Tropical cyclones, also known as hurricanes or typhoons, are large storm systems that form over warm tropical oceans and are characterized by strong winds that spiral inward toward the eye of the storm. They develop when warm, moist air rises and condenses, releasing latent heat that powers the storm. Tropical cyclones strengthen over warm ocean waters due to evaporation that fuels thunderstorms and heavy rain. They weaken rapidly when moving over land away from their heat source. Major tropical cyclone basins are monitored by regional warning centers that track storms and issue advisories.
This document discusses hurricanes, including their structure, formation, and naming conventions. It notes that hurricanes are a type of tropical cyclone that forms over warm ocean waters and features heavy rains and strong winds that spiral inward. The document outlines the typical stages of a hurricane's life cycle from formation to maturity to decay. It also describes the vertical structure of hurricanes and notes key factors like sea surface temperature that enable their development. Finally, the document indicates that meteorological organizations name hurricanes to identify and track them, classifying storms on scales of intensity.
this is a presentation of cyclone.in this ppt, various types of cyclones are given.its effects, formation, different names, types, emergency response on cyclone is given
Midlatitude cyclones are large low pressure storm systems that form in the midlatitudes. They develop as warm and cold air masses converge, forming fronts where the air masses meet. As the cyclone moves eastward, the cold front typically advances faster than the storm itself and eventually catches up to the warm front. Meteograms are charts that plot changes in weather conditions over time and can clearly show the passing of fronts and associated changes in temperature, wind, precipitation and other conditions.
This document summarizes different types of natural and man-made disasters. It describes natural disasters such as tornadoes, lightning, earthquakes, cyclones, and tsunamis. It provides details on the causes and characteristics of each type of natural disaster. The document also summarizes some common man-made disasters including war, viruses, factory waste, bacteria, and crime. It briefly explains each type of man-made disaster and its impacts.
WATER RESOURCES ENGINEERING MODULE 1 NOTESReshmaMRaju
This document provides an overview of key concepts in hydrology and water resources engineering. It discusses the hydrologic cycle and its three main processes of evaporation, precipitation, and runoff. It describes different types of precipitation including cyclonic, convective, and orographic precipitation. Measurement of rainfall using rain gauges is also summarized, including factors to consider for the optimal number of rain gauges. Methods for estimating missing precipitation data from nearby rain gauges are outlined, such as the arithmetic mean method, normal ratio method, and inverse distance method.
Cyclones form due to rising warm air that cools and condenses to form clouds. If the air starts spinning horizontally over tropical oceans, it can develop into a tropical depression, storm, and eventually a hurricane or typhoon depending on location and wind speeds. Cyclones cause heavy rainfall, landslides, damage to infrastructure and homes, disruption to ecosystems and agriculture, and harm to human and animal life. Coastal areas need to prepare shelters and strengthen infrastructure to mitigate cyclonic damage.
This document provides information about weather and climate as part of a science lesson. It begins with an opening prayer and introduces a lesson on weather phenomena through a game of identifying true and false statements. The main body of the document then defines and distinguishes between weather and climate. It describes different types of weather phenomena like blizzards, clouds, and heat waves. It also outlines five main climate classification types according to the Koppen system. The document aims to educate students on key concepts and terminology related to meteorology.
Tropical cyclones, also known as hurricanes or typhoons, are large storm systems that form over warm tropical oceans and are characterized by strong winds that spiral inward toward the eye of the storm. They develop when warm, moist air rises and condenses, releasing latent heat that powers the storm. Tropical cyclones strengthen over warm ocean waters due to evaporation that fuels thunderstorms and heavy rain. They weaken rapidly when moving over land away from their heat source. Major tropical cyclone basins are monitored by regional warning centers that track storms and issue advisories.
This document discusses hurricanes, including their structure, formation, and naming conventions. It notes that hurricanes are a type of tropical cyclone that forms over warm ocean waters and features heavy rains and strong winds that spiral inward. The document outlines the typical stages of a hurricane's life cycle from formation to maturity to decay. It also describes the vertical structure of hurricanes and notes key factors like sea surface temperature that enable their development. Finally, the document indicates that meteorological organizations name hurricanes to identify and track them, classifying storms on scales of intensity.
this is a presentation of cyclone.in this ppt, various types of cyclones are given.its effects, formation, different names, types, emergency response on cyclone is given
Midlatitude cyclones are large low pressure storm systems that form in the midlatitudes. They develop as warm and cold air masses converge, forming fronts where the air masses meet. As the cyclone moves eastward, the cold front typically advances faster than the storm itself and eventually catches up to the warm front. Meteograms are charts that plot changes in weather conditions over time and can clearly show the passing of fronts and associated changes in temperature, wind, precipitation and other conditions.
This document summarizes different types of natural and man-made disasters. It describes natural disasters such as tornadoes, lightning, earthquakes, cyclones, and tsunamis. It provides details on the causes and characteristics of each type of natural disaster. The document also summarizes some common man-made disasters including war, viruses, factory waste, bacteria, and crime. It briefly explains each type of man-made disaster and its impacts.
WATER RESOURCES ENGINEERING MODULE 1 NOTESReshmaMRaju
This document provides an overview of key concepts in hydrology and water resources engineering. It discusses the hydrologic cycle and its three main processes of evaporation, precipitation, and runoff. It describes different types of precipitation including cyclonic, convective, and orographic precipitation. Measurement of rainfall using rain gauges is also summarized, including factors to consider for the optimal number of rain gauges. Methods for estimating missing precipitation data from nearby rain gauges are outlined, such as the arithmetic mean method, normal ratio method, and inverse distance method.
Cyclones form due to rising warm air that cools and condenses to form clouds. If the air starts spinning horizontally over tropical oceans, it can develop into a tropical depression, storm, and eventually a hurricane or typhoon depending on location and wind speeds. Cyclones cause heavy rainfall, landslides, damage to infrastructure and homes, disruption to ecosystems and agriculture, and harm to human and animal life. Coastal areas need to prepare shelters and strengthen infrastructure to mitigate cyclonic damage.
This document provides information about weather and climate as part of a science lesson. It begins with an opening prayer and introduces a lesson on weather phenomena through a game of identifying true and false statements. The main body of the document then defines and distinguishes between weather and climate. It describes different types of weather phenomena like blizzards, clouds, and heat waves. It also outlines five main climate classification types according to the Koppen system. The document aims to educate students on key concepts and terminology related to meteorology.
This document is a student project on winds, storms and cyclones. It contains sections that define and describe different types of winds like trade winds and monsoons. It also discusses natural disasters caused by severe weather like floods, earthquakes and tsunamis. Sections are included on air pressure, wind speed, how air expands when heated, wind currents and thunderstorms. The document finishes with descriptions of cyclones, tornadoes and precautions to take during severe storms.
The document provides instructions for using a presentation on weather and climate. It includes how to view slides, advance to the next slide, access different sections from the chapter screen, and exit the slideshow. The presentation covers topics like the water cycle, air masses, fronts, severe weather, and weather forecasting. It contains objectives, lessons, visual concepts, and standardized test preparation questions for each section.
This document defines hydro-meteorological hazards as natural phenomena involving atmospheric, hydrological, or oceanographic processes that can cause loss of life, property damage, economic disruption, or environmental degradation. It provides three examples of hydro-meteorological hazards: floods, which can occur due to heavy rain overwhelming drainage systems; droughts, which are difficult to define but represent temporary climate aberrations; and cyclones, also known as tropical storms or hurricanes, which are intense low-pressure weather systems with winds over 62 kmph.
Cyclones and Tropical Cyclone class 7 social scienceTakshila Learning
A cyclone is a system of wind that moves rapidly inward with a low-pressure area in the middle In meteorology, it refers to a large mass. Know more about cyclones in detail
1. Eyewall replacement cycles occur naturally in intense hurricanes when an outer ring of thunderstorms forms and contracts inward, weakening the inner eyewall by reducing its moisture and momentum. This causes the storm to initially weaken before the outer eyewall replaces the inner one.
2. Project Stormfury in the 1960s aimed to artificially trigger this process by seeding storms, but it was later found that eyewall replacement can occur naturally due to hurricane dynamics.
3. Nearly half of all major hurricanes undergo at least one eyewall replacement cycle, during which the storm may fluctuate between categories before re-intensifying with a new eyewall.
1) Aerosols can both decrease and increase rainfall through their effects on cloud microphysics and radiation. They slow the conversion of cloud droplets to raindrops but can invigorate deep convective clouds under certain conditions.
2) Observational studies show that aerosols can completely suppress precipitation from shallow clouds but do not generally reduce rainfall amounts from all cloud types. Heavy aerosol loading has been observed to both suppress rainfall from tropical clouds and invigorate deep convective clouds with warm cloud bases.
3) The document proposes a conceptual model to explain how slowing droplet conversion through increased aerosols can enhance rainfall in deep convective clouds by increasing latent heat release and upward heat transport
Tropical Low Pressure Systems are intense low pressure systems with closed circulation also known as hurricanes, typhoons or cyclones. They form over warm ocean waters and have diameters between 200-650km. They contain an eye that is calm at the center surrounded by an eyewall with the strongest winds and thunderstorms. For a disturbance to develop into a full storm, it needs warm ocean waters, atmospheric disturbances, and conditions that allow the transfer of heat away from the storm.
Tropical Low Pressure Systems are intense low pressure systems with closed circulation also known as hurricanes, typhoons or cyclones. They form over warm ocean waters and have diameters between 200-650km. They contain an eye that is calm at the center surrounded by an eyewall with the strongest winds and thunderstorms. For a disturbance to develop into a full storm, it needs warm ocean waters, atmospheric disturbances, and conditions that allow the transfer of heat away from the storm.
This document discusses tropical cyclones and was prepared by a group consisting of 10 members. It defines a tropical cyclone as a rapidly rotating storm system characterized by low pressure, strong winds, and heavy rain from thunderstorms. Tropical cyclones can cause hazards like storm surge, flooding, winds, and tornadoes. The three main types are tropical depressions, tropical storms, and hurricanes. Tropical cyclones impact many areas around the world and cause loss of life and property damage, especially in coastal regions which experience strong winds, flooding, and storm surge.
The document discusses parameters for detecting tropical cyclones using satellite data in MATLAB. It analyzes water vapor density maps, infrared temperature images, and cloud patterns to identify potential cyclones. Water vapor density, temperature above 30 degrees, and circular cloud patterns larger than a threshold indicate a cyclone. Maps and images from different satellites are processed and segmented to isolate areas of interest exhibiting these parameters, helping detect cyclones in real time.
The document discusses various weather and climate concepts including:
- Weather is the current atmospheric conditions while climate is the average weather over time.
- High pressure systems are associated with clear skies and dry conditions while low pressure systems bring clouds and rain.
- Weather maps use lines of equal pressure (isobars) and symbols to show wind speed and direction helping predict future conditions.
Climate Extreme (extreme weather or climate event) refers to the occurrence of a value of a weather or climate variable above (or below) a threshold value near the upper (or lower) ends of the range of observed values of the variable. Extreme weather and climate events, interacting with exposed and vulnerable human and natural systems, can lead to disasters.
The document discusses the differences between weather and climate. Weather refers to short-term atmospheric conditions including temperature, precipitation, and humidity that are observed each day and can vary significantly in different locations. Climate describes the average weather patterns over many years in a particular region and influences the typical weather experienced there. Factors like latitude, terrain, proximity to bodies of water, and altitude all impact a region's climate.
Weather cells and weather systems of atmosphereSunil Kumar
Jet streams are fast moving air currents in the upper atmosphere. They were first discovered in the 1920s and knowledge of them increased during World War II. There are two main types: polar and subtropical jet streams. Weather features like storms can form when air rises due to low pressure caused by jet streaks. Other weather systems discussed include air masses, frontal systems like cold fronts and warm fronts, mid-latitude cyclones, thunderstorms, tornadoes, and hurricanes.
Cyclones are areas of closed, circular winds rotating in the same direction as the Earth. They form over low pressure systems and can exist on scales from mesocyclones to extra tropical cyclones. Cyclones develop in tropical regions like northern Australia and Southeast Asia between the months of summer, requiring sea surface temperatures of at least 26°C. Cyclones are responsible for loss of life and property damage within 100km of their centers, mainly through strong winds, heavy rainfall, storm surges and tornadoes.
There are two main types of cyclones: tropical cyclones and temperate cyclones. Tropical cyclones form in tropical regions between the Tropics of Cancer and Capricorn, originating from warm, moist air masses. Temperate cyclones, also known as extra-tropical cyclones, form in temperate regions between 30-60 degrees latitude due to the convergence of warm and cold air masses along fronts. Some key differences are that tropical cyclones are smaller in size but more intense, with stronger winds near the surface, while temperate cyclones are larger but less severe, with strongest winds at higher elevations.
Cyclones are intense rotating storms that form over bodies of water. They are classified as either extra tropical or tropical cyclones. Tropical cyclones develop over tropical oceans and organize into a surface-level wind circulation. Cyclones form through a process where air rises and causes winds to rotate faster, forming a large swirling storm. Cyclones can cause damage through strong winds, heavy rain, power outages, injury and loss of life, and destruction of crops and vegetation. Preparation and mitigation efforts are important to reduce risks from cyclones.
1. Cyclones are large rotating storm systems that form over warm ocean waters and bring powerful winds, heavy rain, and storm surges. They include hurricanes, typhoons, and tropical storms.
2. Cyclones originate from warm ocean waters that evaporate water vapor into the atmosphere, which condenses and releases heat to power the storm as it rotates due to the Coriolis effect.
3. Cyclones can cause devastating damage from their strong winds, heavy rainfall, and storm surges. Advanced warning and tracking systems help prepare communities for cyclones and mitigate their impacts.
1) Cyclones form due to low atmospheric pressure and spiral inward in a counterclockwise direction in the Northern Hemisphere. They are known as hurricanes, typhoons, or cyclones depending on the region.
2) Cyclones form from either cold or warm cores and consist of a northern and southern hemisphere surrounding a low pressure center.
3) Major factors for cyclone disasters include human-caused climate change, destruction of coastal barriers, and poverty exacerbating storm impacts.
Advanced control scheme of doubly fed induction generator for wind turbine us...IJECEIAES
This paper describes a speed control device for generating electrical energy on an electricity network based on the doubly fed induction generator (DFIG) used for wind power conversion systems. At first, a double-fed induction generator model was constructed. A control law is formulated to govern the flow of energy between the stator of a DFIG and the energy network using three types of controllers: proportional integral (PI), sliding mode controller (SMC) and second order sliding mode controller (SOSMC). Their different results in terms of power reference tracking, reaction to unexpected speed fluctuations, sensitivity to perturbations, and resilience against machine parameter alterations are compared. MATLAB/Simulink was used to conduct the simulations for the preceding study. Multiple simulations have shown very satisfying results, and the investigations demonstrate the efficacy and power-enhancing capabilities of the suggested control system.
Redefining brain tumor segmentation: a cutting-edge convolutional neural netw...IJECEIAES
Medical image analysis has witnessed significant advancements with deep learning techniques. In the domain of brain tumor segmentation, the ability to
precisely delineate tumor boundaries from magnetic resonance imaging (MRI)
scans holds profound implications for diagnosis. This study presents an ensemble convolutional neural network (CNN) with transfer learning, integrating
the state-of-the-art Deeplabv3+ architecture with the ResNet18 backbone. The
model is rigorously trained and evaluated, exhibiting remarkable performance
metrics, including an impressive global accuracy of 99.286%, a high-class accuracy of 82.191%, a mean intersection over union (IoU) of 79.900%, a weighted
IoU of 98.620%, and a Boundary F1 (BF) score of 83.303%. Notably, a detailed comparative analysis with existing methods showcases the superiority of
our proposed model. These findings underscore the model’s competence in precise brain tumor localization, underscoring its potential to revolutionize medical
image analysis and enhance healthcare outcomes. This research paves the way
for future exploration and optimization of advanced CNN models in medical
imaging, emphasizing addressing false positives and resource efficiency.
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Tropical Low Pressure Systems are intense low pressure systems with closed circulation also known as hurricanes, typhoons or cyclones. They form over warm ocean waters and have diameters between 200-650km. They contain an eye that is calm at the center surrounded by an eyewall with the strongest winds and thunderstorms. For a disturbance to develop into a full storm, it needs warm ocean waters, atmospheric disturbances, and conditions that allow the transfer of heat away from the storm.
This document discusses tropical cyclones and was prepared by a group consisting of 10 members. It defines a tropical cyclone as a rapidly rotating storm system characterized by low pressure, strong winds, and heavy rain from thunderstorms. Tropical cyclones can cause hazards like storm surge, flooding, winds, and tornadoes. The three main types are tropical depressions, tropical storms, and hurricanes. Tropical cyclones impact many areas around the world and cause loss of life and property damage, especially in coastal regions which experience strong winds, flooding, and storm surge.
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- High pressure systems are associated with clear skies and dry conditions while low pressure systems bring clouds and rain.
- Weather maps use lines of equal pressure (isobars) and symbols to show wind speed and direction helping predict future conditions.
Climate Extreme (extreme weather or climate event) refers to the occurrence of a value of a weather or climate variable above (or below) a threshold value near the upper (or lower) ends of the range of observed values of the variable. Extreme weather and climate events, interacting with exposed and vulnerable human and natural systems, can lead to disasters.
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Cyclones are areas of closed, circular winds rotating in the same direction as the Earth. They form over low pressure systems and can exist on scales from mesocyclones to extra tropical cyclones. Cyclones develop in tropical regions like northern Australia and Southeast Asia between the months of summer, requiring sea surface temperatures of at least 26°C. Cyclones are responsible for loss of life and property damage within 100km of their centers, mainly through strong winds, heavy rainfall, storm surges and tornadoes.
There are two main types of cyclones: tropical cyclones and temperate cyclones. Tropical cyclones form in tropical regions between the Tropics of Cancer and Capricorn, originating from warm, moist air masses. Temperate cyclones, also known as extra-tropical cyclones, form in temperate regions between 30-60 degrees latitude due to the convergence of warm and cold air masses along fronts. Some key differences are that tropical cyclones are smaller in size but more intense, with stronger winds near the surface, while temperate cyclones are larger but less severe, with strongest winds at higher elevations.
Cyclones are intense rotating storms that form over bodies of water. They are classified as either extra tropical or tropical cyclones. Tropical cyclones develop over tropical oceans and organize into a surface-level wind circulation. Cyclones form through a process where air rises and causes winds to rotate faster, forming a large swirling storm. Cyclones can cause damage through strong winds, heavy rain, power outages, injury and loss of life, and destruction of crops and vegetation. Preparation and mitigation efforts are important to reduce risks from cyclones.
1. Cyclones are large rotating storm systems that form over warm ocean waters and bring powerful winds, heavy rain, and storm surges. They include hurricanes, typhoons, and tropical storms.
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1) Cyclones form due to low atmospheric pressure and spiral inward in a counterclockwise direction in the Northern Hemisphere. They are known as hurricanes, typhoons, or cyclones depending on the region.
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5. INTRODUCTION
Drought is a prolonged dry period in the natural climate
cycle that can occur anywhere in the world. It is a slow-
onset disaster characterized by the lack of precipitation,
resulting in a water shortage.
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9. INTRODUCTION
In meteorology, a cyclone is a large air mass that rotates
around a strong center of low atmospheric pressure,
counterclockwise in the Northern Hemisphere and
clockwise in the Southern Hemisphere as viewed from
above (opposite to an anticyclone).
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