The dry air flowing along the central dense overcast descends at the periphery and the eye region. Most soundings taken within the eye show a low-level layer, which is relatively moist, with an inversion above suggesting that the sinking in the eye, Another feature of tropical cyclones that probably plays a role in. These cyclones start with a westward movement, but turn northwards around 20 latitude. Space is filled with fresh moisture-laden air. The ascending air will lose moisture at some point and descends (subsides) back to the surface through the calm regions (descending limbs of convection cell subsiding air) that exist between two rain bands. The cloud size decreases from center to periphery. As a result, they rarely form within 5 of the equator. As divergence prevails on the eastern side of the troughs, a rising motion occurs; this leads to the development of thunderstorms. Hurricanes are steered by global winds. . The space is filled by fresh moisture laden air. Tropical waves form in the easterly flow along the equatorial . Meteorologists believe the. Temperature contrasts between these air masses must exist when the. Cyclonic disturbances are rapid weather systems, which include weather depressions, deep depressions, and tropical cyclones (of severe, very severe, extremely severe, and super cyclonic storms depending on their intensity). The reason why tropical cyclones often follow the direction from West [sic] to East [sic] is b/c tropical cyclones do not often follow the direction from west to east. Had it been Anti-clockwise in Northern Hemisphere, it would have been correct. . Remote sensing by radars, aircraft and satellites helps predict where exactly the cyclone is going to strike. High-velocity winds cause most of the damage associated with these weather events. Between 1891 and 2000, 48 tropical cyclones impacted the west coast, of which 24 were severe cyclonic storms, while about 308 cyclones, including 103 severe cyclonic storms, impacted the east coast of the country from the Bay of Bengal. As divergence prevails on the eastern side of the troughs, a rising motion occurs; this leads to the development of thunderstorms. Low-level disturbance (thunderstorms they are the seeds of cyclones) in the form of easterly wave disturbances in the Inter-Tropical Convergence Zone (ITCZ) should pre-exist. ; They are irregular wind movements involving closed circulation of air around a low pressure center. The 7517 km coastal area of India is hit by over 10 percent of the world's tropical cyclones year on year. Subsidence is distributed over a wide area on the outside of the rain band but is concentrated in the small inside area. 3 Why tropical cyclones form mostly on the western margins of . It helps in taking advance steps in the following areas: provision of shelter with sanitation facilities (safety homes). Rain bands are mostly made up of cumulonimbus clouds. At these locations, the strong local convectional currents acquire a whirling motion because of the Coriolis force. Yet another inquiry we ran across in our research was Why do tropical cyclones form on the west coast?. The remains of an upper tropospheric cyclone from the Westerlies move deep into the tropical latitude regions. When do tropical storms begin to lose energy? After developing, these cyclones advance till they find a weak spot in the trade wind belt. The above condition occurs only in western tropical oceans because of warm ocean currents (easterly trade winds push ocean waters towards the west) that flow from the east towards the west forming a thick layer of water with temperatures greater than 27C. Advertisement The faster-moving cold front closes in on the warm front, decreasing the size of the warm sector. The dense overcast at the upper levels of troposphere is due to. All the wind that is carried upwards loses its moisture and becomes cold and dense. First of all thanku so much for providing such an amazing materials for geography optional. These are ferocious storms that originate over oceans in tropical areas and move over to the coastal areas causing violent winds, very heavy rainfall, and storm outpourings. Tropical cyclone is like a heat engine . Under favorable conditions, multiple thunderstorms originate over the oceans. Moving air is deflected by the rotation of the Earth. The air from surroundings rushes in and undergoes deflection due to, Due to centripetal acceleration (centripetal force pulling towards the center is countered by an opposing force called the centrifugal force), the air in the vortex is forced to form a region of calmness called an. Clockwise in the southern hemisphere and counter clockwise in the northern hemisphere. Hurricane Irma may be getting most of the headlines right now, but its sharing the Atlantic, The water vapour it carries condenses and forms cumulonimbus clouds. Polar cyclones are cyclones that occur in polar regions like Greenland, Siberia and Antarctica. In the temperate regions, wind shear is high due to westerlies and this inhibits convective cyclone formation. The average number of tropical storms per, There are 3 hurricanes in the Atlantic right now. Why do Atlantic hurricanes move East to West? Subscribe to our newsletter and never miss an important update !! Write about the steps that you will take. Thus, the convergence of these air masses of different temperatures and the resulting instability are the prerequisites for the origin and growth of violent tropical storms. If you purchase the notes with Download Validity == 2 Years, on 17/01/2023, then you will be able to download the Static Files + Current Affairs files till 18/01/2025. Also called typhoons, tropical cyclones generally have been moving westward by about 18 miles per decade (30 kilometers) since 1982, putting them closer to land and making them more dangerous, a study in Thursday's journal Science said. If the storm front is directed northwards, the center moves towards the north, but after two or three days, the pressure difference declines and the cyclone dissipates. must-have You are doing amazing work. They are irregular wind movements involvingthe closed circulationof air around a low-pressure center. Today, it is possible to detect a cyclone right from its genesis in the high seas and follow its course, giving a warning at least 48 hours prior to a cyclone strike. Reasons for the Emergence of the Tropical Cyclone Structure of the Tropical Cyclone The atmospheric pressure causes air to travel from a high-pressure to a low-pressure state, causing the air to move. They carry hurricanes and other tropical storms from east to west. The Coriolis force explains why winds circulate around high and low pressure systems as opposed to blowing in the direction of the pressure gradient. Warm air rises quickly. - The post-monsoon period sees a higher number of cyclones than the pre-monsoon period. Reasons why the western coast sees fewer cyclones than . In India, there are detection radars along both the coasts. All the wind that is carried upwards loses its moisture and becomes cold and dense. Types of Cyclone. Large sea surface with temperature higher than. Tropical cyclones are violent storms that originate over oceans in tropical areas and move over to the coastal areas bringing about large scale . Eyes range in size from 8 km to over 200 km across, but most are approximately 30-60 km in diameter. These can lead to the formation of a tropical cyclone. These are low pressure weather systems in which winds equal or exceed speeds of 62kmph. A tropical cyclone is a weather phenomenon that is essentially a rapidly rotating storm system with characteristics such as a low-pressure center, strong winds, and thunderstorms that produce heavy rain, among others. #kt-info-box_fd7786-59 .kt-blocks-info-box-link-wrap{border-radius:10px;background:#ffffff;padding-top:5px;padding-right:6px;padding-bottom:5px;padding-left:6px;margin-top:1px;margin-right:0px;margin-bottom:0px;margin-left:0px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;}#kt-info-box_fd7786-59 .kt-blocks-info-box-link-wrap:hover{border-color:#eeeeee;background:#f1f3ef;}#kt-info-box_fd7786-59 .kadence-info-box-image-inner-intrisic-container{max-width:30px;}#kt-info-box_fd7786-59 .kadence-info-box-image-inner-intrisic-container .kadence-info-box-image-intrisic{padding-bottom:100%;width:512px;height:0px;max-width:100%;}#kt-info-box_fd7786-59 .kt-info-svg-icon, #kt-info-box_fd7786-59 .kt-info-svg-icon-flip, #kt-info-box_fd7786-59 .kt-blocks-info-box-number{font-size:50px;}#kt-info-box_fd7786-59 .kt-blocks-info-box-media{color:#444444;background:#ffffff;border-color:#eeeeee;border-radius:200px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:10px;margin-top:0px;margin-right:20px;margin-bottom:0px;margin-left:0px;}#kt-info-box_fd7786-59 .kt-blocks-info-box-media .kadence-info-box-image-intrisic:not(.kb-info-box-image-ratio) img{border-radius:200px;}#kt-info-box_fd7786-59 .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-media{color:#444444;background:#ffffff;border-color:#eeeeee;}#kt-info-box_fd7786-59 .kt-blocks-info-box-title{color:#4f4e4e;font-size:15px;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:0px;margin-top:5px;margin-right:0px;margin-bottom:10px;margin-left:0px;}#kt-info-box_fd7786-59 .kt-blocks-info-box-learnmore{background:transparent;border-color:#555555;border-width:0px 0px 0px 0px;padding:4px 8px 4px 8px;margin:10px 0px 10px 0px;}#kt-info-box_fd7786-59 .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-learnmore{color:#ffffff;background:#444444;border-color:#444444;} Primary References:NCERT Geography, IMD,Encyclopedia Britannica[Images],Spectrums Geography [Amazon and Flipkart] and Savindra Singh[Amazon and Flipkart]. After developing, these cyclones advance till they find a weak spot in the trade wind belt. As climate change triggered tropical cyclones are on the rise in coastal India, the unplanned development adds to the vulnerability of these cities. This blocks the rise of air from the water, and the subsequent formation of clouds . There are three divisions in the vertical structure of tropical cyclones. Current Affairs of 2021 & earlier are available for free on PMF IAS Google Drive Folder. Temperate cyclones can be formed on both land and sea, A tropical cyclone doesnt last for more than 7 days, Temperate cyclone can last for a duration of 15 to 20 days. Two factors explain why hurricanes very rarely form and come close to land on the west coast. Because of the pressure falls on the inside, the tangential winds around the tropical cyclone increase due to increased pressure gradient. Cyclones originate in the Bay of Bengal region as well as in the Arabian Sea region whereas Tornadoes of weak strength occur in the north-western and north-eastern region of the country causing significant damage to man and material. Subscribe to our newsletter and never miss an important update! Tropical cyclones are regarded as one of the most devastating natural calamities in the world. provision of shelter with sanitation facilities (safety homes). The wind velocity may range from nil to 1200 km per hour. These waves travel in east to west direction at the rate at 32-48 kms per day. Tropical cyclones across the globe, except Atlantic hurricanes, are moving closer to land in recent decades, a new study found. This is because summers and pre-monsoons see dry and hot air moving from north-western India towards the Bay. The Tropical Cyclones are violent storms that originate over oceans in tropical areas and move over to coastal areas bringing about large-scale destruction caused by violent winds, very heavy rainfall and storm surges. A pre-existing weak low-pressure area or low-level-cyclonic circulation. The maximum outflow is found at 12 km and above. This closed air circulation (whirling motion) is a result ofrapid upward movement of the hot airwhich is subjected toCoriolis force. Tropical Cyclones Tropical cyclones are regarded as one of the most devastating natural calamities in the world. Low-level disturbance (thunderstorms they are the seeds of cyclones) in the form of easterly wave disturbances in the Inter-Tropical Convergence Zone (ITCZ) should pre-exist. Presence of the Coriolis force enough to create a cyclonic vortex. The normal motion is called direct motion, while the backwards motion is called retrograde motion. The explanation is v good. Under normal circumstances, the red planet appears to move to the East (upwards in the gif below), but when its being overtaken by the Earth, our faster motion makes Mars appear to be going backwards (downwards in the gif below). An analysis of the frequencies of the cyclones suggests that during the period 1891-2000, nearly 308 tropical cyclones crossed the east coast, of which 103 were severe in intensity. A cyclone is an atmospheric system of rapidly circulating air massed about a low-pressure centre, usually accompanied by stormy often destructive weather. What is the relationship between the temperature of seawater and cyclones? The eye is surrounded by the eye wall, the roughly circular ring of, The eye is composed of air that is slowly sinking and the eye wall has a net upward flow as a result of many moderate occasionally strong . #kt-info-box_2611e5-91 .kt-blocks-info-box-link-wrap{border-radius:10px;background:#ffffff;padding-top:5px;padding-right:6px;padding-bottom:5px;padding-left:6px;margin-top:1px;margin-right:0px;margin-bottom:0px;margin-left:0px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;}#kt-info-box_2611e5-91 .kt-blocks-info-box-link-wrap:hover{border-color:#eeeeee;background:#f1f3ef;}#kt-info-box_2611e5-91 .kadence-info-box-image-inner-intrisic-container{max-width:30px;}#kt-info-box_2611e5-91 .kadence-info-box-image-inner-intrisic-container .kadence-info-box-image-intrisic{padding-bottom:100%;width:512px;height:0px;max-width:100%;}#kt-info-box_2611e5-91 .kt-info-svg-icon, #kt-info-box_2611e5-91 .kt-info-svg-icon-flip, #kt-info-box_2611e5-91 .kt-blocks-info-box-number{font-size:50px;}#kt-info-box_2611e5-91 .kt-blocks-info-box-media{color:#444444;background:#ffffff;border-color:#eeeeee;border-radius:200px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:10px;margin-top:0px;margin-right:20px;margin-bottom:0px;margin-left:0px;}#kt-info-box_2611e5-91 .kt-blocks-info-box-media .kadence-info-box-image-intrisic:not(.kb-info-box-image-ratio) img{border-radius:200px;}#kt-info-box_2611e5-91 .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-media{color:#444444;background:#ffffff;border-color:#eeeeee;}#kt-info-box_2611e5-91 .kt-blocks-info-box-title{color:#4f4e4e;font-size:15px;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:0px;margin-top:5px;margin-right:0px;margin-bottom:10px;margin-left:0px;}#kt-info-box_2611e5-91 .kt-blocks-info-box-learnmore{background:transparent;border-color:#555555;border-width:0px 0px 0px 0px;padding:4px 8px 4px 8px;margin:10px 0px 10px 0px;}#kt-info-box_2611e5-91 .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-learnmore{color:#ffffff;background:#444444;border-color:#444444;} May The dense overcast at the upper levels of the troposphere is due to. It is in a cold core (non-tropical cyclone) can also spread far away from the center of the storm. Cyclones have intense low pressure areas and pressure increases outwards. 5: theory: India: CLIMATE Tropical cyclones are the violent storms that originate over oceans in the tropical areas and move over to the coastal areas bringing about large-scale destruction that is caused by violent winds, heavy rainfall and storm surges. The cloud size decreases from center to periphery. Cyclones occur in the pre-monsoon months of May-June and the post-monsoon months of October-November. As the tropical cyclone transfers energy from the ocean into the atmosphere, the ocean cools. Air in the tropics generally moves in the direction of the equator. This warm water lies well within the belt of easterly winds, so almost all the storms that form there move away from the coast, toward the west. Subsidence is distributed over a wide area on the outside of the rain band but is concentrated in the small inside area. Since these cyclones move with the westerlies (Jet Streams), they are oriented eastwest. An inverted trough (an elongated area of relatively low pressure) or cyclonic curvature maximum moving east to west across the tropics. https://youtu.be/tVQVVZJtUOw. Where do tropical storms form in the world. These winds, called trade winds, blow from east to west in the tropics. This can and does happen because the currents arent stationary. In the thunderstorm, air is uplifted as it is. Canada reports the second largest number of tornadoes. There are three divisions in the vertical structure of tropical cyclones. It becomes a . There has been an increase in tropical storms and hurricanes from the previous 30-year record NOAA announced Friday. High humidity (around 50 to 60 per cent) is required in the mid-troposphere, since the presence of moist air leads to the formation of, Such conditions exist over the equatorial. UPSC CDS 1 2023 Syllabus and Latest Exam Pattern IMA INA OTA AFA 1 hour ago; Gulab Resurrects as Cyclone Shaheen over Arabian Sea A hurricane is a tropical cyclone that has maximum sustained surface winds of 74 mph or greater (64 knots or greater). A tropical cyclone is characterized by lack of warm/cold fronts attached, a "warm core" (air is . Tropical Cyclone. A few storms recurve right next to the coast. Around south-east African coast and Madagascar-Mauritius islands. #kt-info-box_e33a87-d2 .kt-blocks-info-box-link-wrap{border-color:#ffefd9;border-radius:8px;background:var(--global-palette8, #F7FAFC);padding-top:5px;padding-right:5px;padding-bottom:5px;padding-left:5px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;}#kt-info-box_e33a87-d2 .kt-blocks-info-box-link-wrap:hover{border-color:#eeeeee;background:#ffefd9;}#kt-info-box_e33a87-d2 .kadence-info-box-image-inner-intrisic-container{max-width:40px;}#kt-info-box_e33a87-d2 .kadence-info-box-image-inner-intrisic-container .kadence-info-box-image-intrisic{padding-bottom:100%;width:512px;height:0px;max-width:100%;}#kt-info-box_e33a87-d2 .kt-info-svg-icon, #kt-info-box_e33a87-d2 .kt-info-svg-icon-flip, #kt-info-box_e33a87-d2 .kt-blocks-info-box-number{font-size:50px;}#kt-info-box_e33a87-d2 .kt-blocks-info-box-media{color:#444444;background:transparent;border-color:#444444;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;padding-top:10px;padding-right:10px;padding-bottom:10px;padding-left:10px;}#kt-info-box_e33a87-d2 .kt-blocks-info-box-media-container{margin-top:0px;margin-right:15px;margin-bottom:0px;margin-left:15px;}#kt-info-box_e33a87-d2 .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-media{color:#444444;background:transparent;border-color:#444444;}#kt-info-box_e33a87-d2 .kt-blocks-info-box-title{color:#363636;font-size:14px;margin-top:7px;margin-right:3px;margin-bottom:12px;margin-left:3px;}#kt-info-box_e33a87-d2 .kt-blocks-info-box-learnmore{background:transparent;border-color:#555555;border-width:0px 0px 0px 0px;padding:4px 8px 4px 8px;margin:10px 0px 10px 0px;}#kt-info-box_e33a87-d2 .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-learnmore{color:#ffffff;background:#444444;border-color:#444444;} #kt-info-box_115628-3c .kt-blocks-info-box-link-wrap{border-radius:10px;background:#ffffff;padding-top:5px;padding-right:6px;padding-bottom:5px;padding-left:6px;margin-top:1px;margin-right:0px;margin-bottom:0px;margin-left:0px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;}#kt-info-box_115628-3c .kt-blocks-info-box-link-wrap:hover{border-color:#eeeeee;background:#f1f3ef;}#kt-info-box_115628-3c .kadence-info-box-image-inner-intrisic-container{max-width:30px;}#kt-info-box_115628-3c .kadence-info-box-image-inner-intrisic-container .kadence-info-box-image-intrisic{padding-bottom:100%;width:300px;height:0px;max-width:100%;}#kt-info-box_115628-3c .kt-info-svg-icon, #kt-info-box_115628-3c .kt-info-svg-icon-flip, #kt-info-box_115628-3c .kt-blocks-info-box-number{font-size:50px;}#kt-info-box_115628-3c .kt-blocks-info-box-media{color:#444444;background:#ffffff;border-color:#eeeeee;border-radius:200px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:10px;margin-top:0px;margin-right:20px;margin-bottom:0px;margin-left:0px;}#kt-info-box_115628-3c .kt-blocks-info-box-media .kadence-info-box-image-intrisic:not(.kb-info-box-image-ratio) img{border-radius:200px;}#kt-info-box_115628-3c .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-media{color:#444444;background:#ffffff;border-color:#eeeeee;}#kt-info-box_115628-3c .kt-blocks-info-box-title{color:#4f4e4e;font-size:15px;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:0px;margin-top:5px;margin-right:0px;margin-bottom:10px;margin-left:0px;}#kt-info-box_115628-3c .kt-blocks-info-box-learnmore{background:transparent;border-color:#555555;border-width:0px 0px 0px 0px;padding:4px 8px 4px 8px;margin:10px 0px 10px 0px;}#kt-info-box_115628-3c .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-learnmore{color:#ffffff;background:#444444;border-color:#444444;} Cloud formation is dense at the center. Structure of the answer: Introduction: In brief, mention the facts of the case. 2. 2 Years Validity == Validity of the Download links (both Static & Current Affairs) is 2 Years from the date of purchase. A They are irregular wind movements involving closed circulation of air around a low pressure center. The eye is a roughly circular area of comparatively. The regions with cumulonimbus cloud (rising limbs of the convective cell) formation are called. Small variations in the vertical wind speed. A tropical cyclone turns into a typhoon in the western Pacificnear Asiawhen it has winds of 74 MPH or greater. The dry air flowing along the central dense overcast descends at the periphery and the eye region. In the northern hemisphere, the deflection is to the right (seen with the wind in the back) and in southern hemisphere, it . Thus. Why Bay of Bengal is the hot-bed for cyclonic storms Cyclones in the Bay of Bengal can be attributed to the vast low pressure created by the warm water of the ocean. A generic term for tropical depressions, tropical storms, and hurricanes. The condensation of moisture releases enough. par | Mai 29, 2022 | at present, the members of the family hominidae include | fulton county property search qpublic | Mai 29, 2022 | at present, the members of the family hominidae include | fulton county property search qpublic Eventually, the band moves toward the center and encircles it, and the. (Specific question wrt confusing options in prelims). In the Atlantic, storms are carried by the trade winds from the coast of Africa where they typically form westward to the Caribbean and North American coasts. Squall a sudden violent gust of wind or localized storm, especially one bringing rain, snow, or sleet. Tropical cyclones are violent storms that originate over oceans in tropical areas and move over to the coastal areas bringing about large scale destruction due to violent winds (squalls), very heavy rainfall (torrential rainfall) and storm surge. HOW CAN I DOWNLOAD PDF? Due to excess moisture over oceans, the thunderstorm intensifies and sucks in air at much faster rate. A category 5 cyclone, on the other hand, is extremely dangerous and has the potential for major damage. Storms generally move east to west because of trade winds in the tropics, so a greater westward shift usually puts them closer to where the land is, Wang said. How are the tropical cyclones named across the world? Western Disturbance: It is an extratropical storm originating in the Mediterranean region that brings sudden winter rain to the north-western parts of the Indian sub-continent. Hurricanes are found in the Atlantic and Northeast Pacific, whereas typhoons . Winds 40-300+ mph. The wind velocity in a tropical cyclone is much higher and it is more destructive. An analysis of the frequency of cyclones on the east and west coasts of India between 1891 and 1990 shows that nearly 262 cyclones occurred on the east coast and 33 cyclones occurred on the west coast during this period. Whereas the tropical cyclones originate only over the seas and on reaching the land they dissipate. Why do temperate cyclones move from west to east? Actually, the term hurricane is used only for the large storms that form over the Atlantic Ocean or eastern Pacific Ocean. Temperate cyclone affect a much larger area. Due to excess moisture over oceans, the thunderstorm intensifies and sucks in the air at a much faster rate. The condensation of moisture releases enough. This is because tropical cyclones develop over warm sea waters and follow trade winds that blow westward. (This is why hurricanes hit the east coast of the United States.). Also known as an easterly wave. Buy it NOW! Tropical cyclones, hurricanes or typhoons form when convection causes warm, moist air above the ocean to rise. Detection of any unusual phenomena in the weather leading to cyclones has three main parameters: There are a network of weather stations monitoring pressure fall and wind velocities in all countries of the world, including the Arctic and Antarctic regions. It is essentially a vast cell of low-pressure air, with ground-level pressure in the center typically between 990 and 1000 millibars. #kt-info-box_76677b-cb .kt-blocks-info-box-link-wrap{border-radius:10px;background:#ffffff;padding-top:5px;padding-right:6px;padding-bottom:5px;padding-left:6px;margin-top:1px;margin-right:0px;margin-bottom:0px;margin-left:0px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;}#kt-info-box_76677b-cb .kt-blocks-info-box-link-wrap:hover{border-color:#eeeeee;background:#f1f3ef;}#kt-info-box_76677b-cb .kadence-info-box-image-inner-intrisic-container{max-width:30px;}#kt-info-box_76677b-cb .kadence-info-box-image-inner-intrisic-container .kadence-info-box-image-intrisic{padding-bottom:100%;width:512px;height:0px;max-width:100%;}#kt-info-box_76677b-cb .kt-blocks-info-box-media .kt-info-box-image{width:30px;height:auto;}#kt-info-box_76677b-cb .kt-blocks-info-box-media .kt-info-box-image, #kt-info-box_76677b-cb .kt-blocks-info-box-media .kt-info-box-image path{fill:#444444;}#kt-info-box_76677b-cb .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-media .kt-info-box-image, #kt-info-box_76677b-cb .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-media .kt-info-box-image path{fill:#444444;}#kt-info-box_76677b-cb .kt-info-svg-icon, #kt-info-box_76677b-cb .kt-info-svg-icon-flip, #kt-info-box_76677b-cb .kt-blocks-info-box-number{font-size:50px;}#kt-info-box_76677b-cb .kt-blocks-info-box-media{color:#444444;background:#ffffff;border-color:#eeeeee;border-radius:200px;border-top-width:0px;border-right-width:0px;border-bottom-width:0px;border-left-width:0px;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:10px;margin-top:0px;margin-right:20px;margin-bottom:0px;margin-left:0px;}#kt-info-box_76677b-cb .kt-blocks-info-box-media .kadence-info-box-image-intrisic:not(.kb-info-box-image-ratio) img{border-radius:200px;}#kt-info-box_76677b-cb .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-media{color:#444444;background:#ffffff;border-color:#eeeeee;}#kt-info-box_76677b-cb .kt-blocks-info-box-title{color:#4f4e4e;font-size:15px;padding-top:0px;padding-right:0px;padding-bottom:0px;padding-left:0px;margin-top:5px;margin-right:0px;margin-bottom:10px;margin-left:0px;}#kt-info-box_76677b-cb .kt-blocks-info-box-learnmore{background:transparent;border-color:#555555;border-width:0px 0px 0px 0px;padding:4px 8px 4px 8px;margin:10px 0px 10px 0px;}#kt-info-box_76677b-cb .kt-blocks-info-box-link-wrap:hover .kt-blocks-info-box-learnmore{color:#ffffff;background:#444444;border-color:#444444;} Condensation occurs in this air and the cycle is repeated as long as the moisture is supplied. 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