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Willmar

United States · 8 September 2016

WillmarUnited States3:54 AM localChange location
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← 7 September 20169 September 2016 →

Average

19.8°C

low 14°C · high 24.2°C

Rainfall

0.2mm

dry day

Wind

3.1m/s

daily average

Humidity

71%

daily average

Cloud

24%

cover

Pressure

1012hPa

daily average

The temperature ranged from 14°C around 07:00 to 24.2°C around 16:00. Rain was recorded for one hour, around 21:00 (0.2mm total).

How unusual was this day?

Compared against the same 135 calendar days (±7 days) across the other 9 years on file.

High temperature

47th percentile

Low temperature

57th percentile

Rainfall

66th percentile

Wind

30th percentile

A percentile of 100 means this was the hottest/wettest/windiest of the comparable days on file; 50 is right in the middle. This window's average temperature was 18.6°C, versus 19.8°C on this specific day.

Sun & daylight

Sunrise

06:50

Sunset

19:43

Day length

12h 52m

Hour by hour

Temperature (line) and hourly rainfall (bars), local time — America/Chicago.

↓ Download CSV
00:0006:0012:0018:0023:00

Cumulative rainfall through the day.

00:0006:0012:0018:0023:00
Local timeUTCTempFeelsRain mmWind m/sDirHumidity %Pressure hPa
00:0005:0019.7°C19.7°C04.2WSW931010
01:0006:0019.5°C19.2°C04.8W941010
02:0007:0019.1°C18.4°C05WNW931010
03:0008:0018.2°C17.2°C04.9WNW931011
04:0009:0017.3°C15.8°C04.9WNW921011
05:0010:0014.3°C12.5°C03.6WNW891012
06:0011:0014.3°C12.5°C03.6WNW891013
07:0012:0014°C12.6°C03.1WNW901013
08:0013:0014.6°C13.5°C02.8WNW901013
09:0014:0015.9°C15°C02.7WNW831014
10:0015:0020.2°C19.2°C02.4WNW591014
11:0016:0021.4°C20.6°C02.2W571013
12:0017:0022.8°C21.8°C02.3W501013
13:0018:0023.4°C22.5°C02.4W501013
14:0019:0023.5°C22.2°C02.8WSW501013
15:0020:0024.1°C23°C02.6WSW491012
16:0021:0024.2°C23.1°C02.4SW471012
17:0022:0023.5°C22.3°C03.2SW531012
18:0023:0023.3°C22.7°C02.4SSW541012
19:0000:0022.3°C22.7°C0.011.2SSE591011
20:0001:0020.4°C20.3°C0.031.8SE651011
21:0002:0020.8°C20°C0.122.6SE621011
22:0003:0019.2°C18.6°C02.8SE731011
23:0004:0019°C18°C0.023SSE711012

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Data source & coverage — ERA5 reanalysis, 2016–2025 (10 years)details
Source
ERA5 reanalysis, accessed via the Copernicus Climate Change Service (C3S) Climate Data Store
Data type
Reanalysis — a physically consistent reconstruction combining a forecast model with historical observations, not a live station reading or a forecast
Coverage
2016–2025 (10 years) for United States
Location
Willmar — 45.000°, -95.000°, ERA5 grid cell center, 14.0 km from requested point
Time zone
America/Chicago
What's shown here
The hourly and daily record for 8 September 2016 specifically — not a monthly average. See the Willmar climate overview for typical conditions.
Spatial resolution
0.25° (~25 km) distributed grid — ERA5's native model resolution is finer; this is the publicly distributed regridded product
Version / refreshed
Methodology v2026.07 · data last refreshed December 31, 2025
Limitations
A model reconstruction, not a station observation — hyper-local extremes (a single storm cell, an urban heat pocket) can differ from a nearby gauge. See the full methodology.
Attribution
Generated using Copernicus Climate Change Service information

Cite this data

Plain text
PastClimate (2026-07-20). Historical climate data for Willmar, United States (45.00°N, 95.00°W), derived from ERA5 (Hersbach et al., 2023, Copernicus Climate Change Service). Retrieved from https://www.pastclimate.com/
APA
PastClimate. (2026). Historical climate data for Willmar, United States [Data set]. Derived from ERA5 (Copernicus Climate Change Service). Retrieved July 20, 2026, from https://www.pastclimate.com/
MLA
"Historical Climate Data for Willmar, United States." PastClimate, derived from ERA5 (Copernicus Climate Change Service), July 20, 2026, www.pastclimate.com.
BibTeX
@misc{pastclimate,
  author = {PastClimate},
  title = {Historical climate data for Willmar, United States},
  year = {2026},
  note = {Derived from ERA5 (Hersbach et al., 2023), Copernicus Climate Change Service. Accessed 2026-07-20},
  url = {https://www.pastclimate.com/}
}

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