Home / Emerald Mountain / 13 October 2016

Emerald Mountain

United States · 13 October 2016

Emerald MountainUnited States11:21 AM localChange location

← 12 October 201614 October 2016 →

Average

20.7°C

low 12.3° · high 30.2°

Rainfall

0mm

dry day

Wind

1.5m/s

daily average

Humidity

52.7%

daily average

Cloud

26%

cover

Pressure

1021hPa

daily average

The temperature ranged from 12.3°C around 07:00 to 30.2°C around 16:00. No measurable rain was recorded during the day.

How unusual was this day?

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

High temperature

84th percentile

Low temperature

33th percentile

Rainfall

59th percentile

Wind

4th 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 20.5°C, versus 20.7°C on this specific day.

Sun & daylight

Sunrise

06:46

Sunset

18:12

Day length

11h 26m

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 timeUTCTemp °CFeels °CRain mmWind m/sDirHumidity %Pressure hPa
00:0005:0014.112.202.1E681021
01:0006:0013.911.702.2ENE651021
02:0007:0013.611.402.1ENE651020
03:0008:0013.411.302.1ENE671020
04:0009:0012.910.802.1ENE681020
05:0010:0012.410.601.9ENE741021
06:0011:0012.410.901.5ENE761022
07:0012:0012.310.901.4ENE771022
08:0013:0014.813.701.4E701022
09:0014:0019.919.800.9E591022
10:0015:0024.323.500.6S371022
11:0016:002625.401.3W381022
12:0017:0027.82701.4WNW341021
13:0018:0028.828.101.4NW331021
14:0019:0029.428.601.4NW311020
15:0020:0029.92901.3NNW291019
16:0021:0030.229.101.5NNW281019
17:0022:0027.828.301NW421019
18:0023:0028.228.200.9NNW361019
19:0000:002625.501NW381019
20:0001:0024.723.901.1NNW381020
21:0002:0022.221.501.1NNE461020
22:0003:001716.501.5NNE711021
23:0004:0015.714.801.7NE741020

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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
Emerald Mountain — 32.500°, -86.000°, ERA5 grid cell center, 10.6 km from requested point
Time zone
America/Chicago
What's shown here
The hourly and daily record for 13 October 2016 specifically — not a monthly average. See the Emerald Mountain 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 (2026-07-17). Historical climate data for Emerald Mountain, United States (32.50°N, 86.00°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 Emerald Mountain, United States [Data set]. Derived from ERA5 (Copernicus Climate Change Service). Retrieved July 17, 2026, from https://www.pastclimate.com/
MLA
"Historical Climate Data for Emerald Mountain, United States." PastClimate, derived from ERA5 (Copernicus Climate Change Service), July 17, 2026, www.pastclimate.com.
BibTeX
@misc{pastclimate,
  author = {PastClimate},
  title = {Historical climate data for Emerald Mountain, United States},
  year = {2026},
  note = {Derived from ERA5 (Hersbach et al., 2023), Copernicus Climate Change Service. Accessed 2026-07-17},
  url = {https://www.pastclimate.com/}
}

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