The museum marks this watercolor in copyright. An open reproduction licence has not been established.
A study against the weather record
Joseph Fiore
Black Mountain Lake Eden
A summer storm above Lake Eden? Nephos’s reading meets a dry season with repeated thunder.
Storm reading plausiblePainted day unknown
The Nephos method
How this study was read
The method in fullWhat is written
Nephos reads the green foliage, foreground lake and dark cloud masses as a summer storm building or passing. This is Nephos’s visual interpretation, not a museum statement or an execution date. The college poster supplies a separate test window: 21 June–4 September 1954.
JUNE 21 TO SEPTEMBER 4
Black Mountain College summer 1954 poster, 2017.40.324; holder’s transcriptionPAINTING Joseph Fiore
Black Mountain College summer 1954 poster, 2017.40.324; holder’s transcription
Records of those days
- Black Mountain daily rain, NOAA USC0031084376/76 daily amounts accepted in the session window; 34 complete matching windows in the long record.
- Asheville airport rain and reported thunder, WBAN 03812GHCN-Daily rain and GSOD thunder are kept separate. The 1954 airport was about 24 km from Lake Eden; its later site and observing equipment changed.
Not found or not yet searched
- The depicted storm is a visual reading. No dated source identifies this watercolor’s day, month or execution session.
- Black Mountain has no thunder entries for this 1954 window. Airport thunder is regional evidence; unreported thunder is not a confirmed absence.
- No securely object-linked letter, preparatory view or lake-level record establishes what weather Fiore altered.
Each claim tested
- Could summer storms occur during a dry teaching season? Yes. Black Mountain recorded 120.8 mm, the driest of 34 complete matching windows, while the airport reported thunder on 23 days. A local newspaper also reports a lightning strike west of town.
- How many substantial rain days occurred nearby? Black Mountain had 16 days with at least 1 mm, 3 with at least 10 mm and 1 with at least 25 mm. These are daily amounts, not storm intensity.
- How does the same season compare with 1991–2020? Airport rain days: 16 in 1954 versus a 25.6-day reference mean. Reported thunder days: 23 versus 17.0. This is an archive comparison across station and reporting changes, not a climate trend.
Verdict
A storm sky within a dry summer: 120.8 mm at Black Mountain, the lowest of 34 complete session windows, and 23 reported thunder days at the airport. The records support the plausibility of the reading, without selecting a painted day.
- Partially agreesSummer-storm reading Nephos’s visual reading is consistent with independent seasonal storm evidence.
- ContradictsAn unusually wet season The local rain total is the lowest of 34 complete comparable windows.
- UnknownA dated painted storm No source connects this watercolor to a particular event.
What this cannot tell you. The summer quarter is a hypothesis-testing window, not a date assigned to the picture. Foliage does not rule out late spring or early autumn. Ranks exclude every incomplete window and are not homogenized for gauge changes. Nearby gauges are never pooled. Rain days use station observation dates; GSOD thunder uses UTC dates. Aligned chart dates do not establish the same storm. GSOD zero means no or not reported. Modern thunder counts are reported occurrences, not a homogeneous thunderstorm climatology. The airport comparison uses all 30 matching windows in 1991–2020, calculated from daily data; it is not an official NOAA normal or a Lake Eden anomaly.
Step 1 · Read the painting
A storm sky above a green landscape
Nephos’s reading of the picture, not a museum statement: Green, fully leafed hills and trees, a lake in the foreground, and heavy dark rain clouds massed over the mountains: a summer storm building or passing over Lake Eden.
In the museum’s small color preview, leafy trees and green slopes carry the eye toward the ridge. Dark grey cloud masses fill much of the sky, broken by pale openings; the lake occupies the lower right. That combination makes a passing or gathering summer storm a useful reading to test. The pale gaps leave its direction unresolved. No lightning bolt or measurable rain shaft is visible, and foliage alone does not exclude late spring or early autumn.
The museum identifies the subject as the Lake Eden campus and dates the watercolor to 1954. The Black Mountain College Museum + Arts Center biography places Fiore’s teaching of painting and drawing between 1949 and 1956. He knew this landscape; the painting is evidence of how he represented it, even though no document identifies its day.
The test: did the summer teaching season contain storms, and was it especially wet? Those are different questions. A dark painted sky need not describe the prevailing weather of an entire summer.
Step 2 · Establish a window
The summer quarter: 21 June–4 September 1954
A surviving college poster, held by Asheville Art Museum as accession 2017.40.324, advertises the regular summer quarter and lists Fiore under painting. Its dates define a 76-day inclusive comparison. They are not a newly assigned date for this watercolor.
“JUNE 21 TO SEPTEMBER 4”
Black Mountain College summer 1954 poster, 2017.40.324; holder’s transcription
“PAINTING Joseph Fiore”
Black Mountain College summer 1954 poster, 2017.40.324; holder’s transcription
The dates are taken from the museum’s transcription of the contemporary announcement. The Western Regional Archives finding aid also lists the 1953–54 bulletin and 1951–54 publicity material; that catalogue establishes surviving records, not a second independently read timetable. A poster documents advertised teaching, not daily attendance or the making of this sheet.
The same 21 June–4 September dates are used in every comparison year. A separate June–August calculation checks whether the result depends on the college’s endpoints. No storm date is selected because it looks like the painting.
Step 3 · Test the storm reading
Storms in the driest comparable summer window
Black Mountain’s gauge recorded 120.8 mm: the lowest of 34 complete matching windows in its 1949–2010 archive. Yet the airport’s hourly-derived daily summaries report thunder on 23 days. The two records describe different aspects of the season: little accumulated rain locally, with repeated evidence of storms in the region.
| Station | Accepted days | Rain, mm | Days ≥ 1 mm | Days ≥ 10 mm | Days ≥ 25 mm |
|---|---|---|---|---|---|
| Black Mountain | 76/76 | 120.8 | 16 | 3 | 1 |
| North Fork | 76/76 | 130.8 | 20 | 4 | 1 |
| Beetree Dam | 76/76 | 121.3 | 17 | 4 | 0 |
| Asheville–Hendersonville Airport | 76/76 | 141.8 | 16 | 4 | 1 |
Here a rain day means at least 1 mm; 10 mm marks a substantial daily amount and 25 mm is this study’s heavy-rain threshold. These thresholds measure daily accumulation, not the intensity or number of storms. Black Mountain’s one day over 25 mm recorded 25.1 mm; at a stricter one-inch threshold (25.4 mm), its count becomes 0. A nearby thunderstorm can be heard or seen without delivering much rain to a particular gauge.
The catalogue gauge positions lie 2.6 km (Black Mountain), 3.9 km (North Fork) and 3.4 km (Beetree) from the mapped lake point. The 1954 airport site was about 24 km away. None is the scene or an easel location. The gauges are not averaged, and their differing daily totals matter.
Black Mountain has no thunder entries for this window in the inspected GHCN archive. That is unknown, not zero. The airport supplies positive thunder reports on 23 days, with daily summaries present for the whole window. NOAA defines a zero thunder flag as no or not reported, so 23 is a count of recorded occurrences, not proof that every other day was storm-free.
Check every day and the complete-window ranking
Every admitted window has 76 accepted daily precipitation amounts. Missing values, nonblank quality flags and missing-presumed-zero flags are rejected; incomplete present-weather-derived precipitation is also rejected. Traces retain their flag and the archived zero. 28 windows are excluded. This is an archive rank, not a homogenized estimate of climatic rarity.
The June–August sensitivity check gives 168.3 mm in 1954, also rank 1 from driest among 34 complete summers. The dry result therefore survives the alternative seasonal boundary.
| Date label | Rain, mm | Trace flag | Airport thunder, UTC day |
|---|---|---|---|
| 21 June | 0.0 | — | No / not reported |
| 22 June | 0.0 | — | No / not reported |
| 23 June | 0.0 | — | No / not reported |
| 24 June | 0.0 | — | No / not reported |
| 25 June | 0.0 | — | No / not reported |
| 26 June | 0.0 | — | No / not reported |
| 27 June | 0.0 | — | No / not reported |
| 28 June | 0.5 | — | No / not reported |
| 29 June | 0.0 | — | No / not reported |
| 30 June | 0.0 | — | No / not reported |
| 1 July | 0.0 | — | No / not reported |
| 2 July | 0.0 | — | Reported |
| 3 July | 3.6 | — | Reported |
| 4 July | 16.8 | — | Reported |
| 5 July | 0.0 | — | Reported |
| 6 July | 0.0 | — | No / not reported |
| 7 July | 0.0 | — | No / not reported |
| 8 July | 5.6 | — | Reported |
| 9 July | 0.0 | Trace | Reported |
| 10 July | 0.0 | — | No / not reported |
| 11 July | 0.0 | — | No / not reported |
| 12 July | 0.0 | — | No / not reported |
| 13 July | 0.0 | — | No / not reported |
| 14 July | 0.0 | — | No / not reported |
| 15 July | 0.0 | — | Reported |
| 16 July | 2.5 | — | Reported |
| 17 July | 0.0 | Trace | No / not reported |
| 18 July | 0.0 | Trace | Reported |
| 19 July | 0.0 | — | No / not reported |
| 20 July | 0.0 | — | Reported |
| 21 July | 8.4 | — | No / not reported |
| 22 July | 1.8 | — | Reported |
| 23 July | 0.0 | Trace | No / not reported |
| 24 July | 0.0 | — | No / not reported |
| 25 July | 0.0 | — | No / not reported |
| 26 July | 0.0 | — | No / not reported |
| 27 July | 0.0 | — | No / not reported |
| 28 July | 0.0 | — | No / not reported |
| 29 July | 0.0 | — | No / not reported |
| 30 July | 0.0 | — | Reported |
| 31 July | 0.0 | — | Reported |
| 1 August | 0.0 | — | Reported |
| 2 August | 8.1 | — | No / not reported |
| 3 August | 0.0 | Trace | No / not reported |
| 4 August | 0.0 | — | No / not reported |
| 5 August | 0.0 | — | No / not reported |
| 6 August | 6.1 | — | Reported |
| 7 August | 0.0 | — | No / not reported |
| 8 August | 5.1 | — | No / not reported |
| 9 August | 0.0 | — | Reported |
| 10 August | 11.7 | — | No / not reported |
| 11 August | 0.0 | — | No / not reported |
| 12 August | 0.0 | — | No / not reported |
| 13 August | 0.0 | — | No / not reported |
| 14 August | 0.0 | — | No / not reported |
| 15 August | 0.0 | — | Reported |
| 16 August | 0.0 | — | No / not reported |
| 17 August | 0.0 | — | No / not reported |
| 18 August | 0.0 | — | Reported |
| 19 August | 0.0 | — | No / not reported |
| 20 August | 0.0 | — | Reported |
| 21 August | 6.4 | — | Reported |
| 22 August | 0.0 | — | No / not reported |
| 23 August | 0.0 | — | No / not reported |
| 24 August | 0.0 | — | Reported |
| 25 August | 25.1 | — | No / not reported |
| 26 August | 0.0 | Trace | Reported |
| 27 August | 6.9 | — | No / not reported |
| 28 August | 1.3 | — | Reported |
| 29 August | 9.4 | — | No / not reported |
| 30 August | 1.5 | — | No / not reported |
| 31 August | 0.0 | — | No / not reported |
| 1 September | 0.0 | — | No / not reported |
| 2 September | 0.0 | — | No / not reported |
| 3 September | 0.0 | — | No / not reported |
| 4 September | 0.0 | — | No / not reported |
| Year | Rain, mm | Days ≥ 1 mm | Days ≥ 25 mm |
|---|---|---|---|
| 1950 | 270.9 | 29 | 2 |
| 1951 | 212.3 | 22 | 1 |
| 1952 | 246.9 | 28 | 1 |
| 1954 | 120.8 | 16 | 1 |
| 1955 | 369.6 | 28 | 4 |
| 1956 | 229.1 | 22 | 2 |
| 1957 | 187.4 | 17 | 1 |
| 1958 | 188.6 | 27 | 2 |
| 1959 | 278.2 | 31 | 3 |
| 1960 | 412.0 | 34 | 5 |
| 1961 | 346.2 | 35 | 3 |
| 1962 | 358.0 | 22 | 5 |
| 1963 | 198.4 | 21 | 1 |
| 1964 | 435.1 | 31 | 6 |
| 1965 | 333.3 | 23 | 3 |
| 1966 | 283.6 | 27 | 2 |
| 1967 | 490.7 | 32 | 6 |
| 1968 | 211.8 | 24 | 1 |
| 1969 | 312.6 | 26 | 6 |
| 1970 | 297.6 | 29 | 3 |
| 1971 | 291.1 | 28 | 2 |
| 1972 | 371.8 | 21 | 6 |
| 1973 | 151.6 | 21 | 1 |
| 1975 | 252.9 | 23 | 3 |
| 1976 | 145.5 | 22 | 0 |
| 1980 | 220.2 | 19 | 2 |
| 1989 | 285.1 | 29 | 4 |
| 1991 | 326.8 | 27 | 4 |
| 1992 | 282.7 | 27 | 3 |
| 1993 | 156.3 | 21 | 0 |
| 2003 | 309.2 | 24 | 4 |
| 2004 | 366.2 | 24 | 5 |
| 2005 | 483.2 | 30 | 8 |
| 2008 | 246.0 | 12 | 3 |
Excluded years: 1949, 1953, 1974, 1977, 1978, 1979, 1981, 1982, 1983, 1984, 1985, 1986, 1987, 1988, 1990, 1994, 1995, 1996, 1997, 1998, 1999, 2000, 2001, 2002, 2006, 2007, 2009, 2010. The data companion preserves the rejected dates, flags, other gauges and full-year context.
Step 4 · Hear the contemporary witnesses
Dry gardens; a lightning strike west of town
The Black Mountain News supplies two local accounts from within the session. On 22 July, Mrs. C. M. Howie’s Bee Tree column describes hot, dry weather in the Bee Tree and Longs Branch sections, with struggling gardens. On 12 August, the front page reports a lightning strike roughly one mile west of Black Mountain on the preceding Monday afternoon, cutting power for an hour.
“We have had very little rain in the last two weeks.”
Bee Tree News, by Mrs. C. M. Howie, 22 July 1954, p. 2
“This was the first serious damage caused by an electrical storm this summer.”
Lightning Hits Line, Customers Blitz Office, 12 August 1954, p. 1
The lightning report places the event at about 1:40 p.m. The preceding Monday was 9 August. It describes the first serious damage of that summer, not its first thunderstorm. That distinction agrees with the broader finding: a dry season can still contain disruptive storms. Neither witness describes Fiore at work or a storm directly over Lake Eden.
Both short quotations were checked against the newspaper page scans; printed line-break hyphenation has been joined. This is the local weekly, not the Asheville Citizen-Times. The latter’s historical database is listed by UNCW Library, but no season-specific Citizen-Times article was verified here. That remains an access and research limit, not a claim that no witness survives.
Step 5 · Then and now
Less rain in 1954; thunder tells a different story
For the identical 21 June–4 September window, the airport series recorded 16 rain days in 1954, compared with a mean of 25.6 in 1991–2020. Its rain total was 141.8 mm against 306.3 mm. These are airport-to-airport archive comparisons; the modern mean is never substituted for Lake Eden.
| Measure | 1954 | 1991–2020 mean |
|---|---|---|
| Precipitation, mm | 141.8 | 306.3 |
| Days ≥ 1 mm | 16.0 | 25.6 |
| Days ≥ 10 mm | 4.0 | 10.1 |
| Days ≥ 25 mm | 1.0 | 2.9 |
| Days with thunder reported | 23.0 | 17.0 |
The means above are calculated from all 30 complete reference windows, not copied from an official monthly normal. The airport’s modern reported-thunder counts range from 6 to 34 days; 1954’s 23 lies within that range. Storm occurrence and accumulated rain do not rank seasons in the same way. By reported thunder days, 1954 ranks 8 from highest among these 31 windows (1954 plus 1991–2020). That is a rank of surviving reports.
This does not establish a decline in thunderstorms. The station history places the 1954 observations at the former Asheville–Hendersonville Airport, with the later record at Asheville Regional Airport; it also records a 1996 move and automation. Thunder flags depend on reporting practice, and zero conflates no with not reported. Neither the thunder counts nor the rain comparison has been homogenized for those changes.
At Black Mountain itself, only 7 complete session windows survive inside 1991–2020, so no 30-year local mean is presented. Its full surviving record supplies the ranking instead.
Step 6 · Return to the watercolor
The drama belongs to a moment, not a seasonal average
Nephos reads the contrast between bright green land and the dark, broken sky as the picture’s weather drama. The records make that reading historically plausible: summer storms occurred in the region even while local rainfall was unusually low within the surviving comparison. The watercolor need not stand for a rain-soaked summer.
What Fiore chose is visible; what he changed is not established. The loose grey washes of the sky, green slopes and small upright trees organize contrasts of tone and scale. That is Nephos’s account of the composition. The museum’s biography describes his broader combination of nature, abstraction and color experiments, but supplies no evidence that he darkened a particular cloud, invented a storm or altered the lake level in this sheet.
No securely object-linked letter or dated preparatory view inspected here fixes the painting session. The course dates remain a testing convention; 9 August remains a newspaper event, not a proposed painted day. Gauge readings are not lake levels, and airport thunder is not a Lake Eden observation. The warranted result is a supported seasonal possibility, not a reconstruction of the sky at the easel.
Sources
Every source on this page
Each file was downloaded and given a fingerprint (its sha256). The page is rebuilt from these files and will not build if a fingerprint changes, so every number above comes from them rather than being typed in.
- Asheville Art Museum, Black Mountain Lake Eden, 2012.53.01.22
sha256 54a72372c8221834777ad4cbbbc725c938ebfc66cf730d1b59066d45b98df256 - Black Mountain College summer 1954 poster, 2017.40.324; holder’s transcription
sha256 10038ee6af1aa21da4c1f4fdb85335e9f10c0c6445cf8b8699355a0a06e381df - NOAA GHCN-Daily format, units and flags
sha256 0e4e6f0e6947cf1add884c328a01760f31c56ef5fb86b85ed57dd5dc4c4aeaa6 - NOAA GHCN-Daily dataset metadata and citation
sha256 82d2cd09b3dab3d99b9123d56973ae352c76c2cd0b9539da4cea939eeced150a - NOAA GHCN-Daily, BLACK MTN 2 W, USC00310843
sha256 a2a02a9e92a974d4602264b4f76a7f7f0220dcae8dbbbf7c6673ce4d30b54ce4 - NOAA GHCN-Daily, BEETREE DAM, USC00310650
sha256 a974f5b290bf245cf4c776be401fef58fc034dbc08da28452ff232ec1eb3eab9 - NOAA GHCN-Daily, N FK 2, USC00316236
sha256 68081d8c387298be1465e28d67b3f5e1ce62b2f29df4de2819826ec2c2d24879 - NOAA GHCN-Daily station coordinates and names
sha256 14c6467fcce6cce8dc0786eba8bbceed51a2f1c1056b0e221b573157559fc824 - NOAA GHCN-Daily element coverage inventory
sha256 fb8a5b7b5bd25b6828fc822e4a4bc2a036053ac5af30697b4df1386a21cb0e59 - NOAA 1991–2020 monthly normals, Asheville Regional Airport
sha256 7bedd90a47e1ffae327208daa1a970ba97178fdc967d498d0dd29cd8d4c1662e - Asheville Art Museum, Joseph Fiore biography
sha256 247d5e3a0f756fad076d1127eb7b1add98ed874073a195714def436bfc6c973c - OpenStreetMap Lake Eden, relation 309372
sha256 a8fdfb475afc87578fd391b7942d1665976d562bbf5f73b1c3af03bf9e358ea2 - NOAA GHCN-Daily, Asheville airport series USW00003812
sha256 0d7c5549876878ed331de047d7424d71f34a5d7180f1e617f4888a3bc0bc21ac - NOAA Global Summary of the Day: day boundary and FRSHTT definitions
sha256 25a784a4cba0eab5f070137c57c4b4bd113982e054c77812b2d22e96c5818bc1 - NOAA 2023 Asheville Local Climatological Data, station history, p. 8
sha256 65d2d6185f330a8e990add135b47731aa32a3e8525e2b596149d47cff15c0f67 - Text extraction of NOAA Asheville station history, p. 8
sha256 5a0c1894ca5d37bbef855df4f7e6b9062b00595844686877e005f369bcc77e52 - Black Mountain News, 12 August 1954, p. 1, Lightning Hits Line, Customers Blitz Office; ALTO text
sha256 649895801dea339a8afadfbdb0b6e5343d412678b441b46094575d269e9de5b3 - Black Mountain News, 12 August 1954, p. 1; source scan
sha256 6e95b9188726244a0054a08d97b16e41b4481449e9a1c6a7215e7c9e2404d01b - Mrs. C. M. Howie, Bee Tree News, Black Mountain News, 22 July 1954, p. 2; ALTO text
sha256 f55efb915cc77bf9ed56922cd6932cce3c901ab07624d06666ccc888e5325e04 - Black Mountain News, 22 July 1954, p. 2; source scan
sha256 2f7182eb1984c917c7731f7c62e9559802ab29aaf8792ace95b6bf42dc18d04e - Black Mountain College Museum + Arts Center, Joseph Fiore
sha256 13ffbd5c410e8f937797530176c64f8cd8db2885d3fdeeb62007bfb2d70b5890 - Western Regional Archives, Black Mountain College Records, 506
sha256 02e24289d96b61e8430c55c3aceb87e44262b6c2971fdcd2d5f994cca2637872 - UNCW Library, Asheville Citizen-Times historical newspaper database access
sha256 d406314cdc5f3c3db2e35f2d15044e9dec44356e9124300fac57fbb0dde09cf5 - Asheville Art Museum preview, accession 2012.53.01.22; private visual inspection
sha256 67d25b34459f9b199f90aa78efc04d3b2cd512b725ab554311d9266a33f9740b - NOAA GSOD, Asheville airport, 1954; WBAN 03812
sha256 7afde54a4b62042e9a20f6840dfa0f818015bd14256c6814fcfd1355e8b77e69 - NOAA GSOD, Asheville airport, 1991; WBAN 03812
sha256 f27c8eb5b8feaca4fc7993b7c7c18edc65723933f10180c430fa0e3572b20afd - NOAA GSOD, Asheville airport, 1992; WBAN 03812
sha256 1d4cb806af0631ecef004e2f635ebf3220957c9574ed55fe6b7163addc572668 - NOAA GSOD, Asheville airport, 1993; WBAN 03812
sha256 f4ff2b5ce4c3be1f363f57b9339042d80f2071b39366df6ff52ad8c7aafd579b - NOAA GSOD, Asheville airport, 1994; WBAN 03812
sha256 7d473ca6125045f86644cf3cd630b3a8079fa599cd090db8eb633ec921369fc1 - NOAA GSOD, Asheville airport, 1995; WBAN 03812
sha256 8df085838aec1def94c275922336c4dcbd5b9b80a2744946dffc3d34023d802e - NOAA GSOD, Asheville airport, 1996; WBAN 03812
sha256 86b985c1e9dc5a0d1bd20f97bbd57b9cb055f77b2750dd87368b43052a9e32f4 - NOAA GSOD, Asheville airport, 1997; WBAN 03812
sha256 c21034dc88e5ceeb2069d52941553f6a21cd567bc070b4fc391f864c14f44af1 - NOAA GSOD, Asheville airport, 1998; WBAN 03812
sha256 74e63430d4b346c325488a8562d464805e7b6b367839dddb518975e19d0e6968 - NOAA GSOD, Asheville airport, 1999; WBAN 03812
sha256 5003d0635152eb639b51177c6dc6f9ce104de14d195e358693b9e583cebc387f - NOAA GSOD, Asheville airport, 2000; WBAN 03812
sha256 55107ff95284494cbdb40b331d659057cbead9fdcb920be4982ea84a5f817588 - NOAA GSOD, Asheville airport, 2001; WBAN 03812
sha256 7163851a27172b4ba12a54f59f33e9ae322097be946e32083c23de129fa34cc3 - NOAA GSOD, Asheville airport, 2002; WBAN 03812
sha256 8077ee957a6d8fdbace6b1cf8d6e61c70715eaaa66a246416b4bf0d0097b276f - NOAA GSOD, Asheville airport, 2003; WBAN 03812
sha256 f67517bd10c08cf5573a639ea322741e4ea4dded2868f5b5f9520d9a756ea6a7 - NOAA GSOD, Asheville airport, 2004; WBAN 03812
sha256 b98f3e119dd1b8c8f2190c73967a21a4737591ecc604bd02181e06f4a63d221e - NOAA GSOD, Asheville airport, 2005; WBAN 03812
sha256 09fbe8d68e22b45643e98d67f66c104b7940c23bc2cc700d647e59bac3b4f836 - NOAA GSOD, Asheville airport, 2006; WBAN 03812
sha256 83fa6055d6d086350d1a03cfa706a67bbb381692e766ffe0c1e7835248b0a3a9 - NOAA GSOD, Asheville airport, 2007; WBAN 03812
sha256 c7174a2b6cea7db80cc7b28a3a317efab697a87e0d32f418cbc864b1bfb7a8a7 - NOAA GSOD, Asheville airport, 2008; WBAN 03812
sha256 27089ffc3d4d5c9550c8996e3d2a68d145e14b1bd08d0d5ea24ca3713934f7e1 - NOAA GSOD, Asheville airport, 2009; WBAN 03812
sha256 c4e8d2b74f1c9f56ffb9f87eb1b95c82a89a9a215e64b86698c6f870e627a857 - NOAA GSOD, Asheville airport, 2010; WBAN 03812
sha256 3e0de8a9e02437ba4420306f912716acf03b912ccad8aac259571533f9e7a561 - NOAA GSOD, Asheville airport, 2011; WBAN 03812
sha256 042bb7e22817aa591fece513809163dd386c859adada2bf7942a521aeff537da - NOAA GSOD, Asheville airport, 2012; WBAN 03812
sha256 f84282110ab87cb46b6937c013767490a931f72c98401d2c3aa19480ba35cea5 - NOAA GSOD, Asheville airport, 2013; WBAN 03812
sha256 0cd29023ee4241f183147f2a28426cce40ba1ab1cf9b7d524821785a8e7aecd8 - NOAA GSOD, Asheville airport, 2014; WBAN 03812
sha256 3bc2a074925a9d00541cb97b307e397bc4cd71bd2a2f8aacd837476755f7d4c5 - NOAA GSOD, Asheville airport, 2015; WBAN 03812
sha256 cba5220af33c69c1a4b98aaec6806dd673ab350586d44d1c44e7858cec6801a9 - NOAA GSOD, Asheville airport, 2016; WBAN 03812
sha256 34655daae6eb579f29f1261c9d46218627d544928a9713b820b623e1d6d46ac9 - NOAA GSOD, Asheville airport, 2017; WBAN 03812
sha256 98811bc21e8d3ea43d2f1f93d94778e728365e3b03faf309fc4628a6b8d52528 - NOAA GSOD, Asheville airport, 2018; WBAN 03812
sha256 8499f0662df1938a6d6b748c8328adabe65d4baa277cf0ad20f4d8d47a3cc9b5 - NOAA GSOD, Asheville airport, 2019; WBAN 03812
sha256 cf6b6ecb89e95a72a0f040cbe009fda60ad29f811bc65a29aaf8822b0adc1400 - NOAA GSOD, Asheville airport, 2020; WBAN 03812
sha256 13705c9fb1f769a0ec5bdf2801bb54ba65de78c93f995105a2514f4550f95410