@Danielbraun
Have you looked at the link I provided here above ?
Windy staff say that they know the issue and that they try to find a solution. So that means you cannot fix it yourself.
Good morning,
I'm using Weather Display to transfer data to Windy via station ID and API keys, but it's not working. Here's what it looks like:
https://www.windy.com/station/pws-f06e5c74
What could it be? I also tried Meteobridge, but it still fails. Until a few weeks ago, everything was working fine.
Thanks
Hi @espenas , the inability to add the exact location of cameras is a bug we're aware of, and it should be fixed in the next update. If you send me the camera's identifier (e.g., the URL you enter for it) and the exact latitude and longitude, I'll update the information in the system. You can do it either here, or use mail webcams@windy.com. Thank you!
@timamart
No, that's not possible.
But you can plan two routes.
One to the stopover (WP 1, 2, 3, 4, 5), the other beyond (WP 6, 7, 8) since you can set the departure time as you wish.
Types of Fog
Fog is classified according to the way it forms . Radiation fog also known as Ground fog is very common . it forms over fairly level surfaces on clear , calm humid nights . as surface cools by radiation the adjucent air is also cooled to it's dewpoint (which is the temperature at that air reaches a state where it can't hold any more water vapor) . radiation fog usually occurs in stable air associated with high pressure system .
Advection fog is caused when a low layer of warm , moist air moves over cooler surface . it is most common under cloudy skies along coastlines where air moves from the warm water to the cooler surface of land .
Upslope fog forms when moist , stable air forced up a sloping land mass . like advection fog , upslope fog occure under cloudy skies .
Precipitation _ induced fog may form when warm air or drizzle falls through a layer of cooler air near surface . evaporation from the falling precipitation saturates the cool air causing fog to form . this fog can be very dense and usually it does not clear until the rain moves out of the area .
Steam fog or Sea smoke occurs as cold , dry air moves over comparatively warmer water . it rises upward from the water surface and resembles rising sea smoke . it is composed entirely of water droplets that often freeze quickly and fall back into water as ice particles .
Note : radiation fog is stronger than advection fog . temperture diffrent between dewpoint and environment temperture for fog formation must be less than 2 degree of C(4 degree of F)
Is it possible to get geopotential height lines drawn for different hectopascal levels eg. 850,700,500hPa? Similar to how pressure lines are drwan at sea level
Types of tunderstorms
Tunderstorms usually have similar physical features but their intensity degree of development and associated weather to differ . thay are generally classified as Airmass and Frontal .
Air mass Thunderstorms
Air mass thunderstorms generally form in a warm , moist air and isolated or scattered over large area . they are usually caused by solar heating of the land which results in convection currents that lift unstable air and are most common during summer afternoons or in coastal areas at night . Air mass thunderstorms can also be caused by orographic lifting . although they are usually scattered along individual mountain peaks . they may cover large areas . they may be embedded in other clouds making them difficult to identify when approached from the Windward (the opposite of Lee ward ) side of a mountain . Nocturnal thunderstorms can occure in late spring and summer during the late night or early morning hours when relatively moist air exists aloft . they are usually found from the mississippi valley westward . nocturnal storms cover many square miles and their effects may continue for hours at a given location .
Frontal Thunderstorms
Frontal thunderstorms can be associated with any type of front . those which occure with a warm front are usually obscured by stratiform clouds . you should expect thunderstorms when there is showery precipitation near warm front . in a cold front the cumulonimbus clouds are often visible in a continuous line parallel to the frontal surface .
Note : Squall line is a narrow band of active thunderstorms which normally contains very severe weather and is often forms 50 to 300 miles ahead of front .
Only getting around to this now because electricity was gone for days. Very high impact storm, although it was an Ex-Hurricane. It sure felt like a Hurricane!! High damage across all of Ireland which unfortunately also caused the deaths of 3 people. "The strongest eastern Atlantic hurricane on records" apparently
