January 29-30, 2004 Minor Windstorm compiled by Wolf Read |
A strong cold front trailing south of a deepening low slammed into the Pacific Northwest around midnight from January 29-30, 2004. For much of Oregon, strong, gusty winds were associated with the frontal boundary, often reading 35 to 45 mph in gusts, sometimes higher. These winds typically did not last long, say 10 to 20 minutes, and were associated with a period of heavy rain. As the low moved inland and deepened to 986 mb over Southern British Columbia, tight gradients were carried over Northwest Oregon and Western Washington behind the front. A second round of wind resulted, generally weaker than the frontal winds in Oregon, but stronger in Washington, with gusts into the 50 mph range in places. Though it didn't affect the Seattle area as strongly, this storm had similar effects to the December 27, 2002 event for much of the Western Pacific Northwest. Here's what I noted about this storm in my journal: |
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January 29-30, 2004: Meteorological Details The surface map for 01:00 HRS PST is shown in Figure 5, below. These are the conditions approximately one hour after my peak gust of 44 mph (23:57). Note the closely-packed isobars along the cold front, especially in Oregon. The isobars are oriented almost west-east over the region, a nearly ideal situation for strong ageostrophic (jumping the gradient) winds in the south-to-north trending valleys, such as the Willamette. |
Figure 6, below, adds further detail on the storm's progress across the Pacific Ocean. Interestingly, the cyclone appears to have continued deepening even as it moved inland, reaching its strongest over Southwest British Columbia. The low center began to fill after 04:00 PST on January 30, 2004. This track does not show the low's double structure from about 16:00 PST on the 29th to 22:00 PST. The circles indicate the position of the trailing low of the pair--it followed right on the heels of the lead low, which depressed barometers early across much of Western Washington. |
General Storm Data Table 1, below, lists the barometric minimums for the January 29-30, 2004 storm at selected sites. Many Pacific Northwest windstorms have produced lower readings. These values are similar to the December 27, 2002 windstorm. The most depressed pressures during this storm were along the tip of the Olympic Peninsula, and included 29.17" at 00:00 on the 30th at Tatoosh Island. Sources: National Weather Service, Eureka, Portland and Seattle offices, METAR reports, and the National Data Buoy Center, realitime meteorological data. |
Table 1 Notes: [1] Last of two occurrences, the other having happened the hour before. [2] Last of three occurrences, the others happening at 22:00 and 23:00 on the 29th. [3] Last of two occurrences, the other having happened the hour before. [4] Last of three occurrences, the others happening at 01:00 and 02:00 on the 30th. |
Table 2, below, lists the maximum gradients for some standard measures during the January 29-30, 2004 cyclone. The readings aren't particularly strong, and are generally similar to the December 27, 2002 windstorm. Sources: National Weather Service, Eureka, Portland and Seattle offices, METAR reports, the National Data Buoy Center, realitime meteorological data, and the National Climatic Data Center, unedited surface observation forms (for historical storm pressure data). |
Table 2 Notes: [1] Last of two hourly occurrences, the other having happened the hour before. |
Another measure for storms that track across the Olympic Peninsula and/or South Vancouver Island is the longer PDX-BLI gradient. Table 3, below, ranks a number of memorable, and not-so-memorable, storms by this measure. The January 29-30, 2004 storm ranks a meager 12th place in this incomplete list of windstorms from 1934 to present. The +22.7 mb gradient (+0.67") for the October 21, 1934 storm was taken from spotty pressure data, and could have been higher--the mark of one of the top most powerful storms of the 20th century. Sources: National Weather Service, Eureka, Portland and Seattle offices, METAR reports, and the National Climatic Data Center, unedited surface observation forms (for historical storm pressure data). |
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Pressure Tendencies The January 29-30, 2004 event, interestingly, favored the Western Oregon interior with the strongest pressure changes. Quite possibly the Coast Range gave the cold front an extra kick of instability that may have contributed to the stronger pressure falls compared to those on the coast. The tendency for the maximum hourly fall to be around 23:00 and 00:00 and maximum hourly rise to be around 01:00 to 02:00 marks the strong, fast-moving, frontal system, which nearly paralleled the coast. Source: National Weather Service, Eureka, Portland and Seattle offices, METAR reports, and the National Climatic Data Center, unedited surface observation forms (for historical storm pressure data). |
Table 4 Notes: [1] The -1.5 mb hourly fall at Arcata is the last of two occurrences, the other having occurred in the hour before. [2] Pressure data missing at Quillayute for about four hours before minimum and during the time of max hourly falls at other coastal stations; the -2.0 maximum hourly fall may be low. |
Table 5, below, lists the peak wind and gust for eleven key stations in the Pacific Northwest, their direction, and their time of occurrence. "Peak Wind" is a 2-minute average, and "Peak Gust" is a 5-second average. By my own personal methodology, a wind event rates the term "windstorm" when the average peak gust of these eleven stations reaches 39.0 mph (gale force) or higher. The January 29-30, 2004 cyclone just made the cut, and is a minor windstorm. Moderate windstorms have an average of 45.0 to 54.9, and major windstorms are those that reach or exceed 55.0. Only a handful of storms have made the majors, including December 12, 1995, November 14, 1981 and October 12, 1962. Note that the newer 5-second gust adopted by the NWS alters the meaning of the kind of storm ranking system I describe here. See "Adjustments to Modern Storms." Sources: National Weather Service, Eureka, Portland and Seattle offices, METAR reports. |
Location | Peak |
Direction |
Obs Time of |
Peak |
Direction |
Obs Time of |
California: | ||||||
Arcata | 26 |
270 |
00:56 HRS, 30th |
36 |
260 |
00:45 HRS, 30th |
Oregon: | ||||||
North Bend | 30 |
260 |
23:15 HRS, 29th |
48 |
260 |
23:15 HRS, 29th |
Astoria | 31 |
190 |
16:55 HRS, 29th |
47 |
180 |
21:44 HRS, 29th |
Medford | 32 |
230 |
00:44 HRS, 30th |
47 |
210 |
00:53 HRS, 30th |
Eugene | 22 |
180 |
22:54 HRS, 29th |
39 |
230 |
00:54 HRS, 30th |
Salem | 24 |
200 |
23:56 HRS, 29th |
44 |
220 |
00:56 HRS, 30th |
Portland | 23 |
260 |
00:35 HRS, 30th |
41 |
260 |
00:35 HRS, 30th |
Washington: | ||||||
Quillayute | 23 |
270 |
04:37 HRS, 30th |
47 |
290 |
05:53 HRS, 30th |
Olympia | 25 |
230 |
00:12 HRS, 30th |
37 |
230 |
00:12 HRS, 30th |
Sea-Tac | 25 |
230 |
09:56 HRS, 30th |
40 |
230 |
05:56 HRS, 30th |
Bellingham | 35 |
180 |
03:53 HRS, 30th |
43 |
180 |
03:53 HRS, 30th |
AVERAGE | 26.9 |
227 |
42.6 |
232 |
Last Modified: March 19, 2004 You can reach Wolf via e-mail by clicking here. | Back | |