Posts made by Caefix

For me it works fine with Andro 14 (Samsung S7), but not with 8.1 (S. A7).
Tried 42.5.5 and Browser (DuckDuckGo). Only grey map, no time-bar.

@Seapig57 Maybe You toggeled the switch?

@David-Polášek Other layers use arrow keys for a defined step. Maybe horizontal to shift left/both bars, vertical for the right?

@vujacicm https://en.wikipedia.org/wiki/Geopotential_height
https://en.wikipedia.org/wiki/Pressure_altimeter

@Browndog1 🏭 Have You tried the air-quality switch?

📸 Photographic Firsts in Cyclone History

@forsbergdk There are archives for radar & satellite only.

@NurlG Yes, I also miss those features every day several times...

@ronaldjarush Have You tried to log in?

🛰 🌎

@pavelneuman 🌪🦘 Australian Tornadoes

@vujacicm 🚬🎈 https://en.wikipedia.org/wiki/Equivalent_potential_temperature

@ortlepp It´s the track of radar-forecast, the red part of the time-line.

@vujacicm 🏔🎈 https://www.weather.gov/source/zhu/ZHU_Training_Page/convective_parameters/skewt/skewtinfo.html

From there in Skew-T FAQs 3)

While potential temperature can be used to compare temperatures at different elevations and the trajectory air parcels will take (rising or sinking), equivalent potential temperature can be used to compare BOTH moisture content and temperature of the air. The equivalent potential temperature (or Theta-e as it is usually called) is found by lowering an air parcel to the 1000 mb level AND releasing the latent heat in the parcel. The lifting of a parcel from its original pressure level to the upper levels of the atmosphere will release the latent heat of condensation and freezing in that parcel. The more moisture the parcel contains the more latent heat that can be released. Theta-e is used operationally to map out which regions have the most unstable and thus positively buoyant air. The Theta-E of an air parcel increases with increasing temperature and increasing moisture content. Therefore, in a region with adequate instability, areas of relatively high theta-e (called theta-e ridges) are often the burst points for thermodynamically induced thunderstorms and MCS's. Theta-e ridges can often be found in those areas experiencing the greatest warm air advection and moisture advection. For more information on Theta-e, consult Chaston's book "weather maps" used in the Synoptic I (starting on page 127).

@Conrad-Nutschan ⚡ Hopefully not.
It´s the thunderstorm layer, means lightnings, not liters.

@vujacicm In global scale a topic is the transport of heat in moisture from the aequator towards the poles. Remember winterstorm "Ingunn". The airmass originated near Galapagos islands, passed Popocatepetl, brought record windgusts to Norway and ended up in the polar vortex, causing a "sudden stratospheric warming".

@John-Kenneth-2 You can change the units...

Btw. 🟣 Purple is mostly a hail-indicator,

@John-Kenneth-2 said in Weather Radar:

... in my place it is raining but in weather radar not showing in my place its raining? Why does matter? thank you!

(Maybe living in India?)