Tuesday, April 30, 2013

Never Too Late To Snow

Monday, April 29, 2013
10:52 P.M.


First off, let my apologize for my lack of punctuality when it comes to posting these blogs as of late. I've been very busy recording an album for a funk band I am in, and I have had a string of seizures to boot. Thankfully, the album is almost done, and I'll be going into the Swedish Neuroscience Institute on Thursday to get some brain tests done and see if we can get the seizures under control. If anybody knows how to fix the human body, it's those Swedes. I've also been in the process of writing a more in-depth post about a climate talk I went to, but when the Snoqualmie Pass WSDOT cams took my breath away today, I knew that the Weather Gods were calling upon me to write a quick blog in the immediate future.

In any event, I hadn't been following the weather closely, so I was extremely surprised when I saw a layer of white covering I-90 from Denny Creek to Easton. I've seen Snoqualmie Pass covered in snow in mid-June, so it wasn't the time of year that had me trippin'. What really struck me was that most regions in the sound reached the mid-to-upper 50s today, which meant that for there to be sticking snow at Denny Creek (I think Denny Creek is at approximately 2,000 feet), there must have been an incredibly steep environmental lapse rate (decrease in temperature with height). This would imply that the atmosphere was very unstable, but I don't recall seeing any massive cumulonimbus popping up over the area this afternoon. 

I tried to get the Sand Point profiling data which would give me an estimation of how the temperature varied with height, but I was having problems opening the .gif files from the profiler. Instead, I decided to look at the radiosonde soundings from the 00z Quillayute weather balloon launch. The plot below shows the temperature and winds as a function of increasing elevation (and hence decreasing pressure), and it also gives the statistics for things like CAPE (Convective Available Potential Energy) and other acronyms that are Greek to me.



This plot is called a "Skew-T" plot because the axes for temperature are angled and have a positive slope instead of simply being vertically oriented parallel to the y-axis. At first glance, it would look like the temperature more or less remains the same before increasing in the upper levels up the atmosphere, but once you know that this t-plot is skewed, you know that the temperature decreases until it more-or-less flattens out above 200mb. We are concerned with the air near the surface, and you can see that there is an extremely rapid decline in temperature with height between the 1000-900mb levels.


Here are the current conditions along I-90. Seattle has cooled down to 46 degrees, but it is still snowing well below the pass. This snow will continue throughout the night before dying down tomorrow morning.

The Summit at Snoqualmie is technically still open for the season, and they claim that the last day they will be open is May 5th for Cinco de Mayo. I hope to be up there listening to Jimmy Buffett with the best of 'em, but even if that doesn't end up happening, I would not be surprised in the least if they extended the season for another week. This is what happened during the massive snow year of 2007-2008, and I skied the Alpental Backcountry on Memorial Day of that year, which was officially the last day any part of the Summit was open. Don't count on them keeping it open much longer though... even if there is enough snow, they still gotta find a way to make a profit. And if only season's pass holders are coming up to the slopes, Boyne is losing money.

Thanks for reading! My brain is still a little scrambled for a seizure I had Sunday night, so if you come across any awkward phrasing, cut me a little slack. I'll get my other post-in-progress up soon.

Charlie

Saturday, April 20, 2013

A Taste of Summer

Saturday, April 20, 2013
12:28 A.M.

Long Beach, California - Taken April 3, 2013 using a Nikon D3000. Photo credit: Michael Trofimov.
Hey everybody. Sorry for leaving you guys hanging for a couple days, midterms called. I think I had a false sense of this quarter being easy just because I have relatively more time compared to last quarter. Well, it turns out I still have a lot of work to do, more than I anticipated.

On another note, the above picture was taken by Michael Trofimov, a fellow weather buddy who is four years my junior and therefore still in high school. He's an extremely bright kid and takes some great pictures, and he's given me permission to use them on this blog. His Flickr Photostream is here, and I'll also post his site under the "My Favorite Weather Links" list on the left side of this blog. Thank you Michael!

This last week has been pretty darn wet. So wet, in fact, that it has pushed our April rainfall total to the second-highest total on record at Sea-Tac. The record for April precipitation is 6.53 inches, and this was set way back in 1991. As of 6 PM Friday, we've received 5.49 inches, which is 3.63 inches above our average value to date: 1.69 inches.

January had 4.16 inches of rain, February had a measly 1.58 inches, and March had 2.74 inches. These values were all below average, with those months averaging 5.57, 3.50, and 3.72 (yes, March is rainier on average than February!) inches respectively. Thus, our average value through these three months is 12.79 inches, and we received 8.48 inches, leaving us 4.31 inches below normal. As of 6 PM Friday, we have received 13.97 inches since January 1 (and probably over 14 inches by the time I will be finished writing this blog), which is only 0.68 inches below our average yearly-to-date value of 14.65 inches. Well done, April.

By the way, I got all these climate statistics from "Climate Data" under "Data and Forecasts" from the University of Washington atmospheric sciences department page. Here's the link: http://www.atmos.washington.edu/data/data.php?loc=climatological.

I wish we could use the next eleven days of the month to smash the rainfall record, but that won't happen. We look to be entering an extended period of abnormally warm and dry weather. Here are the predicted 6-10 day temperature and precipitation anomalies over our area from the Climate Prediction Center. Take a look for yourself, we will be warm and dry.



Here's a look at the 500 millibar chart for Monday over the Eastern Pacific. The semi-permanent Eastern Pacific High is creeping northward, a sign that summer isn't too far away.

Valid 08:00 pm PDT Mon, 22 Apr 2013 - 75hr Fcst: UW 00z WRF-GFS: 36km 500mb absolute vorticity, heights
This trend looks to continue for the foreseeable future. Brace yourselves, we are in for a boring ride.

Charlie

Monday, April 15, 2013

How to: Take a Shower

Monday, April 15, 2013
4:34 P.M.


Last night, I had a spiritual revelation of sorts. I had just finished shaving (my face) and was getting ready to hop in the shower. I eagerly turned on the water, but after about five seconds or so, I estimated that the temperature had only risen from ~50 degrees at the start to ~70 degrees, and it plateaued there. I was extremely discouraged that all the work I had put into successfully taking a shower had gone to waste, so I trekked 20 feet back to my dorm room to try and kill time for 20 minutes while waiting for the water to heat up.

Twenty minutes later, I marched straight into the bathroom and authoritatively turned on the showerhead. Much to my dismay, the water temperature was still a bone chilling 70 degrees. This time, though, I wasn't just gonna let this water be the boss of me. I was going to own the shower and nothing was going to stop me from scrub-a-dub-dubbing.

As I attempted to boldly glee as the frigid water trickled down my back, I came to an amazing realization. I realized that if I wanted to keep warm, I should use the absolute least amount of water possible. So, after dousing myself for a good 60 seconds, I turned the shower completely off and proceeded to wash my head, shoulders, knees and toes. I was able to get them pretty clean... I feel like the increased friction due to the relative lack of water made for a more effective cleansing method, as I had the ability to apply more force towards unearthing the unwanted grime that covered my body due to the higher friction coefficient k of slightly moist skin as opposed to wet skin.


After I was done evacuating the unwanted contaminants nested upon my epidermis, I proceeded to turn the water back on and wash everything off. The whole washing off process probably took around 90 seconds, as I needed to get the shampoo off my hair and get the soap off everywhere else. The soap was deeply nested in my skin and didn't just slide off by itself... further evidence that when it comes to scrubbing, a little lubrication goes a long way.

Soon, I was fresher than Bel-Air, and I only had the water on for around 2-3 minutes.

People always say that the trick to reducing water usage is to take short showers with low-flow showerheads. While there is definitely truth to this statement, the shower is more than just a cleaning cubicle. Some of life's greatest awakenings occur in this sacred place. With my newly embraced shower-taking method, I can use minimal water in a slippery, soapy silence, and shine brighter than the sun with the knowledge that somewhere, some salmon is smiling.

Charlie

Saturday, April 13, 2013

Die Another Day

Saturday, April 13, 2013
5:04 P.M.

From Wednesday, April 10, 2013:

"We'll have some rain coming in Friday afternoon, but I'll bet my life on having a strong convergence zone somewhere in the area Saturday afternoon due to a cool, moist, onshore flow splitting around the Olympics and converging somewhere along Puget Sound. If I'm still alive on Sunday, you'll know I was right."

Well, it looks like I will be alive on Sunday, and more alive than I've ever been.

Alright, well know that ya'll know I'm like... the best forecaster ever... let's actually talk about what is happening outside right now.

Camano Island Radar: 04:58 pm PDT Sat 13 Apr 2013
This is the radar picture taken from the Camano Island radar at 4:58 pm today, and you can see that there are a lot of showers around Puget Sound. Interestingly enough, there actually look to be two convergence zones, one over the San Juans and another, stronger one directly over the Seattle area. Because there are so many other showers in the area, it is a little tough to make out zone over Seattle, but as evidenced by the band of precipitation and the extremely heavy showers embedded within this band, it is there.

The scale on the right uses different colors to denote different rainfall rates. More specifically, it measures dBZ (decibels relative to Z), and is the meteorological measure of Z (reflectivity) of a radar signal reflected off an object. This is a logarithmic scale, so small increases in the scale represent much larger increases in reflectivity (and therefore precipitation in most cases). Whenever you see reds on this radar, you can be assured that there is heavy rain or hail in the area, and if you look closely at this picture, you can see that the reds are centered right over Seattle.

UW Campus looking out over Red Square: ~ 5 pm
I've counted about 4-5 lightning strikes at the UW in the last 15-20 minutes or so, which is quite a few for a springtime northwest thunderstorm. There was some hail mixed in with the rain at one point, which indicates strong updrafts and instability within the shower, as hailstones cannot form without updrafts suspending them to a point where they can accumulate ice before they finally become too heavy and fall to the ground. Right now (5:23), the rain has almost completely stopped, so let's take another look at the radar.

Camano Island Radar: 05:18 pm PDT Sat 13 Apr 2013
As you can see, the rain has moved south of the UW area and is now directly over downtown Seattle. The actual shape of the convergence zone is better defined in this picture.

1km resolution GOES-West: Pacific Northwest Visible Satellite 05:00 pm PDT Sat 13 Apr 2013
You can even see the convergence zone over Seattle on the satellite. See that little finger extending westward from the Central Cascades over to Hood Canal? That's the convergence zone. Another thing to note is the incredible rain shadow over Eastern Washington. Look at how the clouds just completely die out once you move to the east of the Cascade crest and there is downslope flow. Simply beautiful stuff.
With the cold air aloft, there are very low snow levels. The passes are getting hammered, and I even heard of a few snowflakes flying by Western Washington University this morning.

The convergence zone should gradually dampen as we head towards midnight, but I'd still be on the lookout for a couple more strikes here and there. Springtime Pacific Northwest weather... it can be exciting!

Stay safe.
Charlie

Friday, April 12, 2013

Working Together to Forecast Weather Better

Friday, April 12, 2013
2:57 PM

If any of you ever watched a certain t.v. show that's about more than just card games, you are familiar with the picture above.
We need to work together more as a society in general. I mean, look at Congress. The rifts between the Democratic and Republican Parties are huge, and progress is being stifled by people who are unwilling to make compromises. I disagree strongly with a lot of the actions that are being perpetrated both domestically and abroad by our government, and I know that a lot of my priorities don't match up with those being debated in our nation's capital. However, even if I disagree, it is still better to try and work out a solution that works for the majority of people rather than just debate, pass, filibuster, veto, etc. One of the sectors that is in the most dire need of cooperation, though, is the meteorological sector.

There is plenty of international cooperation when it comes to climate change. There is a conference called the IPCC (International Panel on Climate Change) that has produced four major scientific reports drawing upon scientists all over the world with the first one occurring in 1990 and the last one occurring in 2007, with the next one expected to be completed in 2014. The Kyoto Protocol (1997) to the United Nations Framework Convention on Climate Change (UNFCCC) is an international treaty that restricts the amount of greenhouse gases that an industrialized country can release. Greenpeace, a non-governmental environmental organization that has offices in over 40 countries, focuses on essentially everything necessary to keeping our earth green and peaceful, and climate change is one of their chief priorities. There are countless other organizations that work together to research paleoclimate, assess our current climate and GHG emissions, and predict future scenarios based on the magnitude of GHGs emitted into the atmosphere, with particular emphasis on predicting both the direct warming from the greenhouse effect due to these gasses and the additional warming that will be experienced due to positive feedbacks, as there are far more positive feedbacks than negative feedbacks at this time. One of the strongest positive feedbacks right now is the relationship between declining sea ice in the arctic and an increased absorption of solar insolation due to the much lower albedo of water. Just to clarify, albedo represents the amount of solar radiation radiated back into space. Snow has a high albedo, so it reflects a bunch of solar radiation to space. Water has a low albedo and absorbs most of this radiation, thus warming the planet at a higher rate.

Unfortunately, the meteorological sector of atmospheric sciences is dominated the competition and not cooperation. While some competition is good (basketball games would be really boring if the teams both tried to help each other win), competition results in inconsistencies in data collection and forecasting. This was brought into the forefront of American media when Superstorm Sandy hit the United States, as the European model consistently forecast a U.S. landfall while the American model took the storm harmlessly out to sea. Around a month ago, the two main American models, the NAM and the GFS, predicted a monster snowstorm to hit D.C.. The storm never came. To be fair, this was an extremely difficult forecast and made forecasting Sandy look like a piece of cake, and even the European model wasn't perfect. However, it produced far less of a snowstorm than the American models. The bottom line is that there are countless examples of the European model clearly outperforming the U.S. models, and there are very few examples of the U.S. models triumphing over the European model.

Now, at first glance, it may seem like I'm trying to advocate for the U.S. to simply try to hitch a ride with the European model to improve their weather forecasting. Well, it'd be nice if we could run UW's super high resolution mm5/WRF models using output from the European model, but I believe we could even improve upon the European model if we lumped our resources together. The European model has ten times the computing power of the GFS, yet we have some extremely powerful computers that we would be using that are currently being used for other services, particularly climate prediction. If we could work together with the Europeans to "spread the responsibilities" of meteorological and climatological prediction, we would certainly end up with better forecasts for the short term. Much of climate research is applicable worldwide (after all, when was the last time there was an international conference on Puget Sound Convergence Zones?), but meteorological research pertains to certain areas. We share our expertise on climate with the world, but we have limited access to the extensive numerical prediction programs that are occurring in Europe. If we could further propagate our research throughout the world and create agencies that work across countries (ex: not NOAA or NASA but something that all countries are involved in), I feel like we would have better success. I'm sure there are some agencies like this, but I cannot name any off the top of my head. Regardless, I still think they are a good idea.

Additionally, there is research that has been done by the U.S., particularly for mesoscale modeling, that has not been done on the same scale in Europe. A prime example is our high-resolution models that have a resolution of 4/3 km. This is extremely useful in predicting certain types of weather in certain regions, but it is useless if the models they are initialized off of (like the GFS and NAM) are poor forecasters in the first place. If we could share our knowledge, research, and resources dedicated to mesoscale meteorology with the European's clear advantage in synoptic scale meteorology, amazing things could be accomplished.

But wait, there's more! In the U.S., we have a very cool program associated with the National Weather Service (NWS) called "CoCoRaHS" (Community Collaborate Rain, Hail, & Snow Network) where volunteers send in daily precipitation reports. On average, 18,000 - 20,000 precipitation reports from average citizens all across the U.S. and Manitoba are reported each day. That's a lot of precipitation reports. Because of the higher computer power that the European model has, they can take in more data and therefore obtain better forecasts by being more specific with their numerical inputs and avoiding the need to "approximate" what the weather would be in certain locations between the data points. I do not know if the ECMWF (European Center for Medium-Range Weather Forecasts) has a system like this, and I also do not know if any of the models use any of this data. Still, it just goes to show that there is plenty of data available, and by combining resources with those Europeans, we could achieve even better weather forecasting.

I am technically a CoCoRaHS member but I have had problems with my weather station and haven't sent in reports. It's something I definitely want to do in the future; it's a great way to help education and research applications. You definitely learn a lot about simple ways to accurately measure precipitation and report it to the NWS. Anybody can become a CoCoRaHS member, but you are required to attend a training session (either in-person or online) to be certified and have your reports actually be recognized by the NWS. It's something I'd highly recommend; you can apply here.

I should point out that I believe it is important to have different weather models, however, as the equations that each weather model uses to create forecasts from numerical data are slightly different. Often, the weather that ends up occurring is a "blend" of what was forecast by individual models, so it is definitely important to have different models. Another thing that is becoming more and more common in weather forecasting is the use of "ensembles" of output from models, with each ensemble using a slightly different set of initial conditions. This statistical and probabilistic approach to weather forecasting has been proven to have greater accuracy than the "operational" approach, which just uses all the data from one set of initial conditions (at least to my knowledge, somebody please correct me if I'm wrong). The UW runs their own probability forecasting tool for the Pacific Northwest, and the few times I have used it, it has done an exceptional job, particularly with short-range temperature forecasts. You can learn more about it here.

I know I've written a lot... I'm not the best writer by any means and I'm definitely not as knowledgeable about this subject as I would like to be, but to sum things up, the Americans and Europeans could share the resources they have between them and obtain better forecasts as a result. And as we saw with Hurricane Sandy, the benefits of doing so would be crucial to the health of our economy and the safety of individuals.

On another note, the competition between private sectors can also have negative consequences for the accuracy of forecasts. Most people do not get their weather information from the NWS; they get it from guys like Al Roker, Steve Pool, Jim Cantore, and large commercial organizations like The Weather Channel or Accuweather. Now, my understanding of the economy is extremely poor, as evidenced by this meme I just made.


However, I do know that some weather sites have resources that others do not, and that weather forecasts would be better communicated to the public if these private companies helped each other out and built upon the resources that each of them have.

Perhaps somebody could take these ideas that I have laid forth on this blog and think of some way to practically apply them. But the benefits of increasing weather forecasting accuracy would be huge, and I believe that international, domestic, and commercial cooperation is a very efficient way to do this.

Charlie