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Lecture 2 – From observations to measurements Prof. Dr. E. Igenbergs (LRT) Dr. D. Koschny (ESA) 1 Image: © David A. Hardy/www.astroart.org' Near-Earth objects – a threat for Earth? Or: NEOs for engineers See also: final report from the asteroid retrieval mission study run by JPL and Caltech, through the Keck Institute for Space Studies. It's available here: http://kiss.caltech.edu/study/asteroid/asteroid_final_rep ort.pdf News 2 Outline 3 3 Survey programmes Catalina Sky Survey • http://www.lpl.arizona.edu/css/ • Mount Bigelow, north of Tuscon, AZ – 68/76 cm f/1.9 Schmidt telescope • Siding Spring, Australia – 50 cm Schmidt telescope for survey, 1-m telescope for follow-up (5 nights per month) • Mt. Lemmon 1.5 m f/2 telescope 4/574 Survey programmes - 2 Panoramic Survey Telescope & Rapid Response System http://pan-starrs.ifa.hawaii.edu/public/ Several ‘key projects’ – one of them is Populations of Objects in the Inner Solar System Not observing asteroids all the time – but very successful when it does 5 Survey programmes - 3 http://scully.cfa.harvard.edu/cgi-bin/skycov.cgiSky 6 TOTAS – Teide Observatory Tenerife Asteroid Survey 1 m aperture, 10 % obstruction Focal length 4.4 m Camera with 1.26” per pixel image scale 7 Survey programmes - 4 TOTAS = Teide Observatory Tenerife Asteroid Survey http://vmo.estec.esa.int/totas/ Only a few hours every month since 2010 – ca. 500 new discoveries, 2 NEOs Small field of view => scan 5 x 5 images every 30 min – results in a field of 4 deg x 4 deg to be covered 8 The observatory code The IAU defines so-called observatory codes All asteroid observers must have one Defines name, longitude, latitude, elevation, contact person Examples: • J04 – Optical Ground Station, ESA (on Tenerife) • B12 – The Koschny Observatory (in the Netherlands) • 230 - Mt. Wendelstein Observatory • 703 - Catalina Sky Survey • F51- Pan-STARRS 1, Haleakala 9 The detection system - 1 Observing goal of ESA’s SSA-NEO programme: • Detect all asteroids in dark sky larger than ~40 m at least 3 weeks before closest encounter to Earth How: Telescope network • Size and number of telescopes versus field of view • Location of telescopes (North/South – space-based sensors…) Follow the system engineering approach • Collect activities • Collect options, visualize them, order them • Set up matrix, evaluate them 10 The detection system - 2 Main parameter options (to be traded-off) • Automation versus human recognition – cost versus robustness • 3 or 4 images of the same field – duration versus robustness • Repeat cycle - duration • Pointing direction • Maximum angular velocity – neglect fast objects versus robustness • Telescope aperture – detection limit • Field of view – duration versus constraints on aperture • Exposure time – detection limit versus duration, smearing 11 Modelling the detection system Telescope Asteroid Sun Camera 12 Modelling the detection system Telescope Asteroid Sun Camera Abstract model 13 Modelling the detection system Albedo p Phase function f() Distance to Earth Telescope Distance to Sun - Effective Aperture in m2 - Throughput Asteroid Sun Emitted light - 1366 W/m2 Abstract model with parameters Camera - Quantum efficiency - Noise => Signal-to-Noise of a given asteroid 14 Brightness of the asteroid - 1 Apparent magnitude • Hipparcos divided star brightnesses in 6 ‘equal’ classes from 1 – 6, ‘1’ being the brightest stars • Response of the eye: non-linear • Objects with flux density relations 1:10:100 look like having the same brightness difference • Pogson 1856 defined the magnitude in a mathematical way… noting that the brightness difference of 1 mag and 6 mag stars is roughly 100 => m Pogson defined the ratio of the brightnesses of class n and n+1 to be sqrt (100) ~ 2.512. • Let F be the flux density in W/m2, then F2 m2 m1 2.5 log F1 • m = ‘magnitude’, brightness class • F0 is defined as the flux density of magnitude 0 • Astronomers use Vega (Alpha Lyrae) as the reference • Sun: Mv = -26.8 mag; MR = -27.1mag and FSun = 1366 W/m2 15 Johnson-Cousins Filter bands passband in nm average wavelength in nm U – ultraviolet 300 – 400 360 B – blue 360 – 550 440 V – visual 480 – 680 550 R – red 530 – 950 700 I – infrared 700 – 1200 880 Name 16 Good to know Flux in W/m2 is energy per time and area Energy of one photon: EPhot hc Where h = 6.626.10-34 Js, c = 2.998.108 m/s Brightness of the asteroid - 2 Fast, Earth Fast 1 pAf ( ) 2 2d ast Assume a simple sphere, homogeneous (Lambertian) scatterer: 18 In magnitudes: Absolute magnitude versus size Absolute magnitude = magnitude of the asteroid at 1 AU from the Sun, seen from a distance of 1 AU, at a phase angle (angle Sun – asteroid – observer) of 0 degrees Assumption: Albedo is 0.05 Abs. magnitude Size 14.0 9400 m 16.0 3700 m 18.0 1500 m 20.0 590 m 22.0 240 m 24.0 95 m 26.0 37 m 28.0 15 m 30.0 6m 20 The telescope Definition of the f-ratio: Focal length f ratio Flux at detector: fl d Diameter of lens FDetect Fin ( A Aobstr ) where FDetect the detected flux, Fin the incoming flux from the object, A the surface area of the prime mirror, Aobstr the area of the obstruction, and the throughput. Sketch of a telescope - incoming flux F in W/m2, surface area A in m2 21 The detector CCD = Charge Coupled Device Converts photons into e Readout results in data matrix in computer containing Digital Numbers Quantum efficiency QE • Percentage of photons which generate an electron Gain g • e- per Digital Number Full well • Maximum no. of e- in a pixel 22 The detector – 2 Star image taken with CCD 100 102 98 100 101 100 99 150 223 140 102 100 150 402 803 400 200 98 102 130 220 130 107 102 98 99 120 98 100 100 Not all light goes to center pixel – the percentage is ppx Noise: comes from different sources: photon noise, dark noise, readout noise, bias Digital Number DN 23 The detector - 3 Signal-to-Noise ratio: SNR Signal / Noise DN signal DN signal DN bias DN dark DN readout DN Sky Signal is a function of input flux and detector properties: DN Signal texp p px g FDetect, hc / QE d Assume an ‘average wavelength’: DN Signal texp p px g FDetect QE hc / 24 Typical values for TOTAS 1 m aperture, f/4.4 CCD camera has four sensors, 2048 x 2048 px2 Pixel scale 1.2”/px, field-of-view 0.7 deg x 0.7 deg For survey: We use 1 min exposure time Reaches ~21.0 mag ‘Deepest’ surveys go to 22.5 mag 25 Stephan’s Quintett 2 min exposure Summary We have learned how asteroid surveys work We know which parameters are important • Number of telescopes, sensitivity, field of view • The same sky area is observed three or four times to detect moving objects • Many trade-offs are necessary to optimize a survey We have modelled the complete observation chain We can compute the sensitivity of a telescope For modelling the complete survey, a simulator is required Workshop 30 Impact energies What was the impact energy of the ‘Sudan event’ compared to the Hiroshima bomb? The ‘Sudan event’ (2008 TC3) was an elongated object with <10 m size – assume 5 m x 5 m x 5 m Assume an entry velocity of 15 km/s Densities of recovered meteorites varied from 2 to 3 g/cm3 – assume 2.5 g/cm3 Impact energies are often given in ‘kilotons TNT’ or ‘megatons TNT’ • 1 kt TNT = 4.184 * 1012 J The ‘little boy’ Hiroshima bomb had an explosive yield of 15 kt TNT 31/ Sensitivity of ESA’s 1-m telescope The camera at ESA’s telescope on Tenerife is cooled by liquid nitrogen to temperatures such that the dark current and its noise contribution can be neglected. The readout is slow enough so that also its noise contribution can be neglected. The camera is operated with a bias of DNbias ~ 8000. For a reliable detection, the SNR of an object should be larger than 5. Compute the sensitivity of ESA’s telescope, using the following assumptions for the CCD camera: QE = 20 %; g = 0.9 e-/DN. Assume that all the photons coming from the object are red at a wavelength of 600 nm. Assume that the telescope transmits = 60 % of the photons to the CCD; ppx = 20 % of the photons fall on the center pixel. The telescope obstruction is 20 % of the size of the main mirror. 32 Step 1 Compute the flux in W/m2 and the apparent magnitude of a 1000 m object and an albedo of p = 0.05, 1 AU from the Earth, 2 AU from the Sun. 33 Step 2 With the flux coming from the asteroid, compute the flux at the sensor Step 3 Using the properties of the CCD camera, compute the SNR for the 1 km asteroid. Bonus task: Compute the minimum Digital Number of the asteroid on the sensor for a Signal-to-Noise ratio of 5. 36