Mid-latitude cyclone What is a mid-latitude cyclone?
Solution containing material leached from a soil. Process in which water removes and transports soil humus and inorganic nutrients in solution. Leaf Drip The rain water that fall to the ground surface from plant leaves after it has been intercepted by these structures.
Lee Side of a slope that is opposite to the direction of flow of ice, wind, or water.
Downwind side of an elevated area like a mountain. Legume Angiosperm plant species that is a member of the Fabaceae Pea or Bean family. These plants form symbiotic relationships with specific bacteria species for the purpose of acquiring nitrogen for growth.
Less Developed Country LDC Country characterized by minimal industrialization, low technological development, low per capita income, and high population growth rates. Also see more developed country.
Levee Ridge of coarse deposits found alongside the stream channels and elevated above the floodplain. Forms from the deposition of sediment during floods.
Liana Species of plant that uses the support of wood plants to elevate its leaves above the forest canopy. Lichen Organism that consists of a symbiotic joining of a species of fungi and a species of algae. Light A humanly visible form of electromagnetic radiation.
This radiation has a wavelength between 0. Visible discharge of electricity created by thunderstorms. Light Year Distance that light travels in the vacuum of space in one year.
Also called brown coal. Limestone Sedimentary rock composed of carbonate minerals, especially calcium carbonate. Limestone can be created by clastic and non-clastic processes. Clastic limestones are formed from the break up and deposition of shells, coral and other marine organisms by wave-action and ocean currents.
Non-clastic limestones can be formed either as a precipitate or by the lithification of coral reefs, marine organism shells, or marine organism skeletons. Limiting Factor Abiotic condition that most controls the growth of a species.
For most terrestrial plants this condition is the supply of the nutrient nitrogen in the soil.An extratropical cyclone is a synoptic scale of low-pressure weather system that does not have tropical characteristics, as it is connected with fronts and horizontal gradients (rather than vertical) in temperature and dew point otherwise known as "baroclinic zones".
"Extratropical" is applied to cyclones outside the tropics, in the middle latitudes. These systems may also be described as "mid. Mid-latitude cyclone What is a mid-latitude cyclone?
|Caribbean, Puerto Rico, Gulf, Florida, Eastern US hurricane radar and satellite views||Introduction to the Atmosphere s. The Mid-Latitude Cyclone Introduction Mid-latitude or frontal cyclones are large traveling atmospheric cyclonic storms up to kilometers in diameter with centers of low atmospheric pressure.|
|Current Conditions and Forecast Maps||Melting The physical process of a solid becoming a liquid.|
- The mid-latitude cyclone is a synoptic scale low pressure system that has cyclonic (counter-clockwise in northern hemisphere) flow that is found in the middle latitudes (i.e., 30 ° N ° N).
Definitions 1. What is a tropical cyclone?
A tropical cyclone is defined as a non-frontal low pressure system of synoptic scale developing over warm waters having organised convection and a maximum mean wind speed of 34 knots or greater extending more than half-way around near the centre and persisting for at least six hours.
Lagoon (1) A body of seawater that is almost completely cut off from the ocean by a barrier beach. (2) The body of seawater that is enclosed by an atoll. Lahar A very rapid type of downslope mass movement that involving mudflows from volcanic ash. Ranking and naming a cyclone Intensity scales.
A wide range of wind speeds is possible between tropical cyclones of minimal strength and the most intense ones on record, and tropical cyclones can cause damage ranging from the breaking of tree limbs to . The mid-latitude cyclone is rarely motionless and commonly travels about kilometers in one day.
Its direction of movement is generally eastward (Figure 7s-2). Precise movement of this weather system is controlled by the orientation of the polar jet stream in the upper troposphere.