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Other Stations in Asheville
About this Station
The city of Asheville is located on both banks of the French Broad River, near the center of the French Broad Basin. Upstream from Asheville, the valley runs south for 18 miles and then curves toward the south-southwest. Downstream from the city, the valley is oriented toward the north-northwest. Two miles upstream from the principal section of Asheville, the Swannanoa River joins the French Broad from the east. The entire valley is known as the Asheville Plateau, having an average elevation near 2,200 feet above sea level, and is flanked by mountain ridges to the east and west, whose peaks range from 2,000 to 4,400 feet above the valley floor. At the Carolina-Tennessee border, about 25 miles north-northwest of Asheville, a relatively high ridge of mountains blocks the northern end of the valley. Thirty miles south, the Blue Ridge Mountains form an escarpment, having a general elevation of about 2,700 feet above sea level. The tallest peaks near Asheville are Mt. Mitchell, 6,684 feet above sea level, 20 miles northeast of the city, and Big Pisgah Mountain, 5,72l feet above sea level, 16 miles to the southwest.
Asheville has a temperate, but invigorating, climate. Considerable variation in temperature often occurs from day to day in summer, as well as during the other seasons.
While the office was located in the city, the combination of roof exposure conditions and a smoke blanket, caused by inversions in temperature in the valley on quiet nights, resulted in higher early morning temperatures at City Office sites than were experienced nearer ground level in nearby rural areas. The growing season in this area is of sufficient length for commercial crops, the average length of freeze-free period being about 195 days. The average last occurrence in spring of a temperature 32 degrees or lower is mid-April and the average first occurrence in fall of 32 degrees is late October. The orientation of the French Broad Valley appears to have a pronounced influence on the wind direction. Prevailing winds are from the northwest during all months of the year. Also, the shielding effect of the nearby mountain barriers apparently has a direct bearing on the annual amount of precipitation received in this vicinity. In an area northwest of Asheville, the average annual precipitation is the lowest in North Carolina. Precipitation increases sharply in all other directions, especially to the south and southwest.
Destructive events caused directly by meteorological conditions are infrequent. The most frequent, occurring at approximately 12-year intervals, are floods on the French Broad River. These floods are usually associated with heavy rains caused by storms moving out of the Gulf of Mexico. Snowstorms which have seriously disrupted normal life in this community are infrequent. Hailstorms that cause property damage are extremely rare.
Data Inventories
Please note that additional data (digital and non-digital) may be available for this station. Contact NCDC if additional details are needed.
Click on the following where available:
- DAT to obtain digital ascii data (charges may apply),
Please do not order these data if you do not know what a Digital ASCII File is.
- INV to view inventory, or
- DOC to view documentation
Surface
DAT INV DOC 3200 -Cooperative Summary Of The Day
DAT INV DOC 3210 -Summary Of The Day - First Order
DAT INV DOC SOD -Daily Surface Data (TD3200/3210 combined)
DAT INV DOC 3220 -Summary Of The Month (SOM) Cooperative
DAT INV DOC 3240 -Hourly Precipitation Data
DAT INV DOC 3280 -Surface Airways Hourly And Airways Solar Radiation
DAT INV DOC 3290 -Summary Observation
DAT INV DOC 3292 -Weather Duration
DAT INV DOC 9950 -DATSAV 2 Surface (see Global Surface Station Information).
DATA
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Forms, Publications, and Web Pages
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Digital ASCII Files
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Station History
Asheville Rgnl Airport
Additional Station History Data from MMS
| Date Began | Date Ended | Lat/Lon | Elevation meters/feet | COOP ID | WBAN | Call Sign | WMO ID | Type |
| ASHEVILLE RGNL AP |
| 01 Jun 1996 | Present | 35°26'N / 82°32'W | 645.3m / 2117' | 310300 | 03812 | AVL | 72315 | LAND SURFACE COOP B ASOS ASOS-NWS WSO |
| 01 Jan 1995 | 01 Jun 1996 | 35°26'N / 82°33'W | 652.3m / 2140' | 310300 | 03812 | AVL | 72315 | LAND SURFACE COOP B WSO |
| 06 Jan 1990 | 01 Jan 1995 | 35°26'N / 82°33'W | 652.3m / 2140' | 310300 | 03812 | AVL | 72315 | LAND SURFACE COOP B WSO |
| 01 Jul 1980 | 06 Jan 1990 | 35°26'N / 82°33'W | 652.3m / 2140' | 310300 | 03812 | AVL | 72315 | LAND SURFACE COOP WSO |
| ASHEVILLE AP |
| 01 Jan 1976 | 01 Jul 1980 | 35°26'N / 82°33'W | 652.3m / 2140' | 310300 | 03812 | AVL | 72315 | LAND SURFACE COOP WSO |
| 01 Sep 1964 | 01 Jan 1976 | 35°26'N / 82°33'W | 652.3m / 2140' | 310300 | 03812 | . | . | LAND SURFACE COOP WSO |
| 25 Aug 1964 | 01 Sep 1964 | 35°26'N / 82°33'W | 652.3m / 2140' | . | . | . | . | LAND SURFACE FAA |
| 30 Apr 1961 | 25 Aug 1964 | 35°26'N / 82°33'W | 654.1m / 2146' | . | . | . | . | LAND SURFACE FAA |
| 10 Apr 1961 | 30 Apr 1961 | 35°26'N / 82°33'W | 654.1m / 2146' | . | . | . | . | LAND SURFACE LAWRS FAA |
| 05 Apr 1961 | 10 Apr 1961 | 35°26'N / 82°33'W | 654.1m / 2146' | . | . | . | . | LAND SURFACE LAWRS FAA |
| 01 Jan 1961 | 05 Apr 1961 | 35°26'N / 82°33'W | 654.1m / 2146' | . | . | . | . | LAND SURFACE LAWRS |
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