
Oregon Climate Service, October 2005
Overview
The 2006 Water Year began with generally mild temperatures (most stations reported above-normal values) and wet conditions (mostly above-normal precipitation). All in all, October was a very pleasant autumn month, but watch out – here comes winter!
Table 1 is a summary of monthly
averages and totals at selected stations throughout the state. Table 2 lists
daily temperatures and precipitation for most of the locations listed
in Table
1. In Table 3, monthly and
seasonal precipitation totals throughout the state are listed.
Basin Summary
Here is a summary of water indicators at the end of the month, by river basin:
|
|
|
|
||
| BASIN |
|
|
|
|
| OWYHEE | 243 | 67 | 83 | 0.2 |
| MALHEUR | 168 | 96 | 128 | -0.7 |
| GRAND RONDE, POWDER, BURNT | 150 | 103 | 82 | -2.4 |
| UMATILLA, WALLA WALLA, WILLOW | 137 | 113 | 80 | -2.5 |
| UPPER JOHN DAY | 202 | 136 | 76 | -1.7 |
| UPPER DESCHUTES, CROOKED | 132 | 87 | 41 | -1.1 |
| LOWER DESCHUTES, HOOD RIVER | 139 | 116 | 85 | -2.1 |
| WILLAMETTE | 122 | 86 | 72 | -0.9 |
| ROGUE, UMPQUA | 74 | 64 | 77 | -0.6 |
| KLAMATH | 48 | 60 | 83 | -2.3 |
| LAKE COUNTY, GOOSE LAKE | 207 | 80 | 78 | -0.2 |
| HARNEY | 104 | 134 | 85 | -0.4 |
| NORTH COAST | 141 | 132 | 71 | 0.0 |
| SOUTH COAST | 110 | n.a. | 46 | -0.7 |
n.a. Not available
(1) Percent of normal October precipitation, from NOAA Cooperative
sites
(2) Percent of normal October precipitation, from Natural Resources
Conservation Service (NRCS) SNOTEL sites
(3) Percent of normal October stream flow, from U.S. Geological
Survey (USGS)
(4) Surface Water Supply Index, from NRCS (-4 = very dry, 0 =
normal, +4 = very wet)
Forecasts
The Climate Prediction Center’s (CPC) forecasts for November-January
appear below. Temperatures for all of Oregon are likely to be above normal.
Precipitation probabilities suggest an equal probability of below-, near-,
or above-normal precipitation. CPC also says:
Tropical influences – including ENSO and tropical 30-60-day oscillations
are currently neutral or weak and are expected to have little or no impact
on the climate in the near-term. Trends are used in this forecast. Their impacts
are especially large in forecast leads beyond 0.5 months. The impact of the
NAO [North Atlantic Oscillation] this winter is uncertain for at least two
reasons. First- the NAO is currently near its neutral phase. Also – we
are currently able to predict only a small fraction of the climate variability
associated with the NAO. Research is being conducted with the aim of improving
the use for prediction of all of these factors.

Oregon Climate Service predicts above-normal precipitation and normal temperatures.
For the three-month period ending in January, we predict above-normal precipitation
and slightly above-normal temperatures.
43 Years ago this month: the Columbus Day Storm
October 12 passed without fanfare this year. It wasn’t even “Columbus
Day” – that honor went to October 10 because it was a Monday. But
Northwest weather nuts remember that date every year, and locals who lived
here in 1962 will never forget the “Columbus Day Storm.”
My synopsis of the storm:
When it comes to wind storms in Oregon, the Columbus Day storm stands alone. Nothing before nor since has matched the intensity and damage of that storm, although a few have come close. The "storm" was actually three storms in quick succession. The first formed as a trough off the coast of Oregon on the 11th; it moved northward, and then northwestward, and began to taper off on the 12th. The second (and most destructive) storm formed from the remnants of Typhoon Freda, which moved northeastward from the Philippines, nearing the west coast early on the 12th.
As it neared California, the storm nearly stopped moving, intensified, and began to slowly move northward just off the coast. As it moved, it wreaked havoc from northern California to British Columbia.
The storm reached the Oregon coast on the afternoon of the 12th. The central pressure of the storm dropped lower and lower, finally reaching 28.42 inches. Winds were strong along the coast, but even stronger inland. At Mt. Hebo in the Coast Range west of Salem, measured wind speeds reached 131 mph before the anemometer was destroyed by the winds. On the Morrison Street bridge in Portland, winds gusted to 116 mph (in Naselle, Washington they reached 160 mph). Trees, houses, and power lines were destroyed throughout the state; in some cases residents were without power for 2 to 3 weeks. Giant towers holding the main power lines into Portland (over 500 feet high) were knocked down. The Red Cross estimated that 84 homes were completely destroyed, 5000 severely damaged, and 50,000 moderately damaged. 23 people died in Oregon alone, and damages were estimated at $170 million.
Locally, something remarkable happened. Corvallis Airport collected hourly observations at that time, via a human observer (weather data are now collected on an automated station). On October 12, the wind speeds got higher and higher, finally peaking at 110 (127 mph) at 4 p.m. Just below that, where the next several observations would go, are several blank lines and the words “Abandoned Station” noted at 4:15. A few lines farther down, just before observations began again, the observer wrote that several readings were “unreported due to power failure and instruments demolished.” That brings to mind several questions:
(1) how much stronger did the winds get after the anemometer
was destroyed?
(2) where did the observers go?
To (1) my guess is that it didn’t get much stronger, since most Valley sites seemed to observe their maximum winds at about that time. Question (2) is a different matter, and I’m clueless. I wonder if there was a cellar to hide in. Surely they wouldn’t go outside and drive away, would they? I may never know. But I do know this: the Columbus Day Storm was by far the biggest and most significant wind storm the Northwest ever had. My friend Wolf Read told it this way: In the Willamette Valley on Columbus Day, the lowest of reported maximum wind gusts was Eugene at 86 mph (Salem was 90, Portland 116 and Troutdale 106). No other storm has had a SINGLE location that reached 86 mph in the Valley.
I have placed a scanned copy of the Corvallis Airport
observation form, along with several pictures of storm damage, on the Oregon
Climate Service Web site
at
http://www.ocs.orst.edu/pub/reports/columbus/
Several pictures appear on the below.

A damaged car on the Oregon State University campus after being hit by a
falling tree.

The Van Buren Street bridge, Corvallis, damaged by a falling tree
Oregon Climate Service
George H. Taylor, Oregon State Climatologist
Wayne P. Gibson, Programmer/GIS mngr.
Eileen Kaspar, Research Assistant/Manager of Data Services
Melanie Mitchell, Undergraduate Assistant
Wolf Read, Undergraduate Assistant
Emily Gibson, Student Assistant
Cadee Hale, Publications Assistant
Sara Joos, Student Assistant
Sean Daly, Student Assistant
Kirk Borgerding, Undergraduate Assistant
Kelsey Kuykendall, Undergraduate Assistant
Oregon Climate Service, Strand 326,Phone: (541) 737-5705 Oregon State University Fax: (541) 737-5710 Corvallis, Oregon 97331 E-mail: oregon@coas.orst.edu Web: http://www.ocs.oregonstate.edu