martes, 18 de diciembre de 2012
sábado, 15 de diciembre de 2012
martes, 11 de diciembre de 2012
Main Migration Waves
Accurate methods for the solution of the migration of zero-offset seismic records have been developed. The numerical operations are defined in the frequency domain. The source and recorder positions are lowered by means of a phase shift, or a rotation of the phase angle of the Fourier coefficients. For applications with laterally invariant velocities, the equations governing the migration process are solved very accurately by the phase-shift method. The partial differential equations considered include the 15 degree equation, as well as higher order approximations to the exact migration process. The most accurate migration is accomplished by using the asymptotic equation, whose dispersion relation is the same as that of the full wave equation for downward propagating waves. These equations, however, do not account for the reflection and transmission effects, multiples, or evanescent waves. For comparable accuracy, the present approach to migration is expected to be computationally more efficient than finite-difference methods in general.
Population density
Population Density Population density is a measurement of the number of people in an area. It is an average number. Population density is calculated by dividing the number of people by area. Population density is usually shown as the number of people per square kilometer. The map below is a choropleth (shading) map and illustrates population density. The darker the colour the greater the population density.
World population distribution
Population Distribution Population distribution means the pattern of where people live. World population distribution is uneven. Places which are sparsely populated contain few people. Places which are densely populated contain many people. Sparsely populated places tend to be difficult places to live. These are usually places with hostile environments e.g. Antarctica. Places which are densely populated are habitable environments e.g. Europe.
Map of natural increase of world population
Currently there are 49 independent states in Europe.
· Differences: - Depending on its length: the rule is Russia's largest and the smallest of Andorra.
- Depending on your situation: almost all have sea views.
- Depending on their shape: Many are fragmented.
According to its population: The most populous is Russia and the least populated is San Marino.
- According to your wealth: wealthier and poorer German and Moldova.
World water cycle
En la siguiente fotografía podemos ver el recorrido que hace el agua en la Tierra, es decir, el ciclo del agua.
El Ciclo del
Agua:
viernes, 7 de diciembre de 2012
World Climatological Map
En el siguiente mapa podemo ver ls diferentes climas que se dan en lugares del todo el mundo:
El clima es el promedio de temperaturas, precipitacions y humeda que se dan en lugar determinado. El cambio de temperaturas entre las diferentes latitudes terrestres, las variación de las precipitaciones y la fuerza del viento. Todos ests factores hacen que va´rén los paisajes de estas zonas, dando lugar a bosques, selvas, tierras heladas, taigas... Producen tambien los diferentes fenómenos meteorológicos extremos: sequías tormentas, ventiscas...
También tienen que ver los cambios en las presiones atmosféricas.
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