polar low वाक्य
उदाहरण वाक्य
मोबाइल
- When extremely cold air moves over relatively warm oceans, polar lows can develop.
- It is able to lift approximately into a circular polar low-Earth orbit.
- Polar lows are a second special class of MCS which form at high latitudes during the cold season.
- Mesoscale cyclones known as polar lows can form along the arctic front in the wake of extratropical cyclones.
- Polar lows are a second special class of MCS . They form at high latitudes during the cold season.
- A polar low developing in the English Channel brought fronts of snow over southern England before moving south and dissipating.
- Mesocyclones, tornadoes, hurricanes / typhoons / tropical cyclones, Extratropical cyclones, and polar lows are all cyclones.
- It was able to lift approximately 3, 000 kg ( 7, 500 lb ) into a polar low-Earth circular orbit.
- Although it had the structure of a tropical cyclone, it occurred over water temperatures, suggesting it could have been a polar low.
- They are fueled by a different heat mechanism than other cyclonic windstorms such as nor'easters, European windstorms, and polar lows.
- Imaging was performed with film cameras and television surveillance from polar low Earth orbits with film canisters returning via capsule and parachute with mid-air retrieval.
- On May 27, the remnants of Tropical Depression 26F were absorbed by a large polar low, that was located to the south of the remnants.
- Large polar lows push up through the Indian Ocean directing long range, high period swell from as far south as Heard Island from late March through to September or later.
- A persistent pattern of cold northerly and easterly winds brought cold, moist air to the United Kingdom with many snow showers, fronts and polar lows bringing snowy weather with it.
- During winter, when cold-core lows with temperatures in the mid-levels of the troposphere reach move over open waters, deep convection forms which allows polar low development to become possible.
- The prolonged life of medicanes and similarity to polar lows is caused primarily by origins as synoptic-scale surface lows and heat-related instability . coinciding with a decrease in previously high lightning activity as well.
- Mediterranean cyclones have been compared to polar lows cyclonic storms which typically develop in the far regions of the Northern and Southern Hemispheres for their similarly small size and heat-related instability; however, while medicanes nearly always feature warm-core lows, polar lows are primarily cold-core.
- A mesoscale convective system's overall cloud and precipitation pattern may be round or linear in shape, and include weather systems such as tropical cyclones, squall lines, lake-effect snow events, polar lows, and Mesoscale Convective Complexes ( MCCs ), and they generally form near weather fronts.
- This diverged water moves northward ( equatorward ), and at the same time persistent precipitation ( location is near the polar lows ~ 60�S ) along with an influx of melt water decreases the salinity of the original NADW . Because the salinity of the NADW has changed by so much and it has essentially lost all its unique characteristics to be NADW, this northward propagating surface water is now called Antarctic Surface Water ( AASW ).
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