A link will be sent to all applicants after submission to AADSAS. There, you will pay the non-refundable application fee ($125.00 USD) and upload a photo of yourself. After review, if invited for an interview, applicants will be immediately required to complete Kira and Casper (Casper test only) online assessments. Completion is mandatory and must be completed within the time frame given in the interview invitation. Applicants do NOT need to complete the Casper test unless they are invited for an interview.

Data Profiles contain the most popular social, economic, housing, and demographic data for a single geographic area. The Data Profiles summarize the data, providing both estimates and percentages, to cover the most basic data on all ACS topics. Click on a link below to view these profiles on data.census.gov. From there, you can select Customize Table to select your geography and product (or data set) of interest.


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When your archive is created by using one of these options, we'll email you a link to its location. Depending on the amount of information in your account, this process could take from a few minutes to a few days. Most people get the link to their archive the same day that they request it.

Hey all, sorry for the noob post, but hey, I AM a noob so there it is! Can anyone provide a link to the working DAT files for the MAME 2015 core and FB Neo. Retroarch errors on the ones I am trying to use, saying something about wrong format (sorry can't be more specific on the error @ work at the mo). Any help appreciated, thanks in advance.

This new version of the vocabulary updates and expands the original but preserves backward compatibility. A full list of the significant changes (with links to the relevent github issues) is described in  D. Change history.

Each RDF example in this document is intended to demonstrate specific capabilities of DCAT, and therefore only shows a subset of all the potential properties and links which might appear in a complete DCAT resource.

:dataset-002 is available as a CSV file. However :dataset-002 can only be obtained through some Web page where the user needs to follow some links, provide some information and check some boxes before accessing the data.

:dataset-004 is distributed in different representations from different services. The dcat:accessURL for each dcat:Distribution corresponds with the dcat:endpointURL of the service. Each service is characterized by its general type using dct:type (here using values from the INSPIRE spatial data service type vocabulary), its specific API definition using dct:conformsTo, with the detailed description of the individual endpoint parameters and options linked using dcat:endpointDescription.

Many existing and legacy catalogs do not distinguish between dataset components, representations, documentation, schemata and other resources that are lumped together as part of a dataset. dct:relation is a super-property of a number of more specific properties which express more precise relationships, so use of dct:relation is not inconsistent with a subsequent reclassification with more specific semantics, though the more specialized sub-properties SHOULD be used to link a dataset to component and supplementary resources if possible.

dct:license, which is a sub-property of dct:rights, can be used to link a distribution to a license document. However, dct:rights allows linking to a rights statement that can include licensing information as well as other information that supplements the license such as attribution.

Example 15 uses adms:schemaAgency and dct:creator to represent the authority that defines the identifier scheme (e.g., the DOI foundation in the example), adms:schemaAgency is used when the authority has no URI associated. The CrossRef and DataCite display guidelines recommend displaying DOIs as full URL link in the form

DCAT 2014 handling of license and rights do not appear to satisfy all requirements [VOCAB-DCAT-20140116]. The recently completed W3C ODRL model [ODRL-MODEL] and vocabulary [ODRL-VOCAB] provide a rich language for describing many kinds of rights and obligations. In this section, we describe some patterns for linking DCAT Datasets and/or Distributions to suitable license and rights expressions.

Finally, in the particular case when rights are expressed via ODRL policies, it is recommended to use the odrl:hasPolicy property as the link from the description of the cataloged resource or distribution to the ODRL policy, in addition to the corresponding [DCTERMS] property that matches the same ODRL policy type.

Several properties capture provenance information, including within the citation and title, but the primary link to a formal description of the project is through prov:wasGeneratedBy. A terse description of the project is shown as a prov:Activity, though this would not necessarily be part of the same catalog. Note that as the project is ongoing, the activity has no end date.

Further provenance information might be provided using the other starting point properties from PROV, in particular prov:wasAttributedTo (to link to an agent associated with the dataset production) and prov:wasDerivedFrom (to link to a predecessor dataset). Both of these complement Dublin Core properties already used in DCAT, as follows:

Often datasets are associated with publications (scholarly articles, reports, etc) and this version of DCAT relies on the property dct:isReferencedBy to provide a way to link publications about a dataset to the dataset

Once we have received your verified/completed AADSAS application, you will receive an email from Ohio State's Office of Graduate and Professional Admissions with the link to the supplemental application if you meet our admissions minimums.

The major data sources are theworldwide network of ionosondes, the powerful incoherent scatter radars(Jicamarca, Arecibo, Millstone Hill, Malvern, St. Santin), the ISIS and Alouette topside sounders, and in situ instruments flown on many satellites androckets. IRI is updated yearly during special IRI Workshops (e.g., during COSPAR general assembly). More informationcan be found in the workshop reports. The IRI model and software is updated according to the decisions of the IRI Working Group. The software package includes the FORTRAN subroutines, model coefficients (CCIR, URSI, IGRF), indices files (IG_RZ.DAT, APF107.DAT) and README and LICENSE files. The IRI build-up and formulas are described in detail in a 158-page NSSDC report by Bilitza (1990) and more recently in a 65-page Reviews of Geophysics paper by Bilitza et al. (2022) (see REFERENCE section). An IRI listserver keeps the community informed about model updates, workshops, publication,and other IRI-related matters. To subscribe send a message to info@irimodel.org with 'subscribe IRI your_email_address' in the SUBJECT line and your name, affiliation and mailing address in the body of the message.PARAMETERS: Electron density, electron temperature, ion temperature, ion composition (O+, H+, He+, N+, NO+, O+2, Cluster ions), equatorial vertical ion drift, vertical ionospheric electron content (vTEC; a user can select the ending height for the integration along the electron density profile), F1 probability, spread-F probability, auroral boundaries, effects of ionospheric storms on F and E peak densitiesINPUTS:Required:  solar indices (F10.7 daily, 81-day, and 12-month running mean; sunspot number 12-month running mean)ionospheric index (ionosonde-based IG index 12-month running mean) magnetic index (3-h ap, daily ap) The indices are found internally from indices files for the user-specified date and time. But a user can also input his/her own indices values if so desired.

 Optional: The user can provide a number of input parameters and the IRI profiles will than be adjusted to these input parameters:F2-peak height (hmF2) or propagation factor M3000F2 F2-peak plasmafrequency (foF2) or electron density (NmF2)Bottomside profile parameters B0 (thickness) and B1 (shape)F1-ledge height (hmF1)F1-ledge plasmafrequency (foF1) or electron density (NmF1)E-peak height (hmE) E-peak plasmafrequency (foE) or electron density (NmE)D-ledge height (hmD) D-ledge plasmafrequency (foD) or electron density (NmD)HEIGHT RANGE:Electron density: daytime: 65-2000km, nighttime: 80-2000km Electron and ion temperature: 60-2500km (IRI-95 option: 60-3000km)Ion composition: 75-2000km (DS95/DY85 option: 80-2000km)  AVAILABILITY: * Fortran source code: IRI-2020 (12/07/2023),IRI-2016 (10/13/2021), IRI-2012, IRI-2007, IRI-2001, COMMON FILES for all versions NOTE: Besides the files that come with each version you also need to download the COMMON FILES and INDICES FILES. NOTE: The IRI output arrays are explained here NOTE: The switches available in the IRI code to turn on/off certain dependencies are explained here* Solar and Magnetic Indices (daily updates, 8:00 EST, provided by David Themens ECHAIM website) apf107.dat ig_rz.dat

* Solar and Magnetic Indices (updated twice a year): INDICES FILES (11/19/2023)* Old indices files can be found hereOnline computation and plotting at CCMC (HELP): IRI-2020, IRI-2016, IRI-2012, IRI-2007 

NOTE: Please consult the HELP file for an explanation of the different inputs, outputs and options.

 NOTE: The program iritest.for can be easily adapted to a specific application.

NOTE: The IRI-2012 distribution also includes iriorbit.for and iriorbitmax.for for calculating IRI parameters along a satellite orbit.

* Real-time IRI foF2 & hmF2: IRTAM IRI Real-Time Assimilative Mappingwith GIRO digisonde data

 * MATLAB version: IRI-2012 

 * pyglow - Python wrappers for IRI-2012 and IRI-2016 

FREQUENTLY ASKED QUESTIONS: FAQRELATED LINKS:

* MIT: Real-time IRI worldmaps and movies (last 24 hours) link

* IPS: Global and Regional Maps of real-time TEC using IRI link * WDC Kyoto: Computation of ionospheric conductivities using IRI90 and CIRA72 modelslink

* SPENVIS: The SPace ENVironment Information System developed by the Belgian Institute for Space Aeronomylink 

 REFERENCES (some can be accessed as PDF documents):List of IRI-dedicated issues of Advances in Space Research K. Rawer, D. Bilitza, and S. Ramakrishnan, Goals and Status of theInternational Reference Ionosphere, Rev. Geophys., 16, 177-181, 1978. K. Rawer, S. Ramakrishnan, and D. Bilitza, International Reference Ionosphere1978, International Union of Radio Science, URSI Special Report, 75 pp.,Bruxelles, Belgium, 1978. K. Rawer, J. V. Lincoln, and R. O. Conkright, International ReferenceIonosphere-IRI 79, World Data Center A for Solar-Terrestrial Physics, ReportUAG-82, 245 pp., Boulder, Colorado, 1981.[PDF] K. Rawer and C. M. Minnis, Experience with and Proposed Improvements of theInternational Reference Ionosphere (IRI), World Data Center A forSolar-Terrestrial Physics, Report UAG-90, 235 pp., Boulder, Colorado, 1984. D. Bilitza (ed.), International Reference Ionosphere 1990, NSSDC 90-22, Greenbelt, Maryland, 1990. [PDF1: pages 0-84, PDF2: pages 85-end] D. Bilitza, K. Rawer, L. Bossy, and T. Gulyaeva, International Reference Ionosphere - Past, Present, Future: I. Electron Density, Adv. Space Res. 13, #3, 3-13, 1993.[PDF] D. Bilitza, K. Rawer, L. Bossy, and T. Gulyaeva, International Reference Ionosphere - Past, Present, Future: II. Plasma Temperatures, Ion Composition, and Ion Drift, Adv. Space Res. 13, #3, 15-23, 1993.[PDF] D. Bilitza and K. Rawer, International Reference Ionosphere, pp735-772, in: The Upper Atmosphere - Data Analysis and Interpretation, W. Dieminger, G. Hartmann and R. Leitinger (eds.), Springer-Verlag Berlin Heidelberg, 1996.D. Bilitza, International Reference Ionosphere - Status 1995/96, Adv. Space Res. 20, #9, 1751-1754, 1997. D. Bilitza, International Reference Ionosphere 2000, Radio Science 36, #2, 261-275, 2001. [PDF]D. Bilitza, International Reference Ionosphere 2000: Examples of improvements and new features, Adv. Space Res. 31, #3, 757-767, 2003.[PDF]B. Reinisch and D. Bilitza, Karl Rawer's life and the history of IRI, Adv. Space Res. 34, #9, 1845-1950, doi:10.1016/j.asr.2004.09.002, 2004.[PDF]D. Bilitza and Reinisch, B., International Reference Ionosphere 2007: Improvements and new parameters, J. Adv. Space Res., 42, #4, 599-609, doi:10.1016/j.asr.2007.07.048, 2008. [PDF]D. Bilitza, B. Reinisch, and J. Lastovicka, Progress in Observation-Based Ionospheric Modeling: Space Weather, 6, S02002, doi:10.1029/2007SW000359, 2008.[online]J. Fernandez, C. Mertens, D. Bilitza, X. Xu, J. Russell III, and M. Mlynczak, Feasibility of developing an ionospheric E-region electron density storm model using TIMED/SABER measurements, Adv. Space Res. 46,#8, 1070-1077, DOI: 10.1016/j.asr.2010.06.008, 2010. [PDF]P. Nsumei, B. Reinisch, X. Huang, and D. Bilitza, Comparing topside and bottomside-measured characteristics of the F2 layer peak, Adv. Space Res.46,#8, 974-983, DOI:10.1016/j.asr.2010.06.027, 2010. [PDF]Y. Zhang, L. Paxton, and D. Bilitza, Near real-time assimilation of auroral peak E-region density and equatorward boundary in IRI, , Adv. Space Res.46,#8, 1055-1063, DOI:10.1016/j.asr.2010.06.029, 2010. [PDF]P. Richards, D. Bilitza, and D. Voglozin, Ion density calculator (IDC): A new efficient model of ionospheric ion densities, Radio Sci., 45, RS5007, doi:10.1029/2009RS004332, 2010.[PDF]D. Bilitza, L.-A. McKinnell, B. Reinisch, and T. Fuller-Rowell, The International Reference Ionosphere (IRI) today and in the future, J. Geodesy, 85:909-920, DOI 10.1007/s00190-010-0427-x, 2011. [PDF]D. Bilitza, Steven A Brown, Matthew Y. Wang, Jonas R. Souza, and Patrick A Roddy, Measurements and IRI Model Predictions during the Recent Solar Minimum, J. Atmos. Solar-Terr. Phys., 86,99-106, doi:10.1016/j.jastp.2012.06.010, 2012. [PDF]I. A. Galkin, B. W. Reinisch, X. Huang, and D. Bilitza, Assimilation of GIRO data into a real-time IRI, Radio Sci., 47, RS0L07, doi:10.1029/2011RS004952, 2012[PDF]D. Bilitza, D. Altadill, Y. Zhang, C. Mertens, V. Truhlik, P. Richards, L.-A. McKinnell, and B. Reinisch: The International Reference Ionosphere 2012 - a model of international collaboration, J. Space Weather Space Clim., 4, A07, 1-12, doi:10.1051/swsc/2014004, 2014.[PDF]D. Bilitza, D. Altadill, V. Truhlik, V. Shubin, I. Galkin, B. Reinisch, and X. Huang, International Reference Ionosphere 2016: From ionospheric climate to real-time weather predictions, Space Weather, 15, 418-429, doi:10.1002/2016SW001593, 2017[PDF]D. Bilitza, IRI the International Standard for the Ionosphere, Adv. Radio Sci., 16, 1-11, -16-1-2018, 2018.A. Fron, A.; Galkin, I.; Krankowski, A.; Bilitza, D.; Hernandez-Pajares, M.; Reinisch, B.; Li, Z.; Kotulak, K.; Zakharenkova, I.; Cherniak, I.; Roma Dollase, D.; Wang, N.; Flisek, P.; Garcia-Rigo, A. Towards Cooperative Global Mapping of the Ionosphere: Fusion Feasibility for IGS and IRI with Global Climate VTEC Maps. MDIP Remote Sens. 2020, 12(21), 3531. , 28 October 2020.I. Galkin; Fron, A.; Reinisch, B.; Hernandez-Pajares, M.; Krankowski, A.; Nava, B.; Bilitza, D.; Kotulak, K.; Flisek, P.; Li, Z.; et al. Global Monitoring of Ionospheric Weather by GIRO and GNSS Data Fusion. Atmosphere 2022, 13, 371. D. Bilitza, Pezzopane, M., Truhlik, V., Altadill, D., Reinisch, B. W., & Pignalberi, A. (2022). The International Reference Ionosphere model: A review and description of an ionospheric benchmark. Reviews of Geophysics, 60, e2022RG000792. ff782bc1db

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