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Clear

43°F

Updated	2:36 am
Feels Like	38°F
Humidity	88%
Wind	N 0 mph
Barometer	30.44 in
Dew Point	40°F

Clear

6°C

Updated	2:36 am
Feels Like	4°C
Humidity	88%
Wind	N 0 km/h
Barometer	103 kPa
Dew Point	4°C

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Cloud Cover	0%
Wind Chill	43°F 6°C
Sunrise	7:44 AM
Sunset	6:47 PM
Moonrise	3:32 PM
Moonset	12:42 AM

Civil Twilight
7:15 AM to 7:41 AM
6:47 PM to 7:14 PM
Star School KY Weather - Waxing Gibbous Moon

Waxing Gibbous Moon

Star School Weather Forecast

OVERNIGHT	MONDAY	MONDAY NIGHT	TUESDAY	TUESDAY NIGHT	WEDNESDAY	WEDNESDAY NIGHT	THURSDAY	THURSDAY NIGHT	FRIDAY	SATURDAY	SATURDAY NIGHT

Fog	Sunny	Fog	Sunny	Clear	Sunny	Clear	Clear	Clear	Clear	Clear	Mostly Clear
Lo: 35°FLo: 2°C	Hi: 65°FHi: 18°C	Lo: 35°FLo: 2°C	Hi: 65°FHi: 18°C	Lo: 39°FLo: 4°C	Hi: 69°FHi: 21°C	Hi: 65°FHi: 18°C Lo: 39°FLo: 4°C	Hi: 65°FHi: 18°C Lo: 39°FLo: 4°C	Hi: 69°FHi: 21°C Lo: 41°FLo: 5°C	Hi: 69°FHi: 21°C Lo: 41°FLo: 5°C	Hi: 69°FHi: 21°C Lo: 41°FLo: 5°C	Hi: 69°FHi: 21°C Lo: 40°FLo: 4°C

POP = Probability of Precipitation.

Weather Outlook Updated: 133 AM EDT Mon Oct 19 2026 Star School, KY Weather - WeatherWorld.com

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Issued: 145 AM EDT Mon Oct 19 2026

Key Messages

1) Strong radiational cooling will yield more chances for frost and freeze conditions tonight and once again Monday night. A Frost Advisory is in place for locations remaining in the active growing season late tonight into Monday morning. Temperatures are anticipated to slowly moderate through the course of the week.

2) A stretch of dry weather, courtesy of high pressure, will triumph through the work week into next weekend.

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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.