; padding: 10px 0; } .theNote{ padding:6px 0; clear:both; background-color: rgb(200,200,200); } .theNote h3{ color: rgb(100,100,100); } .theNote h1, .theNote h3{ background-color:white; padding:2px 20px; width:8.0in !important; margin: 0 auto; font-size: 15px; } .theNote h1{ padding-top: 10px; font-size: 15px; } .theNote h1:first-child{ font-size: 20px; } .theNote h3 { font-size: 14px; font-weight: normal; } #options { border: 3px double #ccc; padding: 5px 12px; margin: 10px 50px 10px 20px; float: left; } #info { border-top: 1px solid #ccc; padding-top: 5px; font-style: italic; } li { margin: 5px 10px 5px 25px; } ul li { list-style: disc; } ol li { list-style: decimal; } img { border: 0; } table { clear: both; width: 100%; border: 1px solid #c5c5c5; border-width: 1px 0; margin: 0; page-break-after: always; } table#page { page-break-after: auto; } td { text-align: center; font-size: 12px; border-bottom: 1px dashed #c5c5c5; height: 1.75in; width: 50%; padding-left: 15px; } .leftside { border-right: 1px solid #cccccc; padding: 0 15px 0 0; } .bottom td { border-bottom: none; } .clearfix { clear:both; line-height:1px; height:1px; } img { max-width:80%; max-height:150px; margin:20px; } @media print {.header { display: none; } .content .header{ display:inherit; } table { border: 1px dashed #bbb; border-width: 1px 0; } .theNote{ background-color:white; } } Hurricane Characteristics hurricanes, the most powerful of all storms, have sustained winds of 74 mph average diameters are about 350 mi and pressure averages about 950 mb but may be as low as 870 mb most energy that drives and sustains hurricanes is from latent heat of condensation as clouds form hurricanes form at the times of highest ocean temperatures for the N.H. august and september are the most common for hurricanes Hurricanes: Atlantic and eastern pacific tropical cyclones Typphoon: western pacific Cyclone: indian ocean and australia Hurricanes form between 5 and 20 degrees north or south over tropical oceans Hurricanes consist of: a central eye (clear skies) surrounded by an eye wall. the eye wall has the strongest winds and the heaviest precipitation up to 100 in./day low precipitation regions separate individual cloud bands start with a tropical storm (also known as a tropical depression) steep pressure gradient generates rapid, inward spiraling winds wind speed increase.... Core of the storm: air turns upward and ascends in a ring of cumulonimbus towers (eye wall) greatest wind speed, heaviest rainfall (up to 2500 ... .... Strong uplift... Conditions Necessary for Hurricane Formation Hurricanes form only over deep water layers with surface temperatures in excess of 80 degrees F energy is derived from latent heat release and associated evaporation of water (latitude above about 20 degrees, water temperatures are usually not warm enough) an unstable atmosphere is also necessary coriolis effect is needed to help form cyclonic circulation (between 0 and 5 degrees latitude not enough coriolis effect to start rotation) form in areas not affected by strong winds aloft or subtropical high pressure after forming, hurricanes are self propagating as long as they can get energy from warm ocean waters Formation of Hurricanes condensation: latent heat release Disturbance gets warmer air becomes less dense surface pressure drops cyclonic circulation pressure gradient gets steeper surface winds increase and bring additional moisture Hurricane Decay hurricanes need a constant supply of warm moist air hurricanes decay whenever they move over colder ocean currents move onto land reach a location where the airflow aloft is unfavorable Storm surge: sea water pushed inland by the strong winds associated with storms Wind Shear: large change in wind direction over a short distance