Many of you have thought about this.
And increasingly I am hearing suggestions that it just might be true.
Does Seattle have a weekend weather curse?
With rain, clouds, and cool temperatures on Saturday and Sunday, followed by increasing warmth and sun when we are stuck inside for work or school?
Let us investigate this terrifying possibility by examining the conditions this spring.
I began by looking at the high temperatures at Seattle-Tacoma Airport for March, April, and the first 15 days of May. The results are found below:
Average Weekday High Temperature: 60.4 F
Average Weekend High Temperature: 57.4 F
MY GOD, it's true. High temperatures have been 3F greater during the week. Highly significant difference.
My calculator shaking, I found the average amount of precipitation per day during the same period:
Average Daily Precipitation During Weekends: .35 inches
Average Daily Precipitation During Weekdays: .16 inches
This is scary. More than twice the amount of rainfall per day during the weekends than during weekdays.
I have heard that some folks blame this anomaly on Global Warming. That greater combustion of fossil fuels during weekdays is warming the air both directly and through excessive greenhouse gases. Or that combustion particles are somehow interfering with natural weather processes. You can expect headlines in local newspapers and web media when they learn of these ideas. Particularly one local newspaper.
But the truth is that the origin of this anomaly is beyond science. Beyond logic. It is the Godzilla of weather.
Perhaps we have been cursed. Perhaps we are being punished for some communal sin.
But in any case, my colleagues and I must look for the meteorological silver bullet to end this blight on our communal happiness.
Saturday Update!!
Turns out that Scott Sistek of KOMO TV took my analysis one step further and confirmed the results today in his own blog (found here). For example, after adding January and February 2014 he found that Saturday was the wettest day of the year. And going back to 1949 he got the same results! Don't ask me whether these results are statistically significant, I don't want to get into that. This is metaphysics not physics.
This blog discusses current weather, weather prediction, climate issues, and current events
May 16, 2014
May 14, 2014
An Oddity of This Winter's Precipitation over the Western U.S.
Take a look at this winter's precipitation along the U.S. West Coast from mid-November through mid-May, particularly how much it deviated from normal (the precipitation departure from average). (image below) The most dramatic departure from normal extended from the southern Oregon coast down to central California, with large precipitation deficits (ranging up to 16-20 inches!) also over the Sierra Nevada. You will notice that the Washington Cascades were the wettest place on the map, reaching 12-16 inches above normal. But interestingly, the Washington coast was quite a bit drier than normal, and eastern Washington was a few inches below normal. The northern Rockies were wet.
We can look at the % of normal precipitation for the same period as an alternative (see below). A somewhat similar story but southern California, Arizona, and New Mexico show up as being much drier than normal in terms of percentages: much of region received less than 50% of normal precipitation.
Very strange. What could explain this pattern? If wet storms were more frequent over the Cascades, why was the coast dry?
I suspect I know the answer to this.
The first part of the winter was quite dry over the the entire region and we did not get many strong storms at all. The precipitation turned on during the second half of the winter, starting in early February. And during that period the precipitation was mainly limited to central Oregon northward. The flow was still anomalous with unusual ridging (high pressure) over California and lower than normal pressure over British Columbia. Such a pattern would tend to produce westerly/northwesterly flow over Washington the lower atmosphere, rather than the more typical southwesterly flow.
That is the key.
That is the key.
Westerly flow tends to drop large amounts of precipitation on the windward slopes and crests of north-south oriented high mountain ranges, like the Cascades. But such flow promotes drying east of the Cascade crest as the air is forced to descend and warm. Southwesterly flow produces heavy precipitation along the coast and Olympics, while northwesterly flow is drier. And westerly/northwesterly flow produces descent (and drying) to the east of the Olympics. It all fits. But can we prove it?
I think I know how. Let's examine the flow at around 5000 ft (850 hPa pressure) for the wet period from mid-February though mid-April. Below is the difference from normal of the flow averaged over that period . We call this the height anomaly. As I suspected, the heights were higher than normal (red/orange colors) over CA and southern Oregon and lower than normal to the north. This produced a large north-south gradient in heights (or pressure), which would produce stronger winds than normal over the Northwest from a westerly or northwesterly direction. The black arrows show you the anomalous winds during that period (they are draw parallel to the colored lines). They are from the west to northwest over Washington.
So this explains what happened....with higher heights than normal to our south we had stronger westerly/northwesterly winds than normal, which produce more upslope than normal on the Cascades and more downslope to their lee. Locations to the lee of the Olympics and coastal mountains were also drier.
I think I know how. Let's examine the flow at around 5000 ft (850 hPa pressure) for the wet period from mid-February though mid-April. Below is the difference from normal of the flow averaged over that period . We call this the height anomaly. As I suspected, the heights were higher than normal (red/orange colors) over CA and southern Oregon and lower than normal to the north. This produced a large north-south gradient in heights (or pressure), which would produce stronger winds than normal over the Northwest from a westerly or northwesterly direction. The black arrows show you the anomalous winds during that period (they are draw parallel to the colored lines). They are from the west to northwest over Washington.
So this explains what happened....with higher heights than normal to our south we had stronger westerly/northwesterly winds than normal, which produce more upslope than normal on the Cascades and more downslope to their lee. Locations to the lee of the Olympics and coastal mountains were also drier.
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