Hollywood actress angelina jolie full profile and details

HOLLYWOOD ACTRESS ANGELINA JOLIE PROFILE :-
PERSONAL DETAILS -
Full name - Angelina jolie voight
Megan fox nicknames -angie ,catwoman ,ange ,aj
Date of birth -june 4th 1975 in los angles ,california ,usa
Gender - female
Sexual orientation -bisexual
Race or ethnicity -white
Religion -buddhist
Zodiac sign -gemini
Nationality -american
Speaks - english and french
Trade mark -husky voice and her full lips
Party affiliation - independent

Family and friend of angelina jolie :-
Father - jon voight (actor)
Mother - marcheline bertrand (actress)
Brother - james heaven (actor)
Godfather -maximilian schell
Godmother -jacqueline bisset
Daughter -zahara marley,jolie-pitt, shiloh nouvel,
Son-maddox chivan jolie-pitt ,pax thien jolie-pitt,knox leon jolie-pitt
Uncle-chip taylor
Husband-billy bob thornton jonny lee mortan
Boyfriend - timothy hutton ,val kilmar ,brad pitt
ANGELINA JOLIE EDUCATION

BOLLYWOOD AND AAMIR KHAN MOVIE THE FALLING

RELEASE YEAR -2010
GENRE - SOCIAL
LANGUAGE - HINDI
DIRECTOR -ANUSHA RIZVI
PRODUCER - A
AAMIR KHAN

CAST - NASEERUDDIN SHAH AS SALIM KIDWAI
This movie is about high farmer suicide rate in the country .the story is about a journalist who reveals the misery of the farmer.

BOLLYWOOD MOVIE LAJJO

RELEASE YEAR -2010
GENRE - COMEDY
LANGUAGE - HINDI
DIRECTOR -MANI RATNAM
PRODUCER - BOBBY BEDI
MUSIC DIRECTOR - A R RAHMAN
CAST - AAMIR KHAN

AAMIR KHAN MOVIE BOMBAY VELVET

Bombay velvet is based on true story life incidents that happened in the 1940s .
DIRECTOR -anurag kashyap
PRODUCER - danny boyle
CAST - Aamir khan

AAMIR KHAN UPCOMING MOVIES

THE NEXT UPCOMING MOVIE IS DHOBI GHAT :-
DIRECTOR -KIRAN RAO.
PRODUCER-KIRAN RAO ,AAMIR KHAN.
CAST - AAMIR KHAN.

AAMIR KHAN UPCOMING MOVIES

THE NEXT UPCOMING MOVIE IS DHOBI GHAT :-
DIRECTOR -KIRAN RAO.
PRODUCER-KIRAN RAO ,AAMIR KHAN.
CAST - AAMIR KHAN.

Aamir khan next upcoming movie

Dhobi Ghat (January
21, 2011) - Under
Production
Cast & Crew
Aamir Khan Productions
Status
Under Production
Color
C
Release Date
January 21 , 2011
Language
Hindi
Genre
Social
Shooting Studios
Filmcity
Producer
Aamir Khan
Kiran Rao
Executive Producer /
Co-Producer
B. Shrinivas Rao
Director
Kiran Rao
Star Cast
Prateik Babbar ...... Munna
Aamir Khan ...... Arun
Monica Dogra ...... Shai
Kriti Malhotra ...... Yasmin
Kitu Gidwani ...... Vatsala
Nafisa Khan ...... Amma
Cassettes and CD's on
T-Series
Cinematography
Tushar Kanti Ray
Action
Javed Eijaz
Editor
Nishant Radhakrishnan
Costume
Isha Ahluwalia
Darshan Jalan
Media Relations
Spice

BEST AND TOP ARTICLES

MAKE FRIENDS WITH NATURE :-
how many of u have stayed in a log cabin on a mountain?dont you think it can be a lots of friends to enjoy this experience?if it is during the winter, you might be lucky enough to see snow-covered mountains. Picture-perfect, as it is called!
However,this is not just found in pictures. You can enjoy the myriad effects nature has on the mountains and the meadows,the lakes and trees around you. Come spring and the countryside is a bright hue of colours with the wild flowers in a full bloom and the green grass of meadow looking lush and great for a good game of catch or even football perhaps!
Life in the country side can be a lot of fun and you will find the whole experience very refereshing. There is so much to learn from nature .a very important fact is that you must learn to respect nature. Dont defy and dont defile nature. When you are out in the countryside ,keep your surrounding clean.

RELATIVE HUMIDITY

Relative humidity is the percentage ratio of actual water vapour contained in a given sample of air, to thd maximum quantity of water vapour that the sample can hold at that temperature.
Ie the temperature of asample of air is raised,its capacity to hold water vapour increases and,assuming that no water vapour is allowed to come in or go out of the sample of air,relative humidity decreases the air becomes relatively drier . The opposite happens in the sample of air is cooled its relatively humidity increases.

ABSOLUTE HUMIDITY

Absolute humidity is the mass of water vapour contained in a sample of air. It is usually expressed in grams per cubic metre.

HUMIDITY

Humidity is the quantity of water yapour present in the atmosphere.

WHY POLAR REGION ARE COLDER THAN EQUITORIAL REGION

Since earth is so far from the sun,the sun's ray may be assumed to be parallel to each other when they arrive. The half of the earth towards the sun gets sunlight,during daytime. It will be noticed that each pole receives sunlight only during its summer. This is the reasons why poles are colder.

GREEN HOUSE EFFECT

The foregoing phenomenon is called green house effects because this principal is used to grow tropical plants in cold regions,in a special structure called green hotse. A large room is built with glass roof and glass sides with small windows for air circulation.
Sunlight easily enters the room through the roof od the house ,cannot pass easily through the glass and gets trapped inside the room,thereby raising the temperature of the room.

WHY CLOUDY NIGHTS ARE WARMER

On striking the earths surface,most of the insolation is directly reflected off and only a small fraction is absorbed. If thir was not so, the earths surface melts due to greater heat. The energy, thus absorbed by the earth ,is re-rediated by it this re-rediation,called terrestrial radiation,is of very much longer wave length than insolation and hence cannot easily penetrate the environment.
Terrestrial radiation ,therefore heats the atmosphere .whereas insolation can easily penetrate through clouds ,terrestrial radiation cannot. That is why cloudy nights are much warmer than nights with clear sky.

INSOLATION

Insolation is the name given to all forms energy received by the earth ,from the sun,by the process of radiation.insolation includes includes light,heat,ultra-violet rays, infra red rays etc.
Insolation comes in the form of energy of very short wave length .energy of such short wavelength has the property of passing through transparent media without heating the media. Insolation,therefore,passes through the earth's atmosphere without heating it.

RADIATION

Radiation is the transference of heat from one place to another througs space,without the necessity of any intervening medium. Heat given off by the sun travels through space and reaches the earth by the process of radiation.

CONVECTION

Convection is the transferenre of heat in a fluid(gas or liquid)by the movement of molecules. If one corner of a boul of water is heated,the water particles move about and the heat is distributed throughout the entire body of water.if, small visible dust partical is present in the boul of water,it will be observed that the convection current in the water follow definite patterns. On the earth surface,heat i7 transferred from one place to another by ocean currents and also by convection current of air.

CONDUCTION

In this case ,heat is transferred from one place to another place,through a solid,ay direct contact between molecules.metal objects are very good conductor of heat whereas wooden pieces are bad conductor of heat .if one end of the iron is heated,the other end also gets hot,but it is well known that even if the one end of a wooden stick is burning the other end does not gets heat.land surface are generally poor conductor of heat through different types of soil have different conductivity e.g sand is better conductor than sand.

ATMOSPHERIC PRESSURE

Atmospheric pressure is force extended,per umit area by air.it is thus the weight of the column of air above a unit area.
The average atmospheric pressure is 1013 mb.

SALR

The temperature of a saturated parcel of air,which is made to rise ,falls at a rate of 5 degree per km of ascent i.e the adiabethc lapse rate of a saturated parcel of air or saturated adiabetic lapse rate(SALR) is about 5 degree per km .
Salr is less than dalr because ,as the saturated air is cooled its capicity to hold water vapour decreases and the excess moisture condenses into water droplets.this condensation releases latent heat that warms up the parcel of air therefore ,falls only by about 5 degree per km instead of 10 km .SALR is slightly variable -less at the equator and more at poles.

DALR

It has been observed that the temperature of a dry parcel of air ,which is made to rise,falls at a steady rate of 10 degree celcius for every km of ascent i.e the adiabetic lapse rate of a dry parcel of air , or dry adiabetic lapse rate(DALR) is 10 degree per km.

THE ATMOSPHERE

GENERAL DESCRIPTION :-
The air around earth is called the atmosphere and extend to over 200 km above the surface of the earth.Different layer of earth is called by different names in ascending order,they are the troposphere,stratosphere ,mesosphere and the ionosphere.
The troposphere affects the weather while the ionosphere affects the navigation and communications when using electro-magnetic waves .
THE TROPOSPHERE :- nearly all of the weather changes occurs,and nearly all the water vapour of the atmosphere is contained ,in the troposphere,which extend to a height of about 8 km above the poles and about 16 km above the equator.