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Clear

54°F

Updated	2:56 pm
Feels Like	46°F
Humidity	60%
Wind	SSW 6 mph
Barometer	29.99 in
Dew Point	41°F

Clear

12°C

Updated	2:56 pm
Feels Like	8°C
Humidity	60%
Wind	SSW 10 km/h
Barometer	101.5 kPa
Dew Point	5°C

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Cloud Cover	41%
uv UV Index	2
Sunrise	6:57 AM
Sunset	4:52 PM
Moonrise	5:21 AM
Moonset	3:42 PM

Civil Twilight
6:23 AM to 6:54 AM
4:51 PM to 5:22 PM
Welch MN Weather - Waning Crescent Moon

Waning Crescent Moon

Welch Weather Forecast

REST OF TODAY	TONIGHT	SUNDAY	SUNDAY NIGHT	MONDAY	MONDAY NIGHT	TUESDAY	TUESDAY NIGHT	VETERANS DAY	WEDNESDAY NIGHT	THURSDAY	THURSDAY NIGHT

Sunny	Clearing	Sunny	Increasing Clouds	Partly Sunny	Mostly Clear	Sunny	Partly Cloudy	Mostly Sunny	Partly Cloudy	Partly Sunny	Partly Cloudy
Hi: 51°FHi: 11°C	Lo: 40°FLo: 4°C	Hi: 51°FHi: 11°C	Lo: 35°FLo: 2°C	Hi: 59°FHi: 15°C	Lo: 39°FLo: 4°C	Hi: 55°FHi: 13°C	Lo: 39°FLo: 4°C	Hi: 49°FHi: 9°C	Lo: 31°FLo: -1°C	Hi: 41°FHi: 5°C	Lo: 29°FLo: -2°C

POP = Probability of Precipitation.

Weather Outlook Updated: 1258 PM CST Sat Nov 07 2026 Welch, MN Weather - WeatherWorld.com

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Issued: 119 PM CST Sat Nov 7 2026

Key Messages

Mild and dry weather continues into next week with a brief cool spell Wednesday to Friday.

Discussion

... Issued at 119 PM CST Sat Nov 7 2026

Over the next week, we will keep the same general weather pattern in place, which consists of troughs in the eastern Pac and eastern North America, with ridging across the center of the continent. There will be some minor buckles to this pattern over the next week, which will usher in a couple of dry fropas, but otherwise it will result in fairly ...

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Weather 101: Term of the Day

Barotropic System

A weather system in which temperature and pressure surfaces are coincident, i.e., temperature is uniform (no temperature gradient) on a constant pressure surface. Barotropic systems are characterized by a lack of wind shear, and thus are generally unfavorable areas for severe thunderstorm development. See baroclinic zone. Usually, in operational meteorology, references to barotropic systems refer to equivalent barotropic systems - systems in which temperature gradients exist, but are parallel to height gradients on a constant pressure surface. In such systems, height contours and isotherms are parallel everywhere, and winds do not change direction with height. As a rule, a true equivalent barotropic system can never be achieved in the real atmosphere. While some systems (such as closed lows or cutoff lows) may reach a state that is close to equivalent barotropic, the term barotropic system usually is used in a relative sense to describe systems that are really only close to being equivalent barotropic, i.e., isotherms and height contours are nearly parallel everywhere and directional wind shear is weak.