Thursday, June 17, 2010

CUTE...


REAL PAINTINGS

                                        

BLUE LIKE MARS


This image shows the west-facing side of an impact crater in the mid-latitudes of Mars' northern hemisphere. Like many mid-latitude Martian craters, this one has gullies along its walls that are composed of alcoves, channels and debris aprons. The origins of these gullies have been the subject of much debate; they could have been formed by flowing water, liquid carbon dioxide or dry granular flows.




Many of the other features observed in and around this crater are indicative of an ice-rich terrain, which may lend credence to the water formation hypothesis for these gullies. The most notable of these features is scalloped terrain in and around the crater. This type of terrain has been interpreted as a sign of surface caving, perhaps due to sublimation of underlying ice. Sublimation is the process of a solid changing directly to a gas.



Another sign of ice is the presence of parallel lines and pitted material on the crater floor. Parallel linear cracks are also observed along the crater wall over the gullies, which could be due to thermal contraction of ice-rich material.



together, these features are evidence for ice-rich material having been deposited in this region during different climatic conditions, material that has subsequently begun to melt and/or sublimate under current conditions. More recently, wind-blown deposits have accumulated around the crater, as evidenced by the parallel ridges dominating             

Thursday, June 10, 2010

HUMOUR OF THE DAY



This wife is too jealous
There was once a wife so jealous that when her husband came home one night and she couldn't find hairs on his jackets she yelled at him, "Great, so now you're cheating on me with a bald woman!"
Two People In The Same Grave
A woman and her little girl were visiting the grave of the little girl's grandmother. On their way through the cemetery back to the car, the little girl asked, "Mommy, do they ever bury two people in the same grave?"

NIST joins NASA

The National Institute of Standards and Technology (NIST) and the National Aeronautics and Space Administration (NASA) have launched a joint effort to gather enhanced climate data from spaceborne climate observation instruments planned for a group of satellites now under development.
One of the CLARREO satellites, which will make observations of the energy the Earth absorbs from the sun and radiates back into space. The balance between them affects the climate.
Credit: NASAView hi-resolution image
The Climate Absolute Radiance and Refractivity Observatory (CLARREO) Mission includes a fleet of satellites tentatively scheduled for launch later this decade that will gather data for long-term climate projections. The CLARREO mission will provide an accurate climate record of the complete spectrum of energy that Earth reflects and radiates back into space, measurements that should provide a clearer understanding of the climate system.
NIST’s role will focus on the calibration of the instruments aboard CLARREO satellites, as well as on the accuracy that the sensors must meet. The measurements need to be characterized to far greater accuracy—from two to 10 times better, depending on the wavelength of light in question—and detector standards need to be developed for the far infrared region of the spectrum. NIST will also help NASA improve its own capabilities in instrument calibration. The collaboration was finalized in a Space Act Agreement on Feb. 4, 2010.
CLARREO, led by NASA Langley Research Center in Hampton, Va., is now among NASA’s top-priority missions because of its high ranking by the National Research Council, which designated CLARREO one of its four “Tier One” missions when it evaluated proposals in 2007. NASA is allocating $270,000 for NIST’s contributions to the project this year.
The mission is part of a longer-term effort to establish global long-term climate records that are of high accuracy and traceable to the international system of units (SI). The CLARREO satellites and other instruments will be calibrated against international standards based on SI, so that observations from different times and locations can be compared usefully, creating a more reliable record of long-term climate trends.