Thursday, October 30, 2008

Big Boob Tsunade Comic

Linearity of the CCD: the problem

And 'one of the main advantages of CCD sensors. Indeed, it is the characteristic that makes our CCD sensor and a measuring instrument not just a simple "camera" digital.
Linearity means that there is a simple linear relationship between the input value (the electric charge collected in each photoelement) and the output value (the number assigned to each pixel that composes the final image).

There are two important limits defined by the elements of its CCD sensor input and output elements of the CCD camera: the first is the Full Well Capacity photoelements of making up the sensor while the second is the type of analog to digital converter (or ADC Analog to Digital Converter) used by the CCD camera.
E 'so easy to see that there are two levels of saturation : the first is the ability to collect individual photoelements electrons that make up the CCD, the second is given by the resolution (in bits) of the analog-digital converter.

To fix ideas, always consider the example of the CCD camera sensor with Apogee Ap7p SITE supplied Astronomical Observatory of Cavendish. The size of 24 microns square photoelements have a Full Well Capacity of about 300000 electrons as the analog to digital converter has a resolution of 16 bits, corresponding to 65535 ADU (2 ^ 16).
If we build a graph with the x-axis input data, the number of electrons contained in photoelement, and the ordinate the output value, the number of ADU of the corresponding pixel of the image, these two limits are represented by the saturation two blue lines, respectively (x = 300000) and red (y = 65535).

A CCD camera is not professional but good quality present a curve similar to the linear graph above where the green lines is precisely the section where the camera behaves in a linear fashion while the orange, which starts at around 250,000 photoelectrons captured by photoelement, is the non-linear stretch which is lost by the photometric quality of the chamber.
We note that the same graph gives us a couple of notes: we know from analytic geometry that the equation of a line has an expression:

Y = mX + c where

m is the slope, or the slope of the line and c is the so-called known term, namely ntercetta with the y-axis. Well, the slope m (equal to the tangent of the angle that the line of linearity underlying the x-axis) is no more che l'inverso del gain, mentre c è l'offset della camera CCD (che nel caso della Apogee Ap7p è posto a circa 3080 ADU).

Notiamo immediatamente un'altra cosa importante: il tratto non lineare inizia prima che la curva di linearità raggiunga uno qualsiasi dei due livelli di saturazione: dunque l'operatore non ha nessuna avvertenza o segnalazione di quanto sta avvenendo. Per questo è importantissimo determinare in modo sperimentale le coordinate del punto P.

Wednesday, October 22, 2008

New Spinning Bike From Costco



Saturday, October 18, 2008

Behind Rebel Lines Chapter Summaries

Contrail before 1995 before 1995 Contrail II

Continues Wheeled material that shows how contrails are known - and photographed - a long time. Another documented example and 'an article dating back to 1974 , dedicated to the analysis of a series of observed contrails in the skies of America; complete reference: TG Konrad, JC Howard, "Multiple Contrail Streamers Observed by Radar", Journal of Applied Meteorology, vol. 13, 563-572, 1974 .

Without discussing the article, reporting directly to a series of photos in it (with captions):




Friday, October 10, 2008

Standard Transmission Minivan



I continue with the recovery of materials relating to research on the contrail (condensation trails) in past decades. And I 'have seen, among many supporters of the alleged evidence of "chemtrails", a strong increase in the use of the argument that before a certain date (1995) basically there were no contrails in the sky. Until you get to real challenges, retrieve old photos to show you they were contrails (not counting the obvious point, namely that in the past decades the traffic was much less than today).

As already ' I started doing this blog, the answer to this question is 'much more' simple. In fact in the scientific literature over the years there 'has been a growing attention to the phenomenon of condensation trails, mostly out of concern that with the increase in air traffic, the relative increase in contrail formation could lead to climatic changes ( leading to increased cloud cover, thus blocking a certain percentage of solar radiation). In many studies published even before the '90s, is a clear indication of condensation trails, how are visible and common, but how often is persistent over time.

Turning to practical examples, in a study of 1975 proposes the study of the contrail found in some satellite images of the island of Cyprus (full reference: Joseph JH, Levin Z, Y, Mekler, G Ohring, J. Otterman, "Study of contrails Observed from ERTS-1 satellite imagery", J. Geophys. Res, 1975, vol. 80, no. 3, 366-372 ). , The article reports - should be repeated - explicitly as the contrail formation of both normal and as the trails can be persistent enough to develop into cirrus clouds:

in Some Areas of heavy jet traffic, contrails released by a number of Aircraft May spread to cover a portion of the sky With thin cirrus-type clouds. The Possibility That May Such contrails lead to an increase in the average amount of high cloudiness and that such an increase of clouds may affect the earth's weather and climate has been raised [Murcray, 1970; Machta and Carpenter, 1971].

A parte questo, nel paper si ritrova una delle immagini satellitari usate:


Per la precisione, si noti che le immagini sono state prese nel 1972.

Un altro esempio e' uno studio del 1970 , sempre focalizzato su come le scie di condensazione possano influire sul clima (reference completa: PM Kuhn, "Airborne Observations of Contrail Effects on the Thermal Radiation Budget",Journal of the Atmospheric Sciences, 1970, vol. 27, 937-942 ). Anche in questo caso vale la pena di estrarre alcuni passaggi che rendono palese come le contrail fossero abbondantemente note, osservate e studiate:

The spreading out of jet contrails into extensive cirrus sheets is a familiar sight. Often, when persistent conditions exist from 25,000 to 40,000 ft, several long contrails increase in number and gradually merge into an almost solid interlaced sheet.

Nell'articolo si riportano dunque alcune fotografie di contrail, in territorio statunitense, come ad esempio:


La foto risale al 1969.