![]() ![]() Eclipse Orion: A modern, open source software development environment that runs in the cloud.Terminal for Atom: A simple terminal for the Atom text editor.RStudio: RStudio is an integrated development environment (IDE) for R.Live container-backed terminal uses xterm.js. Next Tech: Online platform for interactive coding and web development courses.Cloud Commander: Orthodox web file manager with console and editor.Spyder Terminal: A full fledged system terminal embedded on Spyder IDE.WebSSH2: A web based SSH2 client using xterm.js, socket.io, and ssh2.Run code in many programming languages, with results displayed by xterm.js. CoderPad: Online interviewing platform for programmers.Codenvy: Cloud workspaces for development teams.Eclipse Che: Developer workspace server, cloud IDE, and Eclipse next-generation IDE.Katacoda: Katacoda is an Interactive Learning Platform for software developers, covering the latest Cloud Native technologies.ttyd: A command-line tool for sharing terminal over the web, with fully-featured terminal emulation based on xterm.js.Microsoft Visual Studio Code: Modern, versatile, and powerful open source code editor that provides an integrated terminal based on xterm.js.SourceLair: In-browser IDE that provides its users with fully-featured Linux terminals based on xterm.js.Xterm.js is used in several world-class applications to provide great terminal experiences. ![]() write ( ' Hello from \ x1B[1 3 31mxterm.js \ x1B[0m $ ' ) Real-world uses Bright reflectivity returns that are stationary and appear during both calm and inclement weather are usually land-based obstructions such as mountains, trees, or especially wind farms (nothing gets electromagnetic signals confused like spinning metal blades!).Var term = new Terminal () term.This is helpful for picking out snow/mix/rain transition zones In all snow situations, dBZ values of 40 indicate 3-4”/hr snowfall rates and whiteout conditions. Anything larger than this is usually due to “bright banding” where the radar is seeing the part of the atmosphere where snowflakes are clumping together and melting into raindrops. In cold climates during the winter months, actual dBZ values rarely exceed 40.This is your standard radar data that shows precip or other solid/liquid particles in the atmosphere. The first type of data currently available is reflectivity. We currently have two types of radar data available with plans to add more soon. Use radar data with caution especially if your area of interest is far from the nearest radar location! A lot can happen between 0 and 5,000 feet and therefore the depiction of precipitation given by radar may differ some from what’s actually happening on the ground. Because of this phenomenon, the radar beam will only see precipitation falling through the mid levels of the atmosphere. To see this in action, imagine a circle (earth) with a straight line emanating from some point on the circle if you continue this line out into space, it will gradually get farther and farther from the circle. Because the earth is round and the radar beam is flat, the farther away from the radar tower the beam (energy) travels, the farther removed from the ground becomes. There is a notable constraint to radar data though. This is the highest resolution radar data available which enables you to see features such as sea breeze or outflow boundaries that standard resolution radar entirely misses. This data is gathered from over a hundred radar towers located across the US. Lake Murray, Ardmore OK (WeatherOK, USA).Lightning CG worldwide (since 2004) Plus. ![]()
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