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Class Notes Weather is the condition of the atmosphere at certain time and place. Weather depends a lot on the amount of water in the air. Therefore, to understand weather, you need to understand the water cycle When the water vapor cools, it may change back into a liquid and form clouds. This is called condensation. The liquid water may fall as rain, snow, sleet, or hail on the land and this is known as Precipitation. THE WATER CYCLE The movement of water between the atmosphere, the land, and the oceans is called the water cycle. The amount of water vapor in the air is called humidity. Warmer air can hold more water vapor than cooler air can. A psychrometer is an instrument that is used to measure humidity. Relative humidity is the ratio of the amount of water vapor in the air to the greatest amount the air can hold. What Is Dew Point? What happens when relative humidity reaches 100%? At this point, the air is saturated with water vapor. The temperature at which this happens is the dew point. At temperatures below the dew point, liquid water droplets can form from the water vapor in the air. A cloud is a group of millions of tiny water droplets or ice crystals. Clouds form as air rises and cools. When air cools below the dew point, water droplets or ice crystals form. Water droplets form when water condenses. Three types of clouds: 1. Cumulus Clouds they tend to have flat bottoms they indicate fair weather . When these clouds get larger, they produce thunderstorms. 2. Stratus Clouds they are clouds that forms in layers. They cover large areas of the sky and often block the sun. 3. Cirrus Clouds they are thin, feathery, white clouds found at high altitudes. They form when winds are strong and they get thicker which indicates that a change in weather is coming. 4. Nimbus clouds are rain clouds. Cumulonimbus are thunderstorm clouds. Water in the air can return to Earth’s surface through precipitation. Precipitation is solid or liquid water that falls to Earth’s surface from clouds. Precipitation is rain, snow, sleet, or hail that falls from clouds to Earth’s surface. An air mass is a very large volume of air that has a certain temperature and moisture content. There are many types of air masses, each of which is associated with a particular source region. Maritime (m) forms over water; wet. Continental (c) forms over land; dry. Polar (P) forms over the polar regions; cold. Tropical (t) develops over the tropics; warm mT – wet and warm; mP – wet and cold; cT – dry and warm; cP – dry and cold The place where two or more air masses meet is called a front. A cold front forms when a cold air mass moves under a warm air mass. It brings thunderstorms, heavy rains or snow. A warm front forms when a warm air mass moves in over a cold air mass that is leaving an area. The warm air replaces the cold air. It brings drizzly rain followed by clear warm weather An occluded front forms when a warm air mass is caught between two colder air masses. Cool temperatures and large amounts of rain. A stationary front forms when a cold air mass and a warm air mass move toward each other. It brings many days of cloudy, wet weather A cyclone is an area of the atmosphere that has lower pressure than the surrounding air. The air in the cyclone rises. As the air rises, it cools. Clouds can form and may cause rainy or stormy weather. An anticyclone is an area of the atmosphere that has higher pressure than the surrounding air. Air in anticyclones sinks and gets warmer. Its relative humidity decreases. This warm, sinking air can bring dry, clear weather. Cyclones and anticyclones can affect each.