Monday, November 26, 2007
Snl Christopherlowell
WANT IS POWER
a while since I wrote and I'm going a bit liadilla. Between gigs, workshops and home, the girl, buying, husband, etc ... etc ... etc ...
Well, there's nothing like propose things and see how you feel it ... it is clear that the power is in the mind.
Great! I practically almost month and a half on a diet "in quotes" and we've lost 4 kilos. This means that we continue on this line, target until this summer.
From Coca Cola I hardly agree, seriously ... clear that there were 138 calories x 3 cans a day approx., if I remember correctly is 414 calories a day "extras" + out of control with food, if a fried potatoes, that if a bollicao ... I tell ya.
Anyway, I think I've gone ape and control what I have in mind.
This week will be decisive in the gigs, more than anything, because they just replace the 3rd of December and again the girl who I am replacing ... Logic is my project to happen to music "we are in negotiations," I hope so.
Well, I'll tell you next week has been, it seems to be "the best of my Head of Department" I have several boyfriends ... that HR has to propose several offers on the table ... Joer, Lucky me! Right?
Still, my priority is to happen to commercial. I hope to choose the best and no mistake.
Sunday, November 11, 2007
Creuset Number Meaning
What is Global Warming? As
Composition of the Atmosphere.
The atmosphere is the gaseous layer covering the planet Earth, and remain trapped by gravitational force. In relative terms the size of Earth, the thickness of the atmosphere is very small because the 99% of its mass is concentrated within 30 km above the Earth's surface.
Parties that make these 30km, or 99% atmosphere.
Near surface air dry (no water vapor) is composed of:
water vapor and CO2 are the two most important gaseous components in the generation of greenhouse gases in the atmosphere.
Global Warming.
global warming is an increase in time, the average temperature of Earth's atmosphere and oceans. The global warming theory postulates that the temperature has risen since the late nineteenth century due to human activity, mainly by emissions of CO2 that fostered the greenhouse effect.
What is the cause of global warming?
Carbon dioxide and other air pollutants accumulating in our atmosphere, creating an increasingly thick layer. Because it traps more heat in the sun and gives result in warming our planet, not given by natural cycles. The main source of carbon dioxide emissions from human activities are the generation of power plants based on coal (2.500 million tons emitted per year). The second source is the cars, which paortan nearly 1.500 million tonnes of CO2 a year.
Greenhouse. Formally
can explain global warming detailing processes that are triggered in the greenhouse effect. The greenhouse effect of Earth's atmosphere is related to radiative processes occurring in it. Radiation is a form of heat energy, and is the only one that is transmitted in a vacuum. Other modes of transmission of heat energy in the natural environment are the conduction and convection. Conduction occurs when heat propagates through a solid (eg the propagation of heat from the surface soil to lower levels). In fluids (gases and liquids) heat is transferred by convection process through which relatively warm parts of the fluid moving and then mixed and integrated into a relatively cooler environment.
The characteristics of the radiation that propagates in the form of electromagnetic waves has to do with the temperature of the issuing body (as all the bodies to a lesser or greater extent they do). In the atmosphere are present two types of radiation. On one side is the solar radiation that comes from the sun's surface to about 6000 ° C.
Continue Reading ...
This is manifested mainly in the form of rays in the visible spectrum. On the other hand, the Earth's surface (continents, oceans, ice caps, all components that lie in the earth's crust) and the atmosphere also emit radiation, but with an energy level much lower than that of the Sun This radiation called infrared, not visible to the naked eye, but is spread similarly to solar radiation .
The atmosphere is quite transparent to solar radiation is considerably more opaque to infrared radiation coming from the Earth's surface. In fact, a large part of terrestrial infrared radiation is absorbed by the atmosphere by so-called greenhouse gases, among which the most important are carbon dioxide (CO2) and water vapor. This infrared radiative energy trapped by the atmosphere is re-emitted into the Earth's surface. That will add up and accumulate during the day, solar radiation, and partially offsetting overnight cooling of the surface.
greenhouse Analysis in the Twentieth Century.
Thus the net effect of greenhouse gases is to increase the average temperature near the surface. Hence then the concern about the effect it can have on global climate continued to register increases in the concentration of CO2 in the atmosphere due to industrial activity:
In the twentieth century records of pioneer scientists early of the 1960's, began to show a clear pattern of sustained growth in a steady increase in the concentration of CO2 in the atmosphere of our planet.
Fuentes.
Composition of the Atmosphere.
The atmosphere is the gaseous layer covering the planet Earth, and remain trapped by gravitational force. In relative terms the size of Earth, the thickness of the atmosphere is very small because the 99% of its mass is concentrated within 30 km above the Earth's surface.
Parties that make these 30km, or 99% atmosphere.
Near surface air dry (no water vapor) is composed of:
- Nitrogen (N)
- 78.1% Oxygen (O2) 20.9% 1%
- Various Gases: Argon (A) 0.93%, sulfur dioxide carbon or carbon dioxide (CO2) 0.033%, and others such as neon (Ne) and helium (He) with lower concentrations.
water vapor and CO2 are the two most important gaseous components in the generation of greenhouse gases in the atmosphere.
Global Warming.
global warming is an increase in time, the average temperature of Earth's atmosphere and oceans. The global warming theory postulates that the temperature has risen since the late nineteenth century due to human activity, mainly by emissions of CO2 that fostered the greenhouse effect.
What is the cause of global warming?
Carbon dioxide and other air pollutants accumulating in our atmosphere, creating an increasingly thick layer. Because it traps more heat in the sun and gives result in warming our planet, not given by natural cycles. The main source of carbon dioxide emissions from human activities are the generation of power plants based on coal (2.500 million tons emitted per year). The second source is the cars, which paortan nearly 1.500 million tonnes of CO2 a year.
Greenhouse. Formally
can explain global warming detailing processes that are triggered in the greenhouse effect. The greenhouse effect of Earth's atmosphere is related to radiative processes occurring in it. Radiation is a form of heat energy, and is the only one that is transmitted in a vacuum. Other modes of transmission of heat energy in the natural environment are the conduction and convection. Conduction occurs when heat propagates through a solid (eg the propagation of heat from the surface soil to lower levels). In fluids (gases and liquids) heat is transferred by convection process through which relatively warm parts of the fluid moving and then mixed and integrated into a relatively cooler environment.
The characteristics of the radiation that propagates in the form of electromagnetic waves has to do with the temperature of the issuing body (as all the bodies to a lesser or greater extent they do). In the atmosphere are present two types of radiation. On one side is the solar radiation that comes from the sun's surface to about 6000 ° C.
Continue Reading ...
This is manifested mainly in the form of rays in the visible spectrum. On the other hand, the Earth's surface (continents, oceans, ice caps, all components that lie in the earth's crust) and the atmosphere also emit radiation, but with an energy level much lower than that of the Sun This radiation called infrared, not visible to the naked eye, but is spread similarly to solar radiation .
The atmosphere is quite transparent to solar radiation is considerably more opaque to infrared radiation coming from the Earth's surface. In fact, a large part of terrestrial infrared radiation is absorbed by the atmosphere by so-called greenhouse gases, among which the most important are carbon dioxide (CO2) and water vapor. This infrared radiative energy trapped by the atmosphere is re-emitted into the Earth's surface. That will add up and accumulate during the day, solar radiation, and partially offsetting overnight cooling of the surface.
greenhouse Analysis in the Twentieth Century.
Thus the net effect of greenhouse gases is to increase the average temperature near the surface. Hence then the concern about the effect it can have on global climate continued to register increases in the concentration of CO2 in the atmosphere due to industrial activity:
In the twentieth century records of pioneer scientists early of the 1960's, began to show a clear pattern of sustained growth in a steady increase in the concentration of CO2 in the atmosphere of our planet. Fuentes.
- http://www.atmosfera.cl/HTML/temas/estructura/estructura5.htm
- http://www.cambioclimaticoglobal.com/atmosfe2.html
- http://www.cambioclimatico.org/
- http://www.cambio-climatico.com/
Alpha Kappa Alpha Letter Of Interest
as the Hail?
Hail forms only in the Cumulonimbus (clouds with a very flat top) that are highly developed. They can reach fifteen thousand feet, and in addition to hail, are responsible for originating storms and tornadoes.
As the ice crystals are stirred restlessly, rub each other, and merging, and polishing their surfaces, making spherical bodies, often in quite perfect. A piece of hail of 3 cm in diameter, has a volume of 10,000 million times larger than a cloud droplet (diameter of a cloud droplet average: 10 to 20 microns). In other words, they must collect some 10,000 million droplets to form a piece of hail of 3 cm in diameter. In the larger stones are alternately transparent ice and opaque ice.
is noteworthy to understand that it is like a conveyor belt driven by strong winds upward, bringing the liquid water to cool it so that it condenses and then freezes every drop adding layers individually frozen until fall under its own weight.
The rate of decline varies in proportion not only the weight of the hailstones, but the storm that is happening around.
Some researchers have suggested that a critical parameter would be the height that is the isotherm of 0 ° C, with respect to the base of the cloud. In general it was observed that the production of hail is more common it is lower that isotherm. Updrafts and downdrafts, allowing ice particles growth, remain in a storm long enough to reach a large size. In the vertical motion, are running up and down with very high speeds. It is assumed that current speeds can exceed 100 m / s (360 km / h).
http://www.mailxmail.com/curso/excelencia/meteorologia/capitulo23.htm ...
http://es.wikipedia.org/wiki/Granizo
http://www.smn.gov.ar/
- What is hail?
would be generated and evolve an atmospheric phenomenon to become hail should be given certain conditions and circumstances, which are processes that must be fulfilled without equanum (inclusive) to result in this type of precipitation.
Hail forms only in the Cumulonimbus (clouds with a very flat top) that are highly developed. They can reach fifteen thousand feet, and in addition to hail, are responsible for originating storms and tornadoes. - hail formation process.
When air currents ascend to heaven in a very violent, the water droplets freeze into ice after ascending to the higher elevations of the cloud (where the temperature is at least 0 degrees Celsius). As time passes, the water droplets earn dimensions that are dense enough to be unstoppable and stay longer in suspension. That's when it happens to fall in between the cloud droplets taking with it finds in its path.
As the ice crystals are stirred restlessly, rub each other, and merging, and polishing their surfaces, making spherical bodies, often in quite perfect. A piece of hail of 3 cm in diameter, has a volume of 10,000 million times larger than a cloud droplet (diameter of a cloud droplet average: 10 to 20 microns). In other words, they must collect some 10,000 million droplets to form a piece of hail of 3 cm in diameter. In the larger stones are alternately transparent ice and opaque ice. is noteworthy to understand that it is like a conveyor belt driven by strong winds upward, bringing the liquid water to cool it so that it condenses and then freezes every drop adding layers individually frozen until fall under its own weight.
The rate of decline varies in proportion not only the weight of the hailstones, but the storm that is happening around.
- Geographic Distribution.
occurs worldwide, especially in middle latitudes. Cause much destruction in rural areas, can cause partial or total loss of crops. In Argentina the most frequent sites ...
Continue Reading ...
... are related to the eastern foothills of the central Andes of Mendoza, the Sierras of Cordoba, Aconquija system. In the area of the Pampas plains occurs in situations where dominant surface warm, moist air to flow inputs cold air height and situations to the continent of very cold air masses.
Unusual hail in Buenos Aires. July 26, 2006.
Continue Reading ...
... are related to the eastern foothills of the central Andes of Mendoza, the Sierras of Cordoba, Aconquija system. In the area of the Pampas plains occurs in situations where dominant surface warm, moist air to flow inputs cold air height and situations to the continent of very cold air masses.
Unusual hail in Buenos Aires. July 26, 2006.
- Occurrence of hailstones.
Some researchers have suggested that a critical parameter would be the height that is the isotherm of 0 ° C, with respect to the base of the cloud. In general it was observed that the production of hail is more common it is lower that isotherm. Updrafts and downdrafts, allowing ice particles growth, remain in a storm long enough to reach a large size. In the vertical motion, are running up and down with very high speeds. It is assumed that current speeds can exceed 100 m / s (360 km / h).
- Fuentes.
http://www.mailxmail.com/curso/excelencia/meteorologia/capitulo23.htm ...
http://es.wikipedia.org/wiki/Granizo
http://www.smn.gov.ar/
Subscribe to:
Posts (Atom)