1 E-ELT site characterization status Vernin J. a, Muñoz-Tuñon C. b and Sarazin M. c a UMR6525 Fizeau, Nice-Sophia Antipolis University, France; b Instituto de Astrofísica de Canarias (IAC), Tenerife-Spain; c European Southern Observatory (ESO) -Germany; ABSTRACT The site characterization for the future European Large Telescope (E ELT) is a key issue within the European proposal funded by the EC, within the ELT Design Study proposal. The organization, working scheme and baseline frameworks are reviewed. For the definition of the working package WP12000 Site Characterization important use has been done of previous works in the definition of techniques and tools for the study of the atmosphere above observing sites. We have also taken advantage of the number of data already available which have naturally defined a ranking among the known places which have also been taken as a base line for preselecting the candidate sites. The work will last 4 years, started in 2005 and is organized in subtasks whose main objectives are the following: WP12100: To characterize two top astronomical sites (ORM and North-Paranal) and to explore 3 other alternatives (Macon in Argentina, Izaña in Spain and Aklim in Morocco) suitable to install an ELT under the best conditions (Dome C is been currently under investigation, and no particular effort will be put in this site, but rather its atmospheric properties will be compared to the above mentioned sites). WP12200 is dedicated to design, build and operate a standard equipment in all the sites and to perform long term campaign.wp12300 will investigate wavefront properties over large baselines ( m) corresponding to the size of the future ELT, as well as the fine characterization of the optical turbulence within the boundary layer. A similar plan is being carried out by the TMT site selection team. For the sake of saving resources (budget and people), the TMT preselected sites (all in America) are not included in our European study. Keywords: FP6, Site testing, Instruments and tools 1. HISTORY, SCOPE AND ORGANIZATION. The site characterization for the future large European telescope is a fundamental issue and will be undertaken within the ELT Design Study proposal funded by the EC (contract number ). The first meetings and contacts to define the project started in Possible interested partners and institutions were approached and a first version with the design and plans was submitted to the EC commission in February After revision, using the committee feedback, the final proposal was accepted at the end of The Site characterization work started formally in 2005 and will end in December The organization, working scheme and baseline frameworks will be discussed, planned and summarized here. For the definition of the tasks important use have been done of all previous efforts that have been carried out during the last decade in the definition of techniques and tools reliable for the study of the atmosphere above astronomical sites. Important also is the relevance that the studies of the atmosphere has acquired, becoming key projects for most important astronomical sites. Therefore we have also taken advantage of the number of data already available which have naturally defined a ranking among the known places which have also been taken as a bottom line for pre-selecting the potential sites. The institutions and persons involved in the project are summarized in Figure 1, left. Further author information: (Send correspondence to J.V.) J.V.: C.M-T.: M.S.:
2 Figure 1. Left: WP Institutions and participants (In IAC list, H. Vazquez Ramio needs to be included). Right: Map of the world with the location of the selected sites. 1.1 Scope and organization of the work This WP covers the characterization of few sites for what concerns the seeing, ground climatology, atmospheric properties, soil and seismicity. Emphasis is put on already existing astronomical sites and on new physics corresponding to such a large telescope. The final report will help to select the best reasonable place to settle the ELT. For practical reasons the work is divided into four tasks, defined in order to better achieve our commitment: WP12000: Site Characterization, General Management Review, Discussion, reports and final conclusions. WP12100: Review of parameters space WP12200: Instrumentation, measurement and modelling. WP12300: Large Scale Atmospheric Properties. For the definition of the parameter space we have made use of previous reviews, some of which are very recent and results from the increasing interest within the astronomical community in the knowledge of the atmosphere. The basic idea is to perform as much as possible observations in each site which implies to reach a good statistical knowledge of its atmosphere. Hereafter is listed some of the review books which give the state of the art in site characterization in 2003, when the work started: ESO workshop on Site Testing for Future Large Telescopes 1983, eds A. Ardeberg & L. Woltjer. Vistas in Astronomy, The Observatories of the Canaries Vol. 28, 1985, Murdin & Beer eds. Identification, Optimisation and Protection of Optical Telescopes Sites, 1986, Flagstaff. VLT site characterization working group; final report (no. 62), 1990 Sarazin, M., eds. Site properties of the Canarian Observatories New Astron. Reviews, vol 42, 1998, Muñoz-Tuñón, C., eds. SITE2000/ IAU technical workshop. Astronomical Site Evaluation in the Visible and Radio Range ASP, vol 266, 2002, Vernin, J., Benkhaldoun, Z. & Muñoz-Tuñón, C., eds.
3 Figure 2. Ventarrones site, North-East to Paranal. The robotic MASS-DIMM. and the erection of the 5 m tower. 2. DEFINITION OF PARAMETERS SPACE The definition of Parameters Space is not restricted to the list of important physical parameters for site characterization but includes also the instruments and tools to be implemented and the procedure for the correct data analysis and interpretation of the results. In summary the tasks in WP12100 are the following: Define the parameters under investigation: Optical turbulence Cn2(h,t), wind velocity V(h,t), outer scale L0(h,t), seeing ε, isoplanatic angle θ AO, coherence time τ, extinction, dust, cloud cover, humidity, precipitable water vapor, sky emission, sky darkness, light pollution, soil properties and seismicity. Define the few top sites for a comprehensive study Define other possible sites Select the adequate instruments to fulfil the goals. As a first step, we selected the sites to be investigated. To help we have taken into account the TMT site characterization programme (see Mathias Schöck, 2007). In order to do not duplicate our efforts, the TMT candidates (all of them in the American continent) have been excluded in the European search. In Figure 1, right, we present a map of the world with the location of the selected sites. We have preselected two sites, which will be considered as the reference ones: The Observatorio del Roque de los Muchachos (ORM) at La Palma in the Canary Islands-Spain, refereed elsewhere as La Palma and Ventarrones North-East to Paranal (see Fig. 2). Three other sites are also considered: Observatorio del Teide (OT) at Izaña in Tenerife (also in the Canary Islands), Aklim at the Moroccan Anti Atlas (see Fig. 3, left) and a place in North-West Argentina, Macon (see Fig. 3, right). Dome C in Antarctica is also considered for comparisons and references but not under ELT-DS contract. The responsibility of the measurements have been split among the following institutions, all running the WPs: ESO, Fizeau and the IAC. For practical reasons, Atlas and Dome C responsibility belongs to Fizeau, while La Palma and Izaña to IAC and finally N Paranal and Argentina to ESO. There is a large number of instruments and tools designed for site characterization. However when a comparison is to be done is important to use those which have been already tested and cross calibrated and which
4 Figure 3. Left: Aklim mountain in Moroccan Anti Atlas (top), the Moroccan team (Dr. Z. Benkhaldoun and Dr. M. Lazrek at right) and the 5 m erected tower.right, Macon in Argentina Table 1. Instruments developed under FP6 contract item Quantity Developed by GS 2 IAC SSS 1 Fizeau MASS 4 ESO DIMM 4 IAC A. Mounts 4 all are based on well sound physics. Instruments under development or designed to research future purposes only are not useful to fulfil our goals. After revision and discussion we selected the following instruments: Generalized Scidar(GS), MASS/DIMM, All Sky Camera(ASC), High Altitude Dust with satellite images, Automatic Weather Station (AWS), Boundary Layer Profiler, Satellite Climatology, Meteorological Models, Soil Mechanics and Seismicity. Besides, it was decided to explore the use of potential future instrumentation. This is the case of the Single Star Scidar (SSS), designed as an alternative to G-SCIDAR when no telescope infrastructure is available at the site. The work with SSS within the ELT DS task will be study its feasibility and to construct a prototype. The final selection was made according to few criteria such as the underlying physics, their reliability, their ability to issue quantitative measurements and finally the fact that they have been extensively used in many sites. The funding limitation have to be considered and, for example, automatic weather Station (AWS) that have been extensively used and are known to be reliable and robust will not be purchased within the FP6, but with contribution from the host country. The AWS results will be also analyzed in the final report. 3. INSTRUMENTS AND MODELLING In what follows we will summarize the status and design of the instruments selected for ELT DS. The validation of data issued by the use of satellite and model will be discussed. As a summary the instrumentation specifically developed within the FP6-ELT Design Study is provided in table Differential Image Motion Monitor (DIMM) DIMM provides accurate, absolute and reproducible data although systematic control tests on the focus or saturation are however important (see e.g. Tokovinin, 2003). The bases of the instrument are given in Sarazin & Roddier, 1990 and Vernin & Muñoz-Tuñón, 1995.
5 Figure 4. Left: Comparison of seeings measured with the reference IAC-DIMM with the ELT-DIMM and the MASS. Both dimms compares very well and, as MASS is insensitive to ground layer turbulence, it gives better seeing than the dimms. Right: People who participated to ORM DIMM calibration campaign: Z. Benkhaldoun, H. Vazquez, V. Kornilov, Casiana and A. Varela. Since the early nineteens, DIMMs have become very popular and copies of the prototypes provided by the French company LHESA Electronique have been used at different observatories. DIMMs are now auxiliary instruments for telescope operation and complement Adaptive Optics experiments. For what concerns the site selection, accurate statistics is an important issue. In Muñoz-Tuñón et al., 1997 and Ehgamberdiev et al., 2002 one will find a lot of results, recorded in large databases. For example, in Ehgamberdiev et al., seeing values at La Silla, Paranal, La Palma and Maidanak are analized during more than two years. From this analysis, the excellent behaviour of the two sites, Paranal and ORM, is clear and reinforces our choice to take those two sites as a reference. The relative contribution of turbulence at different scale heights is very important when evaluating the feasibility of AO programmes. Today the multiconjugate adaptive optics, MCAO, is a challenge from the technical point of view. Intensive campaigns, although expensive and complicated to carry out, are the only way to obtain a comprehensive knowledge of the atmosphere. For this purpose, simultaneous techniques such as balloon soundings (CN2 profiles, water vapour, wind velocity and direction, see Azouit & Vernin, 2005), SCIDAR, DIMMs and meteorological towers equipped with microthermal sensors have been used in the past. For a general description see Vernin & Muñoz-Tuñón (1992, 1994), and references therein. Some comparison can be made by using previous results from intensive campaigns. The ORM, La Silla and Mauna Kea have been compared in this way. The free atmosphere at the ORM has a very low contribution (0.4 ), which compares with values measured at La Silla (0.34 ) and Mauna Kea (0.46 ). The contribution from the surface layer (from 6 to 12 m) at ORM is 0.08 is almost negligible (Vernin & Muñoz-Tuñón 1994). However, the need of statistical knowledge of the relative contribution the free atmosphere and the boundary layer to the integrated seeing required new or updated techniques. Intensive campaigns cannot provide sufficient data. In order to achieve an accurate statistical database with the relative contribution to the turbulence from the different atmospheric layers in the candidate sites, we propose the use of the G-SCIDAR and/or the MASS/DIMM. Now, four MASS/DIMM have been delivered at each site, but before delivery, a calibration campaign was carried out in September 2007 (see Fig. 4) to verify and confirm that the data provided by the new DIMMs correlate well with existing calibrated DIMM instruments, and to guarantee the reliability of the measurements at the four sites.
6 Figure 5. Observatorio del Teide (Izaña, Tenerife). Marked the location of the Telescopio Carlos Sanchez (CST), a 1.5m telescope were SCIDAR is installed). Figure 6. Left: Example of one night measurements taken with SCIDAR attached to the CST at Izaña. Right: Example of one night measurements taken with SCIDAR attached to the JKT (1m) at ORM (La Palma). 3.2 G-SCIDAR G-SCIDAR technique allows to measure the strength of the optical turbulence (CN2) as well as the velocity of the turbulent layers as a function of the height and time. This technique is based on the variance of the scintillation produced by turbulent layers on the light from a binary system. Since the technique was first proposed (Azouit & Vernin 1980; Vernin & Azouit 1983) it has been improved thanks to many efforts led by Jean Vernin and related teams. For a general description and application of SCIDAR and generalized SCIDAR technique see the compilation by Avila et al., Although several SCIDAR campaigns have already been carried out at several astronomical sites, the available data have not still statistical significance. With the initial aim to get a statistics of the turbulent profiles at Teide Observatory and La Palma a prototype has been developed in a collaboration IAC (Fuensalida) & Fizeau (Vernin). The instrument has been developed and tested using the IAC 1.5m, CST at Izaña (see Figure 5) and some results are shown in Figure 6. In Figure 6, an example of one night measurements of turbulence profiles is shown. Data are gathered with the IAC-Fizeau SCIDAR attached to the CST (1.5m) at Izaña. For further details read Fuensalida et al., The blue ribbon in the bottom of the figure is the signature of the dome and mirror turbulence. As one can see
7 the turbulence in this particular night seems to be concentrated in the boundary layer (below one km). Note that the altitude is referred to the sea level and the observatory is located at 2400m (the location of the most intense blue ribbon). Although they vary along the nigh, one can note also the persistence of the layers all along the night. Also important is the number of layers, two or three in this case if we ignore the boundary layer and dome seeing contribution. On top of the figure 6, the integrated average seeing value along the whole night is As above mentioned, the vertical distribution of the layers at different heights is crucial for the AO designs and will, among other things like the isoplanatic angle or the coherence time, be obtained on longer temporal data bases at Paranal and La Palma within the FP6 site characterization program. Further tests have been carried out at La Palma making use of the 1m JKT (see Fig. 6). Two reasons are behind that: First to see whether a 1m telescope size is sufficient to get turbulence profiles or not, and having proved so, to be able to get statistic with SCIDAR at La Palma. A huge effort has been made to improve the instrument, to make it easier to use and simpler to process the data. A friendly version of the G-SCIDAR is now finished at the Instituto de Astrofísica de Canarias (IAC) in collaboration with Nice University. The instrument is to be duplicated and delivered soon to Paranal where it will be attached to one of the Auxiliary telescope in July For details of the instrument and results at OT and ORM see Fuensalida et al., When installed, systematic observations will be carried out at Paranal. The present status of G-Scidar instruments developed under FP6 contract is summarized as follows: Scidar at ORM already operating at the JKT. Scidat at Izaña (Tenerife) in opeartion at Carlos Sanchez Telescope. Scidar for Paranal finished. Control design reviewed. Feasibility to provide Cn2(h) in real time finished. Commissioning done at Paranal in After successful commissioning at Paranal, the G-Scidar was used during two campaigns at the focus of one of tha Auxiliary Telescopes, as seen in Fig. 7. The use of SCIDAR requires all the infrastructure associated with already existing observatories. This is not the case for some of the alternative sites, like in Morocco and Argentina. The solution is to use a MASS/DIMM. 3.3 Multi Aperture Scintillation Sensor (MASS) This instrument detects fast variations of light in 4 concentric apertures using photo-multipliers. The 1-ms photon counts accumulated during 1 min. are converted to 4 normal scintillation indices and to 6 differential indices for each pair of apertures. This set of 10 numbers is fitted by a model of 6 thin turbulent layers at pre-defined altitudes of 0.5, 1, 2, 4, 8, and 16 km above the site (See Tokovinin, 2003). Another model of 3 layers at floating altitudes is fitted as well. Turbulence integrals J i in these 6 (or 3) layers represent the OTP measured by MASS. Turbulence near the ground does not produce any scintillation: MASS is blind to it and can only measure the seeing in the free atmosphere. MASS has been cross compared with the G-Scidar during a campaign performed at Mauna Kea (See Tokovinin, Vernin et al., 2005). 3.4 Single Star Scidar As seen in section 3.2, the G-Scidar analyses the scintillation of a double star and needs a 1-2m telescope, which implies the restriction of its use in large astronomical facilities. To overcome this limitation, we proposed the Single Star Scidar technique based on the scintillation analysis of a single star (see principle in Fig. 8, left. Habib, Vernin et al, 2006, applied this technique using moderate to large telescope. More recently, within the framework of the ELT-DS, we shown the feasibility of the SSS with smaller telescope of 40 cm. It was designed, constructed and put into operation at Nice observatory. A copy of the same instrument is working at Dome C, as seen in Fig. 8, right.
8 Figure 7. Left: AT4 with the IAC Cute SCIDAR instrument and its dedicated UROS. Right: Example of the IAC Cute SCIDAR graphical interface, where the profiles along time with and without dome seeing effects are represented. Bottom: The first turbulence profiles obtained in real time with the cute-scidar/paranal (developed by the IAC) are received with celebrations during the tests carried out in november, 2007, at the Paranal Observatory and which led to ESO s acceptance of the instrument. The photo shows part of the IAC-SCIDAR team (Jesus J. Fuensalida, Hector Vazquez and Jose Miguel Delgado ) with ESO staff, who assisted during the campaign.
9 Figure 8. Left: SSS principle. Right: SSS prototype in operation at Dome C. The same instrument is installed at Observatoire de la Côte d Azur in the framework of ELT-DS. Figure 9. Behavior of the phase structure function D S(ρ) with baseline ρ 4. LARGE SCALE ATMOSPHERIC PROPERTIES Our knowledge of the outer scale is still very poor and when one imagines to construct telescopes larger than say 40m, it becomes important to know the statistical spatial coherence of the turbulence at such large baseline. The problem therefore is to define relative importance of possible wavefront distortion at 50/100m scale, when the diameter of the telescope might be larger that the outer scale (D L0) The task is to identify the relevant theory and experiments which give the trend of wavefront perturbations at spatial scales of the order of the telescope diameter. The starting point was to check for the saturation of the phase structure function at large baseline. It is known that this function behaves like a Kolmogorov trend like D S (ρ) ρ 5/3 at small baseline B < Lo, where Lo is the outer scale of the optical turbulence. But, when B Lo, the phase structure function begins to saturate, as shown in Fig. 9 (See Coulman & Vernin, 1991). But, from the same authors, it is possible that for very large baseline the phase structure function might increase again. This point is very important for AO applicability for ELTs. After discussions and meetings it was decided to coordinate two multiple instruments intensive campaigns at the top sites considered, ORM at La Palma and Paranal, taking benefit of existing telescopes, interferometers
10 Figure 10. Left: Seen from a single star, one can probe four 8 m wave front. Right: Seen from many stars within a 8 arcmin field of view, at 45 degrees from zenith and for a layer moving at 10 km altitude, one can notice that each pupil is larger and they begin to overlap, allowing a full reconstruction of the wavefront over 100 m. Figure 11. LIDAR experiment of Universidad Politecnica de Cataluña, Barcelona. and dedicated instruments, and using two large field wavefront sensors (Due to budget cut, it was not possible to construct four devices). In order to achieve this task, it was decided to construct a Wide Field Wave Front Sensor proposed by R. Ragazzoni (INAF, Italy) who is co-responsible of this WP. To be short, the idea is to sense wavefront distortion within a wide field of view, using a set of Shack-Hartman devices, each one working on various stars in the field of view. In Fig. 10(left) one can see that with a single star, only 8 m portion of the wavefront is attainable. But, if one combine a large field of view with a slant beam and at 10 km altitude, as shown in Fig. 10(right), the full reconstruction of the wavefront is possible over a 100 m baseline. Besides, we count with the participation of Adolfo Comeron group, from the Universidad Politécnica de Barcelona, which will be in charge of the boundary layer studies by using a portable LIDAR to be used in intensive campaigns, both at ORM and Paranal (see Fig. 11)
11 Table 2. Instruments considered for data analysis within the FP6 ELT DS Site Characterization project. A/R means respectively Automatic/Robotic. Instrument/tool ORM (La Palma) N-Paranal Izaña Aklim (Atlas) Macon GS Y Y Y N N SSS MASS/DIMM Y Y Y Y Y R-mount Y N N N N A-mount N Y Y Y Y ASC Y Y Y Y Y Sat. for aerosols Y N Y Y Y AWS Y Y Y Y Y BL profilers Y Y N N N Climatology (satelites) Y Y Y Y Y Meteo Models Y Y Y Y Y Soil Mechanics N Y N Y Y Sismicity N Y N Y Y 5. SUMMARY Within the FP6-ELT Design Study contract, the site characterization is being carried out within a specify Working Group. The Site Characterization WG has defined a strategy based on an intensive characterization of two reference observatories, Paranal (Chile) and ORM (La Palma- Spain). The first one was selected after various campaigns carried out in the nineteens and now it hosts the ESO VLT. The second one, ORM, is a site under investigation since a long time ago and provides very good values in all parameters recognized as important for astronomical observations. Besides, alternative sites are explored: Ventarrones (Chile), Macon (Argentina) and Aklim (Morrocan Anti Atlas). The alternative candidates will be compared with the two reference ones with the same criteria. We are aware that other teams are carring out similar studies. In particular the TMT (30m) is leading a similar strategy with almost the same instrumentation and tools and centred on candidates situated in America. For this reason and in order to concentrate our resources, excellent sites like Hawaii are not included in our work. Cerro Tololo as well as San Pedro Mártir are potential very good alternative but are not included in the ELT DS framework, but are studied by the TMT team. Two generalized SCIDAR have been designed at developed at the IAC workshops. One is already attached at the 1m. JKT telescope at La palma and the other is planned to be installed at one of the VLT auxiliary telescopes at Paranal. Four MASS-DIMMs have been developped, tested and used (see e.g. a MASS-DIMM instaled at Ventarrones. New techniques have been explored (e.g. SSS) and the use of global climatic models and satelites data are discussed (see Muñoz-Tuñón and Varela et al., 2007). Large effort is devoted on validating these techniques, crosscompare them, and in summary in order to, at the end, be able to supply a battery of relible instruments and tools for future use (see Table 2). By the end of 2008 a report with all the deliverables of the project will be produced and we plan also to organize a sientific meeting for making public our experiences, achievments, problems, results, instruments, techniques. ACKNOWLEDGMENTS This work has been funded by European Community under contract number ELT Design Study. We are endebted to the local scientific teams in Morocco, Pr. Zouhair Benkhaldoun of Marrakesh University and in Argentina D. Garcia Lambas, H. Muriel and Pablo Recabarren. We wish to thank particularly Marcos Reyes, project manager at IAC, who also contributes to the coordination of the three institutes, IAC-ESO-UNI.
12 REFERENCES  Avila R., L. J. Sánchez, F. Ibañez, J. Vernin, E. Masciadri, M. Azouit, A. Agabi and S. Cuevas, 2007, RevMexAA, 31,  Azouit M. & Vernin J., 1980, J. Appl. Meteorol., 19, 833  Azouit M.& Vernin J., 2005, PASP, 117, 536.  Coulman C.& Vernin J., 1991, Appl. Opt., 30, 118.  Ehgamberdiev S., Baijumanov, A. K., Ilyasov, S. P., Sarazin, M., Tillayev, Y. A., Tokovinin, A. A., Ziad, A., 2002, A&A Suppl. Ser., 145, 293.  Fuensalida J., B. García-Lorenzo, J. M. Delgado, M. A. C. Rodríguez-Hernández and J. Vernin, 2007, RevMexAA, 31,  Habib A., Vernin J. et al., 2006, MNRAS, 368,  Muñoz-Tuñón C., Vernin J. and Varela A., 1997, A&AS, 125, 183.  Muñoz-Tuñón C., Varela A. and Fuensalida J., 2007, RevMexAA, 31,  Sarazin & Roddier, 1990, A&A, 227, 294  Schöck M., R. Riddle, W. Skidmore, T. Travouillon and the TMT Site Selection Team, 2007, RevMexAA, 31,  Tokovinin A.,Kornilov, V., Shatsky, N. and Voziakova, O., 2003, MNRAS, 343, 891  Tokovinin A., Vernin J., Ziad A. and Chun M., 2005, PASP, 117, 395  Varela A., C. Bertolin, C. Muñoz-Tuñón, J. J. Fuensalida and S. Ortolani, 2007, RevMexAA, 31,  Vernin J.& Azouit M., 1983, Journal of Optics, 14, 131  Vernin J. & Muñoz-Tuñón C., 1992, A&A, 257, 811  Vernin J.& Muñoz-Tuñón C., 1994, A&A, 284, 311  Vernin J.& Muñoz-Tuñón C., 1995, PASP, 107, 265  ESO workshop on Site Testing for Future Large Telescopes 1983, eds A. Ardeberg & L. Woltjer.  Vistas in Astronomy, The Observatories of the Canaries Vol. 28, 1985, Murdin & Beer eds.  Identification, Optimisation and Protection of Optical Telescopes Sites, 1986, Flagstaff.  VLT site selection working group; final report (no. 62), 1990 Sarazin, M., eds.  Site properties of the Canarian Observatories New Astron. Reviews, vol 42, 1998, Muñoz-Tunñón, C., eds.  SITE2000/ IAU technical workshop. Astronomical Site Evaluation in the Visible and Radio Range ASP, vol 266, 2002, Vernin, J, Benkhaldoun and Z & Muñoz-Tuñón, C., eds.
Statistical Vertical Turbulence Profiles at the Canary Islands Astronomical Sites B. García-Lorenzo 1, J.J. Fuensalida 1, J. Castro-Almazán 1, & M.A.C. Rodríguez-Hernández 1 (1) Instituto de Astrofísica
Remote sensing of precipitable water vapour and cloud cover for site selection of the European Extremely Large Telescope (E-ELT) using MERIS H. Kurlandczyk 1 M.Sarazin 1 1 European Organisation for Astronomical
Calibration of the MASS time constant by simulation A. Tokovinin Version 1.1. July 29, 2009 file: prj/atm/mass/theory/doc/timeconstnew.tex 1 Introduction The adaptive optics atmospheric time constant τ
ESO ELT Basic Reference Design 1 st Phase (Jan.-April 2006) ESO/Community Working Groups WG3 - ELT Site Evaluation Working Group Final Report 13 April 2006 Chair: Roland Gredel email@example.com Deputy Chair:
Mon. Not. R. Astron. Soc. 340, 5 58 (003) Statistics of turbulence profile at Cerro Tololo A. Tokovinin, S. Baumont and J. Vasquez Cerro Tololo Inter-American Observatory, Casilla 603, La Serena, Chile
HST-Like Performance from Balloon-borne Telescopes Eliot F. Young Southwest Research Institute Main goal of talk is to describe the near-space environment at 120,000 ft. Imaging: what is the seeing quality?
Chapter 6 Telescopes: Portals of Discovery 6.1 Eyes and Cameras: Everyday Light Sensors Our goals for learning:! How does your eye form an image?! How do we record images? How does your eye form an image?
Introduction to atmospheric speckle Dr Nicolas Védrenne High Angular Resolution Unit, Optical Department, ONERA BP 72, 29 avenue de la division Leclerc 92322 Châtillon Cédex Mail: firstname.lastname@example.org
Agreement on Cooperation in Astrophysics The Government of the Kingdom of Spain, the Government of the Kingdom of Denmark, the Government of the United Kingdom of Great Britain and Northern Ireland and
Name of research institute or organization: École Polytechnique Fédérale de Lausanne (EPFL) Title of project: Study of atmospheric ozone by a LIDAR Project leader and team: Dr. Valentin Simeonov, project
RESULTS FROM A SIMPLE INFRARED CLOUD DETECTOR A. Maghrabi 1 and R. Clay 2 1 Institute of Astronomical and Geophysical Research, King Abdulaziz City For Science and Technology, P.O. Box 6086 Riyadh 11442,
Housing of Robotic Telescopes Hosting www.e-eye.es 2 Entre Encinas y Estrellas HOSTING AND HOUSING OF ROBOTIC TELESCOPES e-eye has built modular observatories with cutting edge technology that can be controlled
Supercool Space Tools! By Linda Hermans-Killam A long time ago, people looked into the dark night sky and wondered about the stars, meteors, comets and planets they saw. The only tools they had to study
STATEMENT OF WORK FOR DESIGN, FABRICATION, INTEGRATION AND TESTING OF THE TELESCOPE STRUCTURE SYSTEM TMT.STR.MGT.12.001.REL01 27 July, 2012 TMT.STR.TEC.12.001.DRF01 Page 2 of 13 Table of Contents 1. INTRODUCTION
STUDY OF ABSORPTION FEATURES OF THE MARS Ratna K. Bade*, Prem R. Dhungel*, Udayaraj Khanal** and S.R. Shahi*** *** Abstract Keywords INTRODUCTION or the planet across which our modern robots trundle of
Accurate Determination of the TOA Solar Spectral NIR Irradiance Using a Primary Standard Source and the Bouguer-Langley Technique. D. Bolsée, N. Pereira, W. Decuyper, D. Gillotay, H. Yu Belgian Institute
RevMexAA (Serie de Conferencias), 31, 25 29 (2007) SITE-TESTING IN ANTARCTICA J. W. V. Storey, 1 J. S. Lawrence, 1 and M. C. B. Ashley 1 RESUMEN Los sitios en el Plateau de la Antártica como el Domo A,
Observing Fog And Low Cloud With A Combination Of 78GHz Cloud Radar And Laser Met Office: Darren Lyth 1, John Nash. Rutherford Appleton Laboratory: M.Oldfield ABSTRACT Results from two demonstration tests
P1.7 INVESTIGATION OF ATMOSPHERIC AEROSOL WITH MULTIWAVELENGTH LIDAR G. Karasinski, T. Stacewicz, S.Chudzynski, W. Skubiszak, S. Malinowski 1, A. Jagodnicka Institute of Experimental Physics, Warsaw University,
WORLD METEOROLOGICAL ORGANIZATION COMMISSION FOR INSTRUMENT AND METHODS OF OBSERVATION OPAG-UPPER AIR EXPERT TEAM ON REMOTE SENSING UPPER-AIR TECHNOLOGY AND TECHNIQUES First Session Geneva, Switzerland,
European Solar Telescope: Perspectives for the coming years M. Collados Instituto de Astrofísica de Canarias 2007: EAST Consortium formed EAST: European Association for Solar Telescopes AIM (among others):
Recent Observations of the solar corona with a new ground-based coronagraph in Argentina (MICA) G. Stenborg, R. Schwenn, N. Srivastava, B. Inhester, B. Podlipnik Max-Planck-Institut für Aeronomie Max-Planck-Str.
PHYS 320 Lecture 6 Optics and Telescopes Jiong Qiu MSU Physics Department Wenda Cao NJIT Physics Department Guiding Questions 1. Why is it important that telescopes be large? 2. Why do most modern telescopes
Dr. Elena Manjavacas Curriculum Vitae Max-Planck-Institut für Astronomie Königstuhl, 17 D-69117, Heidelberg, Germany +49 6221 528 442 email@example.com www.mpia.de/homes/manjavacas/elena_manjavacas.html
ADM-Aeolus pre-launch campaigns with an airborne instrument demonstrator Oliver Reitebuch Institut für Physik der Atmosphäre Background The ADM-Aeolus instrument ALADIN uses several novel techniques, like
High Resolution Imaging in the Visible from the Ground without Adaptive Optics: New Techniques and Results Craig Mackay *a, John Baldwin b, Nicholas Law a and Peter Warner b a Institute of Astronomy and
COMPARISON OF LIDARS, GERMAN TEST STATION FOR REMOTE WIND SENSING DEVICES A. Albers, A.W. Janssen, J. Mander Deutsche WindGuard Consulting GmbH, Oldenburger Straße, D-31 Varel, Germany E-mail: firstname.lastname@example.org,
German Test Station for Remote Wind Sensing Devices A. Albers, A.W. Janssen, J. Mander Deutsche WindGuard Consulting GmbH, Oldenburger Straße, D-31 Varel, Germany E-mail: email@example.com, Tel: (++9)
Twilight phenomena of Venus P. Tanga Laboratoire Lagrange Observatoire de la Côte d Azur Th. Widemann, B. Sicardy LESIA Observatoire de Paris Sakura/Europlanet workshop Paris, March 6 2012 The «ring of
Early CMB anisotropy measurements Rod Davies Jodrell Bank Centre for Astrophysics The University of Manchester Anthony Lasenby came into the CMB field at an exciting time. The 3K radiation had been decisively
Ionospheric Research with the LOFAR Telescope Leszek P. Błaszkiewicz Faculty of Mathematics and Computer Science, UWM Olsztyn LOFAR - The LOw Frequency ARray The LOFAR interferometer consist of a large
SATELLITE USES FOR PURPOSE OF NOWCASTING Kedir, Mohammed National Meteorological Agency of Ethiopia Introduction The application(uses) of satellite sensing data deals to obtain information about the basic
6.4 THE SIERRA ROTORS PROJECT, OBSERVATIONS OF MOUNTAIN WAVES William O. J. Brown 1 *, Stephen A. Cohn 1, Vanda Grubiši 2, and Brian Billings 2 1 National Center for Atmospheric Research, Boulder, Colorado.
The Moon Nicola Loaring, SAAO Vital Statistics Mean distance from Earth Orbital Period Rotational Period Diameter 384,400 km 27.322 days 27.322 days 3476 km (0.272 x Earth) Mass 7.3477 10 22 kg (0.0123
AMIGO Memorandum of Understanding (August 15, 1998) Memorandum of Understanding among L École Mohammadia d'ingénieurs, Université Mohamed V, Morocco (EMI); A Faculdade de Ciências da Universidade de Lisboa,
Evaluation of a Fully Coupled Atmospheric Hydrological Modeling System for the Sissili Watershed in the West African Sudanian Savannah Titelmasterformat durch Klicken June, 11, 2014 1 st European Fully
The Next Generation Science Standards (NGSS) Achieve, Inc. on behalf of the twenty-six states and partners that collaborated on the NGSS Copyright 2013 Achieve, Inc. All rights reserved. Correlation to,
SEASONAL VARIATIONS OF SURFACE SOLAR IRRADIANCES UNDER CLEAR-SKIES AND CLOUD COVER OBTAINED FROM LONG-TERM SOLAR RADIATION MEASUREMENTS IN THE RONDONIA REGION OF BRAZIL T.A. Tarasova, and C.A.Nobre Centro
Speckle Imaging with the SOAR and the Very Large Telescopes Sridharan Rengaswamy, Julien. H. Girard and Guillaume Montagnier European Southern Observatory, Casilla 19001, Vitacura, Santiago, Chile ABSTRACT
Making a reflector telescope telescope built by Sir Isaac Newton Replica of the first reflector Nowadays, professional astronomers use another type of telescope that is different to the first telescope
Hyperspectral Satellite Imaging Planning a Mission Victor Gardner University of Maryland 2007 AIAA Region 1 Mid-Atlantic Student Conference National Institute of Aerospace, Langley, VA Outline Objective
Star Party Introduction Materials Where to observe What to do Observation Sheets Turn in (list) Describing the Equipment Binoculars Telescopes Introduction You will attend a star party where lots of telescopes
FRACTAL S.L.N.E A private company for engineering of scientific projects Instrumentation and Software for Astronomy 1 Introducing FRACTAL FRACTAL S.L.N.E. is a private technological company funded in 2005.
Ján Kaňák Slovak Hydrometeorological Institute Jan.firstname.lastname@example.org Overview of the IR channels and their applications EUMeTrain, 14 June 2011 Ján Kaňák, SHMÚ 1 Basics in satellite Infrared image interpretation
Teaching Astronomy in the University of Granada Eduardo Battaner Departamento de Física Teórica y del Cosmos Some history University created by Charles V in the XVI century (An arabic Madraza was created
Assessing Cloud Spatial and Vertical Distribution with Infrared Cloud Analyzer I. Genkova and C. N. Long Pacific Northwest National Laboratory Richland, Washington T. Besnard ATMOS SARL Le Mans, France
Education and Outreach Lesson Plan Visit our online activities collection http://education.arm.gov/ Grade levels K 2 Common Covering Clouds Common Covering Clouds Approximate Time 1 1/2 hours, or two 45-minute
WORLD METEOROLOGICAL ORGANIZATION COMMISSION FOR BASIC SYSTEMS OPEN PROGRAMME AREA GROUP ON INTEGRATED OBSERVING SYSTEMS EXPERT TEAM ON REQUIREMENTS FOR DATA FROM AUTOMATIC WEATHER STATIONS Third Session
Long-term Observations of the Convective Boundary Layer (CBL) and Shallow cumulus Clouds using Cloud Radar at the SGP ARM Climate Research Facility Arunchandra S. Chandra Pavlos Kollias Department of Atmospheric
Proposals of Summer Placement Programme 2015 Division Project Title Job description Subject and year of study required A2 Impact of dual-polarization Doppler radar data on Mathematics or short-term related
Space-based vs. Ground-based telescopes with Adaptive Optics (AO) 1 Advances in technology make it possible to partially correct the wavefront errors caused by the Earth s atmosphere that blur ground-based
Select the be answer on the answer sheet. Please do not make any marks on this te. 1. Weather is be defined as the A. changes that occur in cloud formations from day to day. B. amount of rain or snow that
Image classification of night time images detected from the International Space Station Alejandro Sánchez de Miguel, José Gómez Castaño and Jaime Zamorano Calvo. Universidad Complutense de Madrid. Image
Weather Radar Basics RADAR: Radio Detection And Ranging Developed during World War II as a method to detect the presence of ships and aircraft (the military considered weather targets as noise) Since WW
Chapter 3 Telescopes Units of Chapter 3 Optical Telescopes Telescope Size High-Resolution Astronomy Radio Astronomy Other Astronomies 3.1 Optical Telescopes Images can be formed through reflection or refraction
CHANGE OF AIR TEMPERATURE WITH ALTITUDE, ATMOSPHERIC STABILITY AND AIR POLLUTION Vertical motion of air governs many atmospheric processes, such as the formation of clouds and precipitation and the dispersal
Realization of a UV fisheye hyperspectral camera Valentina Caricato, Andrea Egidi, Marco Pisani and Massimo Zucco, INRIM Outline Purpose of the instrument Required specs Hyperspectral technique Optical
California Standards Grades 912 Boardworks 2009 Science Contents Standards Mapping Earth Sciences Earth s Place in the Universe 1. Astronomy and planetary exploration reveal the solar system s structure,
Introduction to Plate Tectonic Theory, Geodesy, and VLBI The plate tectonic theory is a relatively new, accepted only around 50 years ago. The following website contains a more detailed and lesson plans
Atmosphere-like turbulence generation with surface-etched phase-screens Stefan Hippler, Felix Hormuth, David J. Butler, Wolfgang Brandner, and Thomas Henning Max-Planck-Institut für Astronomie Königstuhl
Light Telescopes Grade Level: 5 Time Required: Suggested TEKS: Science - 5.4 Suggested SCANS Information. Acquires and evaluates information. National Science and Math Standards Science as Inquiry, Earth
Traffic Management Systems with Air Quality Monitoring Feedback Phil Govier City & County of Swansea The Swansea Project - what are we trying to achieve? Develop a working traffic emissions forecast model
Institute for Astronomy Instrumentation Capabilities and Recent Projects Klaus Hodapp for the IfA Instrumentation Division The distributed IfA The distributed IfA IfA Manoa IfA Kula Haleakala Mauna Kea
Generated using V3.0 of the official AMS LATEX template Evaluations of the CALIPSO Cloud Optical Depth Algorithm Through Comparisons with a GOES Derived Cloud Analysis Katie Carbonari, Heather Kiley, and
COMPUTING CLOUD MOTION USING A CORRELATION RELAXATION ALGORITHM Improving Estimation by Exploiting Problem Knowledge Q. X. WU Image Processing Group, Landcare Research New Zealand P.O. Box 38491, Wellington
How Will ALMA Make Images? Credit: ALMA (ESO / NAOJ / NRAO), Cynthia Collao (ALMA). The invention of the optical telescope by Galileo 400 years ago marked the beginning of modern astronomy. Galileo used
Top 10 Discoveries by ESO Telescopes European Southern Observatory reaching new heights in astronomy Exploring the Universe from the Atacama Desert, in Chile since 1964 ESO is the most productive astronomical
CFHT, Instruments, Queue Scheduling Queued Service Observations with MegaPrime Phase 1 Proposal Submission for Semester 2010A Updated 08/24/09 Table of Contents A - Introduction The QSO Project Document
Climatology of aerosol and cloud properties at the ARM sites: MFRSR combined with other measurements Qilong Min ASRC, SUNY at Albany MFRSR: Spectral irradiances at 6 six wavelength passbands: 415, 500,
Collaborating with professional amateurs: low-mass stars in fragile multiple systems José Antonio Caballero 1 Joan Genebriera 2, Tòfol Tobal 3, F. Xavier Miret 3, Francisco M. Rica 4, Jordi Cairol 3, Núria
NOAA ESRL TOLNet Lidar The Tunable Optical Profiler for Aerosols and ozone (TOPAZ) 3-wavelength mobile differential absorption lidar (DIAL) system can profile O 3 and aerosol layers from near the surface
ACE Automated Soil CO 2 Exchange System Automated operation Automatically exposes soil area between measurements CO 2 analyser in chamber Highly accurate CO 2 IRGA housed directly inside soil chamber assembly
Observer Access to the Cherenkov Telescope Array IRAP, Toulouse, France E-mail: email@example.com V. Beckmann APC, Paris, France E-mail: firstname.lastname@example.org C. Boisson LUTh, Paris, France E-mail:
13 CHAPTER TWO SOME CONCEPTS IN CLIMATOLOGY 2.1 The Adiabatic Process An important principle to remember is that, in the troposphere, the first layer of the atmosphere, temperature decreases with altitude.
GLORIA is funded by the European Union 7th Framework Programme (FP7/2007-2013) under grant agreement n 283783 Specification and source code CODE: DEL-050 VERSION: 01 DATE: November 28 th, 2012 Authors:
Chapter 6 - Cloud Development and Forms Understanding Weather and Climate Aguado and Burt Interesting Cloud 1 Mechanisms that Lift Air Orographic lifting Frontal Lifting Convergence Localized convective
Grade 6 Standard 3 Unit Test A Astronomy Multiple Choice 1. The four inner planets are rocky and small. Which description best fits the next four outer planets? A. They are also rocky and small. B. They
Wind Energy Technology Platform Working Group 1: Wind Energy Resource Presented by Ignacio Martí CENER email@example.com Authors: wg1 participants WG1 Participants Erik Lundtang Petersen (Chairman) Risø
Expert System for Solar Thermal Power Stations Institute of Technical Thermodynamics Stuttgart, July 2001 - Expert System for Solar Thermal Power Stations 2 Solar radiation and land resources for solar
Solar Resource & Radiometry Tasks in Antofagasta, Ph.D. firstname.lastname@example.org Mauricio Trigo, Mg. Tania Varas, Mg. Antofagasta, January 14nd, 2015 Index Introduction to Solar Radiation Measurements Climates
Dr. Elena Manjavacas Curriculum Vitae Instituto de Astrofísica de Canarias C/ Vía Láctea s/n C.P. 38205, San Cristóbal de La Laguna, Tenerife, Spain +34 657478751 email@example.com www.mpia.de/homes/manjavacas/elena_manjavacas.html