web-based package for ray tracing the neutral atmosphere radiometric path delay (New Brunswick Scientific)
90
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New Brunswick Scientific
web-based package for ray tracing the neutral atmosphere radiometric path delay
Web Based Package For Ray Tracing The Neutral Atmosphere Radiometric Path Delay, supplied by New Brunswick Scientific, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/web-based+package+for+ray+tracing+the+neutral+atmosphere+radiometric+path+delay/web+based+package+for+ray+tracing+the+neutral+atmosphere+radiometric+path+delay/10__1016_slash_j__cageo__2008__02__027-6-16-46
Average 90 stars, based on 1 article reviews
Web Based Package For Ray Tracing The Neutral Atmosphere Radiometric Path Delay, supplied by New Brunswick Scientific, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/web-based+package+for+ray+tracing+the+neutral+atmosphere+radiometric+path+delay/web+based+package+for+ray+tracing+the+neutral+atmosphere+radiometric+path+delay/10__1016_slash_j__cageo__2008__02__027-6-16-46
Average 90 stars, based on 1 article reviews
web-based package for ray tracing the neutral atmosphere radiometric path delay - by Bioz Stars,
2026-10
90/100 stars
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other:Article Title: A web-based package for ray tracing the neutral atmosphere radiometric path delay Article Snippet: An online ray-tracing package has been developed to provide zenith and slant neutral atmosphere delays using RAdiosonde OBservation (RAOB) and numerical weather prediction (NWP) models to users worldwide to assist precise global navigation satellite systems positioning scenarios.. The package includes a web interface, necessary scripts to access RAOB and NWP data, and ray-tracing software capable of using both types of data.. In addition, global maps of zenith hydrostatic delay, zenith non-hydrostatic or wet delay, north–south, east–west and total gradient and comparison maps of the University of New Brunswick climate-based models, and values calculated from NWP models every 3 h are also provided. |