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A wind blowing from east to west is called a westerly wind.
The water in the western Pacific is typically warmer than in the eastern Pacific because trade winds blow the warm waters of the eastern Pacific westward and keep it there. Also, upwelling in the eastern Pacific keeps the water cooler.The warmer water creates more clouds and rain, keeping Indonesia and other areas of the western Pacific wetter than Peru and other coastal regions of South America.During El Niño, the pressure gradient (rate of pressure change between areas of high and low pressure) weakens. In the western tropical Pacific, there is unusually high air pressure, while there is unusually low air pressure in the eastern tropical Pacific. This Southern Oscillation causes the trade winds to weaken, and even blow backwards. This pattern reversal leads to unusually wet weather in parts of South America, and unusually dry weather in the western Pacific.El Nino usually occurs every 3 to 7 years, and lasts for about 18 months.La Niña is the opposite of El Niño. These two weather patterns oscillate every few years.During La Niña, there is unusually low air pressure over the western tropical Pacific, and unusually high air pressure in the eastern tropical Pacific. The easterly blowing trade winds strengthen, blowing more warm water away from the equatorial Pacific. As a result, Australia and Indonesia become wetter than normal, and parts of South America become drier than normal.
Cyclones are most often formed in the tropical areas, 5° and 20° north and south of the equator, owing to the Coriolis effect. Initially, a low pressure zone is formed in this area, which eventually forms a tropical wave of low pressure. This disturbance in the warm ocean waters, along with a light wind at the upper level, provides ideal weather condition for the formation of storms. With time, the intensity of the tropical wave may either increase or decrease. If the intensity increases, it goes on to become an organized area, characterized by heavy showers and thunderstorms. This organized area, marked by cyclonic winds blowing clockwise in northern hemisphere and anti-clockwise in southern hemisphere, is referred to as tropical depression. Equatorial areas, 5° north and south of the equator, do not facilitate formation of storms due to the lack of rotary motion of wind in this area.
Increase air flow = increased oxygen flow = increase in burn temperature and rate.
Winds blowing east to west or west to east are referred to as zonal winds
A wind blowing from east to west is called a westerly wind.
An easterly wind is a wind coming from the east. So, if you're feeling a breeze on your face and it's coming from the direction of the rising sun, you've got yourself an easterly wind. Just remember, it's all about perspective, darling.
An easterly breeze is a wind that blows from the east towards the west. It is commonly associated with cooler temperatures and is often observed in coastal areas. Easterly breezes can be influenced by various factors such as local terrain and weather systems.
when the sun is clear then there will be a slight wind blowing toward you it depends where you are and if you are in the north area.
"Jet stream is a swiftly blowing wind at a height of 3 to 5 kms above the subtropical high pressure belt. Himalayas act as a barrier in their path and as such, the jet streams are divided into westerly and easterly jet steams. the westerly jet is responsible for bringing western disturbances into north-west India and Pakistan which bring winter rainfall. the easterly jet blowing over northern India is responsible for bringing tropical depressions over India and Bangladesh. these depressions play an important role in the distribution of rainfall." source: icse geo textbook
The water in the western Pacific is typically warmer than in the eastern Pacific because trade winds blow the warm waters of the eastern Pacific westward and keep it there. Also, upwelling in the eastern Pacific keeps the water cooler.The warmer water creates more clouds and rain, keeping Indonesia and other areas of the western Pacific wetter than Peru and other coastal regions of South America.During El Niño, the pressure gradient (rate of pressure change between areas of high and low pressure) weakens. In the western tropical Pacific, there is unusually high air pressure, while there is unusually low air pressure in the eastern tropical Pacific. This Southern Oscillation causes the trade winds to weaken, and even blow backwards. This pattern reversal leads to unusually wet weather in parts of South America, and unusually dry weather in the western Pacific.El Nino usually occurs every 3 to 7 years, and lasts for about 18 months.La Niña is the opposite of El Niño. These two weather patterns oscillate every few years.During La Niña, there is unusually low air pressure over the western tropical Pacific, and unusually high air pressure in the eastern tropical Pacific. The easterly blowing trade winds strengthen, blowing more warm water away from the equatorial Pacific. As a result, Australia and Indonesia become wetter than normal, and parts of South America become drier than normal.
The leaves would blow in a north-easterly direction.
Trade winds are nearly constant easterly winds that blow towards the equator. The westerly's on the other hand, are winds blowing from the west. which are in the the mid-latitudes of the northern and southern hemispheres.
Wind direction is reported from the direction it is coming from.. if wind is blowing toward the northwest, this is said to be a south easterly wind direction and so on. hope that helps
Cyclones are most often formed in the tropical areas, 5° and 20° north and south of the equator, owing to the Coriolis effect. Initially, a low pressure zone is formed in this area, which eventually forms a tropical wave of low pressure. This disturbance in the warm ocean waters, along with a light wind at the upper level, provides ideal weather condition for the formation of storms. With time, the intensity of the tropical wave may either increase or decrease. If the intensity increases, it goes on to become an organized area, characterized by heavy showers and thunderstorms. This organized area, marked by cyclonic winds blowing clockwise in northern hemisphere and anti-clockwise in southern hemisphere, is referred to as tropical depression. Equatorial areas, 5° north and south of the equator, do not facilitate formation of storms due to the lack of rotary motion of wind in this area.
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Blowing up a balloon can temporarily increase blood pressure because it requires a sustained increase in intrathoracic pressure, which can affect blood flow and heart function. However, this effect is usually short-lived and not a significant factor in affecting overall blood pressure.