Wilder Weather

When I was a little girl in the suburbs of Detroit, spring’s arrival was marked by the lilacs.  The blooms perfumed our neighborhood and tinted it with shades of cream and purple.  We wove construction paper baskets in school and filled them with blooms, and we even rang neighbors’ doorbells and left the little fragrant presents on their porches, just like the May Day traditions we had heard about from our teachers.  In southern Michigan in the 1980s, the lilacs really did usually bloom close to May Day.

Light purple lilacs in bloom

It’s May Day today.  My red bud tree in Omaha has struggled to push out its buds, but that’s pretty smart of it, since we’re not done with freezing.  Hubby and I are on the couch under a pile of blankets with a fire blazing, but in a crazy juxtaposition, we’re watching baseball.  We’ve heard the pitter-patter of sleet on the windows and deck for a couple of hours, but it’s quieting down now as sleet changes to snow.  It was light until about 8:30 PM, but now the coating of sleet and snow on the ground is reflecting the light and prolonging twilight.

May day!  May day!  We have snow in May!  Abandon ship!

In Omaha, we have had measurable snow in May just four times since 1884.  The sleet alone has accumulated at least a measurable 0.1 inches, meaning that we’ll add a fifth day to the record books.  Five times in 129 years!  This is a rarity, indeed.  The record snowfall for any day in the month of May is 2.0 inches, and we’re forecast to threaten that record tonight, too.

What’s causing this funny business? We’ve had a combination of weather systems and longer-term climate patterns that have squashed our spring.  Low pressure has developed and re-developed in the central and eastern United States.  The low pressure systems drag cold air out of Canada on their back sides, keep clouds around, touch off showers, and generally make the weather cool and unpleasant.  A couple of the bigger picture weather patterns, like the Arctic Oscillation and the Madden-Julian Oscillation, have slightly tipped the pattern toward cooler ones for the eastern and central U.S., also.  Mostly, this has just been the result of a stagnant pattern that’s keeping the warm temperatures confined to other parts of the globe.

Does this mean that all that global warming stuff is just nonsense?  Of course not.  Cold weather will still happen as the planet warms.  It will just happen less often.  In the central U.S., March and April were certainly cold, but the previous several months were warm.

Temperature rankings for November 2012 through January 2013, near the tail end of a long warm spell. Source: National Climatic Data Center.

I think this spring’s cold weather feels particularly nasty because last spring was the very warmest one on record, in stark contrast to this cool spring.  The very last spring in our memory was a very warm one.  Even a normal spring would have felt cold, but a cold spring just feels like winter!

Take heart, friends.  The lilacs, violets, and roses will bloom.  Snow will be replaced with thunderstorms, and crops will be planted and tended.  And it will be sweeter than ever to feel the warm sun on our faces with the May snow in our recent memory.

What a storm system!

The strong low pressure system that has been bowling across the central U.S. has brought freezing rain, sleet, snow, and thunderstorms… and often all of those in the same place!  It’s pretty common to get a strong spring storm that produces thunderstorms in the warm air ahead of it, while snow and wintry precipitation follow behind on the cold side.  But it is not common for the thunderstorms to occur on top of the cold air, and that’s exactly what has happened with this storm.

The air temperatures near the ground were well below freezing, in the mid 20s to lower 30s.  About 1000-3000 ft off the ground, though, temperatures were warmer than freezing. That warm “nose” of air just off the deck allowed precipitation to become liquid in that layer.  If the near-ground sub-freezing layer is shallow, precipitation would fall as freezing rain — the kind that is liquid until it touches the frozen ground, then turns to a glaze of ice.  If that sub-freezing layer is a little thicker, the liquid has time to freeze again before it reaches the ground, and it falls as the small ice pellets that we call sleet.

Ice storm in Lawrence, KS, on March 28, 2009.

On Tuesday, April 9, thunderstorms developed in central to northeast Nebraska.  The layer near the ground was very cold, but just above it, there was enough instability thanks to that warm nose to let thunderstorms get tall.  Ahead of and around the storms, lighter precipitation was mainly falling as either sleet or freezing rain.  In the thunderstorms, the precipitation converted mainly to sleet with a few reports of snow.  But then the thunderstorms got stronger, and they started to produce large hail!  Our weather brains in the weather office kind of exploded a little at the thought of issuing severe thunderstorm warnings for storms that were riding over temperatures below freezing!  Our storm spotters were a little uncertain about whether the ice pellets were sleet or small hail… that is, until the hail got bigger and it was clear!

Hubby and I saw a good thunderstorm develop just south of Omaha on Tuesday evening and hopped in the car to go find some hail.  We were only a half mile from home when we got the first “thunk” of a stone hitting the car.  (And yet, we never had a stone of hail at our house!)  The largest stones, on the west side of the storm, were at least golf ball size.  As we went further east across the storm, the hail got smaller — roughly the size of dimes to quarters — but it fell in copious amounts that covered the ground and the roads. Luckily, our temperatures were hovering in the upper 30s, so the hail was mixed with rain instead of the frozen varieties.

Talk about the weirding of weather!  If this is a harbinger of spring, then this is going to be an interesting storm chase season.

On the bright side, the steady rain for the last several days is giving a beneficial soaking (or wintry coating) to the parts of Nebraska and South Dakota that have been driest.  We’re hoping that it’s enough to make a dent in the drought.

Early in The Long Winter, Pa clearly pays attention to the signs for the coming winter.  He checks the thickness of muskrat dens and notes the patterns of birds flying south.  He talks to his fellow townsmen.  Of course, Pa also listens to an old Indian predict that every 7th winter is severe and every 3rd of those is especially severe (that’s a subject that will earn its own post another day).  He didn’t just trust one thing.  He took in information from all kinds of sources to give Ma his prediction that the coming winter would be a hard one.  And if you think Laura lays it on thick in the book, it’s even more extensive in the manuscript.

Those of us who make weather and climate predictions now aren’t all that different.  Instead of muskrats, birds, and folklore, we turn to computer models and observations around the globe to make our predictions.  But we definitely consult more than one source.  In fact, when it comes to our forecast models, we want as many as possible.  We call it an “ensemble” approach, to take as many models as possible and see what range of solutions they give us. Forecast models are run in the U.S. (mainly from the National Centers for Environmental Prediction, a part of the National Weather Service [NWS]… but also from the military and other federal research labs and universities), Europe (the European Center for Medium Range Forecasts [ECMWF] and the U.K. Met Office), and Canada, for the most part.

Sometimes, they agree with each other about an event pretty well.  When they do agree, we feel a bit more confident about the forecast.  When our maps start to look like spaghetti with all of the different possible solutions — and yes, we literally call those “spaghetti plots” — then we know that confidence is low and there is a wider range of possibilities.

One thing that has caught some fire in the news lately is the success of the “European model” (ECMWF) compared to our federally funded American models.  The ECMWF pegged the track for Hurricane Sandy days before the American models settled on the same track as a most likely solution, and several news outlets made a pretty big deal about it (for example, USAToday, Politico, and Popular Mechanics, just to name a few).  As a forecaster, I can tell you that I’m more comfortable with the ECMWF than most others on most days, especially at longer ranges (4 days out and onward).  It does outperform our homegrown models, on the average.  Like every model, it does sometime get it wrong, too.  It just happens less often.

What makes the European model (I’ll call it the ECMWF here) so much better?  One reason is that it runs at finer resolution for more days out in time — meaning, kind of like a TV or computer monitor, the picture is better when there are more pixels covering the same amount of space.  So it’s basically like an HD TV compared to an old tube TV, especially from about 8 days out to about 14 days.  Another reason is that it takes in more data from real observations to start each model run, and it does it using a method that seems to be better.  And the reasons the Europeans can do these things and NWS can’t is because they have better computers to run all these high-powered calculations.

What’s up with us here in the U.S.?  Why can’t we keep up with the Europeans?

In a word…money.  Federal funding for NWS in general, including our forecast models, simply isn’t keeping up with technological advances that would be needed to improve the models.  We can’t afford to upgrade our computers to improve how we run our models.  We can’t afford the research to know what improvements would be helpful to forecasters.  Heck, we are barely able to keep the lights on in NWS with our current budgets, and we’re running on significant staffing and equipment shortages.  The Europeans can afford it because they charge for their model information, while we Americans let everyone have equal access to it for free.  The Europeans also don’t hire forecasters to provide your weather forecasts and warnings for free, with a network of offices around the country to keep in touch with what’s going on locally.  They are focused much more intensely on pure modeling.

Is that better?  I’m not sure.  I think it’s nice that there’s an NWS office pretty close to everyone in the country, and we have a much bigger patch of the globe to cover.  What we need, really, is enough money to support both.  A forecast model isn’t much good if someone isn’t there to interpret it and make decisions from it.  A forecaster can’t do as good of a job if the tools in our toolbox aren’t sharp.  We need both the models and the forecasters to give the best forecasts to our American citizens.

How do we get better models in our National Weather Service?  Well, since I’m a federal employee, I really can’t tell you what to do, even though I’m on my own time and my own blog and my own equipment now.  I’ll leave it to your imagination to think about what to do from here, keeping in mind who it is that makes the decisions about our budgets in a federal agency. 😉

This is still a weather/climate/Laura blog, right?  So why am I posting about the recent study in Pediatrics that investigated the cause of Mary’s blindness?

In a word…

SCIENCE!

I love that scientists can continue to connect their work to their fond childhood memories of reading Laura Ingalls Wilder books (or watching the TV show).  I love that fans of the books can get to talking about science when a cool investigation comes out.

For those who are catching up, a team of medical researchers put their heads together to try to diagnose the the illness that caused Mary’s blindness.  The article, which I first saw at USAToday, has made an appearance on the front page of CNN’s website, not to mention a host of other news and blog sites (CBS, New York Times, LiveScience, Detroit News, NPR, People, and UK Daily Mail, just to name a few).  If you’ll pardon the pun, it has gone viral!  And all because a medical school student remembered hearing about scarlet fever when she read the books as a kid and connected it to her medical school education later in life.  I totally get it.

The ever informative Nancy Cleaveland pointed out that another researcher came to a different conclusion in a project that was discussed in the Homesteader newsletter (chicken pox).  Nancy wondered why this new study is gaining traction over the old one, and it gives me a great opening to talk about the scientific process a bit.

Scientists trust peer-reviewed articles above all others.  These articles, published in very specialized journals, are given to at least 2 or 3 specialists in that field to review.  Let’s take my area of specialty as an example, because I can discuss it knowledgeably.  Eventually, I will submit pieces of the work I’ve done to one of the well-regarded journals in my field — probably the Journal of Climate.  The article will be reviewed by people who have very specific expertise in the very specific aspects of my study — statistical analysis of data, using modern data to investigate historical events, and global climate patterns like El Niño and La Niña.  Those reviewers will tear apart my data, scrutinize my methods, and dig into my conclusions, checking along the way that they think I’ve used the right data and the right techniques, that I’ve used those data and techniques correctly, and that my conclusions are supported by those data and techniques.

Not one of my reviewers, though, will be a Laura expert.  If I want to get those parts correct, I have to run it by some of my Laura expert friends first.

Peer review is the best process we have to show other scientists that we are doing credible science.  It is not a flawless process.  One of the primary ways that mistakes get into peer-reviewed literature is when the material is not in the specialty area of the journal.  If I’m using a paper from the Journal of Climate, I’m not going to use it to verify, say, the life cycles of frogs.  I’m going to use it to verify climate techniques, and if the article happens to discuss the life cycles of frogs in relation to climate, I’m going to pretty much take their word that the frog stuff is all right.  Likewise, when I publish a paper in the Journal of Climate, the reviewers will take for granted that I got the Laura stuff correct, because it’s outside their areas of expertise.  The paper will be credible as a climate paper, but it would be questionable for hard-core researchers to use it as, say, a literary analysis of Laura’s storytelling techniques, because it wasn’t reviewed as a literary paper.

I trust the medical analysis of the new study because it passed peer review of other doctors.  The authors did their due diligence to get Laura’s story right, but I don’t necessarily turn to this paper as the final word on Laura’s story.  I do think, though, that we can turn to it as a credible medical explanation of what happened to Mary.  Until another explanation passes through peer review and makes it into a medical journal, it’s the best explanation that we have.

That is how science works!  We trade evidence among specialists as we work toward getting the best explanation that current evidence can give us.

I make this point because from time to time, confusing information about climate change sneaks through peer review.  It often sneaks through in journals that don’t specialize in climate and don’t have reviewers who have expertise in climate.  They take the leap of faith that the authors got the climate stuff right, while focusing on their expertise in, say, coral reef biology in a journal that focuses on marine biology.  Most authors do their due diligence to get the rest of the story correct.  Some authors have an agenda, or just don’t have all the knowledge that they should, and they put information into those papers that goes against the evidence known in the climate field.  It’s important to know where the body of evidence is pointing when it comes to science.  It’s also important to know which sources are credible.

We continue to add evidence to the research on just about every weather and climate phenomenon out there.  Sometimes, the evidence is in good agreement, such as the overwhelming body of evidence that humans are increasing carbon dioxide in the atmosphere, which is causing warming that is causing all kinds of changes to weather patterns, ocean currents, and plant and animal life.  Sometimes, the evidence is murky and unclear, like whether or not the number of tornadoes will increase as climate changes.  Climate change will have all kinds of impacts on our health, and climatologists and doctors will have to team up to publish papers, to make sure that we get both the climate and the medical science right!

Laura and her family (both as a child and as an adult) lived a very simple life, close to the Earth.  They raised their own food, built their own things, and reused whatever they could.  But they did not shy away from technology and advancements in many cases, either.  Laura was allowed to buy name cards, and she spent her own money on pretty hats and clothing.  Pa may have turned his nose up at threshing machines, but Almanzo sure didn’t.  The elder Wilders owned a car and traveled long-distance several times.

We talk a lot these days about things like “eating locally” and “carbon footprints”, hearkening to days when people did eat food grown close to home and did not belch so much carbon dioxide into the atmosphere just to live their lives.  But just how “green” was Laura’s lifestyle?  And how “green” would she be if she were somehow lifted out of DeSmet as a teen or young adult and planted into 2013?  (For the sake of simplicity, let’s just focus on Laura around the 1880s.)

Certainly, I believe that even a modern Laura would have an extensive garden, if not a small farm.  She’d raise chickens for both eggs and meat, and she would get virtually all of her vegetables from her own garden.  Modern Laura would be a model for eating locally, as well as using as much as possible without wasting.  She’d have a compost pile.  What she didn’t reuse, she certainly would recycle.

I bet Ma and Pa would have kept the thermostat on their heating system turned pretty low in the winter.  With the scarcity of wood in South Dakota, I imagine they would rely on the modern comforts of gas or electric heating, just as most households do in this country.  The Ingalls family might have admired geothermal heating, but I doubt they could afford to install it.  I wouldn’t rule out a solar panel on their roof, but even those cost some money to install.  Turning down the thermostat to something in the mid-60s is how they would save money on energy costs.

But Laura was one for the occasional shiny gadgets.  Her 1880s name cards and autograph books become the modern iPhone and Facebook page.  Her schoolgirl slate becomes a laptop computer, and she’d spend hours researching, studying, and writing reports, even when she occasionally posted on Ida’s Facebook wall about getting together with Mary Power and Minnie over the weekend.  She might even text Mary once or twice, though Ma might take away her phone until her homework was complete.  Of course, all of these modern comforts require electricity to produce and ship, let alone to use, and electricity for energy is the biggest way that we modern folks are putting extra carbon dioxide up in the air.

Wouldn’t those cutter rides really just become modern cruising in a car?  Almanzo might really have a nice “pony” … a shiny, well-waxed classic car that has been carefully restored and meticulously kept.  Buggy rides to the lakes might turn into car rides out to see the sights and visit some places that were just far away enough to be out of the parents’ watchful eyes.  With a car instead of a buggy, the couple could venture farther than just the Twin Lakes.  They could drive over to those distant Wessington Hills, or maybe just down to Sioux Falls to hang out at Falls Park.  It takes a lot of food and energy to keep livestock, but all of those weekend car trips certainly add carbon dioxide to the air.

I ran Laura’s lifestyle through one of the many carbon dioxide footprint calculators available online (The Nature Conservancy’s Free Carbon Dioxide Footprint Calculator, but there are dozens of others).  Laura’s footprint of 17 was below the average U.S. person at 27, thanks to savings on home and water heating, eating organically and only occasionally meat, and recycling and composting.

How do you score?  At 27, I matched the national average.  My energy efficiency at home (we set the thermostat at 62 in the winter and use energy efficient appliances) was not enough to offset my travel habits or the fact that I don’t compost.  You’ve got me beat, Laura!  Now, what can I do to reduce my footprint?  Who wants to visit and help me start a compost pile? 🙂

The change of the year is upon us, and 2012 will go in the books as a year of superlatives.  In many places in the U.S., it was the warmest year on record.  It was a year of extremes, from fires in the Rockies to (Hurricane/Superstorm) Sandy.  It was among the quietest years for tornadoes on record, and yet we still saw the largest outbreak on Christmas Day in the records.

What will 2013 bring?  Will we get a quiet year after such extremes, or will those patterns continue into another year?

Well, one thing 2013 will bring is more from me, thanks to my New Year’s resolution to practice daily writing.

When I go to work tonight, I’ll look at the records for 2012 in Omaha, Lincoln, and Norfolk (all in Nebraska).  My job will be to untangle all the records and see if we set records for the warmest year ever in Omaha and Norfolk (Lincoln will be somewhere in the top 10, too.)  At the other National Weather Service offices around the country, climate weenies like me will be doing the same thing, combing through the records for the end of year summaries.  Watch for those links here and on the Wilder Weather facebook page!

Writing for 15-30 minutes every day will allow me to push out everything from academic journal articles to book chapters to blog posts here.  I’m sure I’ll need inspiration on some of those days, so please send me your weather and climate questions, whether they are inspired by events in Laura’s books or observations out your own windows!

We watched the forecast come together for a good 7 or 8 days.  It looked like a storm system would affect the Central Plains.  It looked like it could be cold enough to snow.  Then it started to look like it could be a bit windy.  I had the good fortune of working the forecast desk on Monday and issuing the Winter Storm Watch for my area, drawing my axis of heaviest snow right over my Omaha, which was later converted to a Winter Storm Warning and then to a Blizzard Warning for Wednesday and Wednesday night.

And then Wednesday came.  Light rain began around 1:00 PM, and it began to mix with snow about an hour later.  By about 2:30 PM, we were getting mostly snow — a heavy, wet, sticky snow.  We got several inches of snow before the wind kicked up, much of it in the form of big, pretty flakes and just enough light breeze to move them around like the inside of a gently shaken snow globe.  We even saw lightning and heard thunder — thundersnow!  By mid-evening, winds were increasing, and the snow took on the look of finer grains that had been shattered by collisions in the wind.  (For a cool time lapse taken from our front window, head here.)

The fruits of our mid-storm labor: The frosted cookies

And then the power flickered.  We were frosting our Christmas sugar cookies, and we looked at each other with our attention grabbed but our concern low.  In my four years in Omaha and three years in Iowa, I had never lost power… even through three or four blizzards and a handful of severe thunderstorms.  The lines in our neighborhood are buried, and Nebraska isn’t exactly a haven of trees.

I grew up in rural northern Michigan, which is pretty much the opposite of Nebraska, with abundant trees and above-ground wires.  Power outages were simply the norm up there, in all seasons.  We stoked the fire in the wood stove during outages.  We ran water when storms were coming (either the thunder or the winter varieties) so that we could power-flush the toilets and wash ourselves, since we got our water from well that required an electric pump.  I was used to outages there.

But when the lights went out between 10-11 PM on Wednesday, we were absolutely unprepared.  We frosted the last of our cookies in the dark, washed the dishes, and kept the gas fireplace running to provide a little heat.  We put on warm jammies and got deep under the covers.  We normally keep our house on the cool side to conserve energy, so we didn’t have far to fall to get into the lower 50s by morning in the house.  We woke to no power.  After shoveling the deck and blowing snow off the driveway, we took our dog to the doggy day care so that he would have a warm place to play, and we headed to work.  I ran the space heater about 3 feet from me for the rest of the morning.

I didn’t wake up to ice crusting over my comforter.  I didn’t have to break ice in the water pail to melt for washing my face.  I was cold while getting dressed, but I couldn’t see my breath inside.  When it comes right down to it, I was inconvenienced for about 12 hours.  I didn’t have to endure worse for six months.

And best of all — I knew it was coming.  Not just because I’m a meteorologist, either — I’m pretty sure everyone in Omaha (and the rest of Nebraska and Iowa) knew it was coming.  We have the ability to see storms like these for about a week in advance.  Imagine how much hay Pa could have hauled if he knew when the next storm was coming, or how much that information would have helped Almanzo and Cap make the seed wheat run.  We might lack some of the details, like when rain would change to snow or which area within about a 100 mile width would get that heaviest band of snow.  But we can get the flavor of the storm, and we can do a darn good job tracking it.

By the way, west Omaha got under that heaviest snow band, and we got a good 8″ or more of heavy snow.  Our winds gusted to about 45-50 mph.  I don’t know yet if it will go in the books as a blizzard, but it was a heck of a winter storm.

And thankfully, my power is back on and I can tell the story!

You’ve got to be kidding me!

I looked out the window of my Omaha home on the morning of October 10, 2009, and saw a few inches of fresh snow covering the ground.  Sure, we had been talking up the chance for a little snow to mix in overnight in the weather office.  And being the eager weather weenie, I had even gotten up with my husband in the middle of the night to watch the first flakes flying.  But 5 inches?  In early October?  I was not ready for this!

As the climate person in our weather office, I started receiving questions almost immediately:  Does a snow in October predict a hard winter?  What has happened in other years when it snowed in October?

Well, I knew about one October snow in the past:  October 1880, the ominous foreshadowing of the fierce Hard Winter.

I had just started to tinker with studying The Long Winter in 2009, but I had not yet grabbed the data to put dates to the big events.  I started that work just two weeks later, according to my email files, spurred into deeper research by the hard winter unfolding around me.

We don’t have weather observations in DeSmet for the winter of 1880-1881, at least not documented ones.  We don’t even have them for Huron.   We do have several sites around the region, surrounding DeSmet in just about all directions.  (See the map below for a reminder of where the data sites are located.)  Those sites all have daily records for the Hard Winter, at least as much as observations were taken in those years.  Observers did not measure snow in the early 1880s, but with measurements of both temperatures and precipitation, we can make a pretty educated guess about whether the precipitation fell as rain, snow, or both.  Occasionally, observers were even helpful enough to put in their notes that snow had fallen.

Map of sites with weather observations in 1880-1881 surrounding DeSmet.

For many of the sites, here is the weather that was observed around mid-October:

Let’s look at these closely.  On the 13^th and 14^th, the high temperature was quite warm around the area, ranging from the upper 50s to the north (Fort Sisseton) to the lower 70s southward (Omaha and Ft. Randall).   Even the low temperatures were above freezing everywhere except in Fort Sisseton.  These are not our blizzard days!

On the 15^th, cooler air is clearly working its way into South Dakota.  Both Fort Randall and Fort Sisseton only reached the lower 30s for highs, and Fort Randall even reported snow, though it was dry in Fort Sisseton.  Even though they are pretty close to each other, Yankton was quite a bit warmer on the 15^th, reaching 54 degrees, and Omaha and Minneapolis/St. Paul both stayed warm.  This says to me, with a “weather eye” on the observations, that there was a strong cold front moving in from the west/northwest, while rain was spreading up from the south and changing to snow as it encountered the colder air.

The snow really got going in the area overnight on the 15^th and into the 16^th.  Cold air reached all of the sites except for Fort Bennett, which seems to have been just far enough out of position to miss the core of the storm.  The precipitation in Omaha probably was a very cold rain or a rain/snow mix on the 15^th, while Fort Sisseton was reporting snow and even Minneapolis/St. Paul probably saw rain changing to snow during the day.  Snow continued into the 17^th at both Fort Sisseton and Minneapolis/St. Paul, with temperatures near or below freezing at all sites.  Snow even continued into the 18^th at Minneapolis/St. Paul, with some light snow appearing likely at Yankton and Fort Randall.

Once the storm departed the area, temperatures bounced back rather quickly, with highs in the 40s to 50s across the area by the 19^th.

So, that covers the snow.  Now, let’s talk about the wind.

We have all kinds of gadgets to measure wind these days, but back in the early 1880s, it was largely estimated based on technology like wind socks and the Beaufort scale.  I have these records, too, but I won’t scare you by posting them here.  They’re not pretty.  Let’s just say this:  It was windy during the October snow.  Winds were strongest on the 15^th and 16^th, though Fort Sisseton got into some wind even on the 14^th.  More importantly, I can see that the wind direction shifted from southwesterly ( a warmer wind) to northwesterly (a cold wind) on the 15^th.

Now, it’s time to put together the whole story, from the weather perspective!

A storm system moved up from southwest Colorado toward eastern Nebraska, while cold air was dipping out of Canada due to a weaker storm system moving through North Dakota into Minnesota.  The initial shot of cold air brought near-freezing temperatures and a little bit of precipitation up north on the 14^th.  The low pressure system deepened on the 15^th as it got spinning in eastern Nebraska, pulling cold air around behind it while it brought moisture up from the south.  Then, the low pressure just sat there for a while and deepened.  As it got deeper, the winds behind it – in eastern South Dakota – got stronger.  The storm stayed in the area of northwest Iowa to southern Minnesota through the 16^th, then pulled away into northern Michigan on the 17^th, leaving cold air and breezy conditions behind it.

Snow in October is always kind of stunning.  It shocks us into the reality that winter is approaching quickly, and that we’d better hurry our preparations before we really get caught.  In Laura’s case, the October blizzard indeed was the first strike of many during an exceptionally cold and snowy winter.  In my case, the October snow also was the first strike of many during a winter that started among the coldest and snowiest.  Luckily, for me, the winter ended a little more “normally” once we got past mid-January, which I can probably at least partially credit to climate change causing warming temperature trends.  I can’t imagine what it was like to endure another three months.

Oh, and if you were wondering:  No, a snow in October does not necessarily predict a hard winter.  Snow has been measured in October in Huron 43 of its 120 years with snow records.  The winters following those snows had no tendencies – they were pretty evenly split between warm winters and cold ones, snowy winters and not snowy ones.

*Thank you to the person who corrected my math in the comments :).  Indeed, 2012 is 132 years after 1880, not 131!

The Detroit Public Library long has been the home of the handwritten original manuscripts of The Long Winter and These Happy Golden Years.  As a part of my Hard Winter research, viewing the manuscript for The Long Winter was high on my list of research necessities.  The University of Nebraska’s Center for Great Plains Studies was even kind enough to bestow on me a travel grant to cover the expenses of traveling to Detroit to conduct this research.  I planned my visit to Detroit in the midst of a long summer trip that took me to Laurapalooza, then to eastern Iowa for a friend’s wedding, and finally to Michigan to do research and then visit family.

I was expecting to view the manuscript on the Tuesday after Laurapalooza.  I called ahead on Friday, as a courtesy call and to see if I needed to set an appointment.  I almost drove off the road, though, when I heard these dreaded words from the librarian in the historical collection:

“The manuscripts are out on loan…

… until September 2013.”

What?!  They’re manuscripts!  They can’t just be loaned willy-nilly!

Upon further investigation, I learned that the manuscripts had been sent to the Michigan Historical Archives in Lansing to be used in a museum display.  I asked the librarian in Detroit if I would be able to view the manuscripts up there, and he said I’d have to get in touch with them.

I scrounged around online until I found the Archives of Michigan, which oddly is now a part of the Department of Natural Resources.  I called the number and spoke to a young lady who gave me the name of the person who has been charged as the keeper of the manuscripts – a Julie Meyerle.  I left a message for her on Friday afternoon and hoped that she’d be around to return a call.

And I waited.  The weekend passed with no word.  I tried to call her again on Saturday and Monday and still had no success.  Hubby and I spent our time in Detroit at the Henry Ford Museum and Greenfield Village to get a taste of history.  We even watched a Laura presentation at Greenfield Village (not bad, if you ever catch it there!).  But it was no replacement for the deep research I needed to do for my dissertation and writing.  Our trip continued on to Higgins Lake, Michigan, as we still had no word on whether it was worth our time to stop in Lansing.

Finally, on Tuesday at about 1pm, I got a call from Julie:  Yes, I could come down and view the manuscripts in Lansing!  I got her message at 1:30pm, and we were on the road by 2pm.  It was a 2-hour drive from Higgins Lake to Lansing, with my husband graciously speeding to save me a few precious minutes while also allowing me a chance to prepare my mind.  I was going to see Laura’s own words, in her own handwriting!

I know that museums and archives have rules and standards for handling and viewing manuscripts and other historical documents.  I had a vague sense that in Detroit, it’s OK to take non-flash pictures, but I wasn’t sure if handling the manuscripts was allowed there.  And I had no idea what the Archives would allow.  Hubby and I checked in with our drivers licenses, put all belongings in a locker (except for an iPad that they allowed, without its case), and sat at a desk.  We were sternly lectured to not take any photographs (even non-flash) of the manuscripts, which I had actually been counting on doing.  Hubby did coax them to let him take a couple of pictures of me, hard at work.

The archivist brought out the manuscripts and laid them on the table in front of me.  Breathless and shaking, I opened the tablets and read her words, her pages.  I noted differences from the published version, including many juicy tidbits that may help me identify the weather events a little more specifically and have given insight into how the family coped.  (I will not be revealing the details on those… you’ll have to wait for the book!)

Barb hard at work on the manuscript review.  Photo by Josh Boustead.

I had arrived at 4pm, and the Archives closed promptly at 5pm.  It was nowhere near enough time to page through the Hard Long Winter manuscript and take all the notes I needed.  I was only about two-thirds of the way through, and that had been rushed and frantic.  I’d have to come back the next day, sacrificing a trip to the wineries of northwest Michigan with my mom to do so.  From opening time promptly at 1pm until around 3pm, I continued to diligently take iPad notes.  I even left myself enough time to glance through These Happy Golden Years for some of my favorite weather events, with a few more juicy tidbits that you’ll have to wait to hear!

Thus ended my research time with the Archives.  I’ve later learned that the Detroit Public Library only allows handling with gloves, and that mainly by their own people.  I have to admit that I was pretty shocked about being able to handle the manuscripts myself, bare handed.  Actually, when I mentioned it to Julie after my visit, she also was surprised.  (The archivists seemed more concerned with being able to see that I wasn’t pocketing the books – I was asked a couple of times to move items to the side so that they could watch me from their desk unimpeded.)  Take heart, historians – I washed my hands and used the utmost of care when handling those books.  And perhaps the group will be more careful to ask any viewers to use gloves from here forward, now that they are aware that my viewing was without gloves.

I learned from Julie after my visit that the books will be a part of the display called “Put it on Paper”, which celebrates the process of taking creative vision (art and writing) from the mind to the paper.  The exhibit will be on display in Lansing from September 29, 2012, through the fall of 2013, and a link will be posted from the Archives website once the exhibit is up.  During the display, the manuscripts will not be available for private viewing and research.  If you had designs on doing research on either of these manuscripts, this will certainly affect your timeline!  I am lucky that I viewed the manuscripts in the nick of time.  And I’m thankful that I did, because some of my findings are just THAT good!

Note:  This article also has been posted at the Beyond Little House site.

My, what a couple of weeks it has been!  I have so much that I want to share, but for once, I’m going to let the Ma/Mary in me win… I’m going to save my explosion of topics to distribute bit by bit, like Laura and the girls prolonging their stories in the Youth’s Companions during the Long Winter.

So, for my first installation, I’d like to talk about Laurapalooza 2012.  This is probably as far into Laura-dom and away from weather/climate as this blog will ever go, but I think I’d be remiss not to give my perspective on this awesome event!  My trip to Laurapalooza was the beginning of a 12-day excursion away from home, so I loaded the car with enough to sustain me for weeks to attend a conference for only one-and-a-half days!  My friend Cindy, a high school English teacher in Sioux Falls, joined me for her first immersion in the world of Laura.  (I hope we didn’t scare her!)

At the first Laurapalooza in 2010, I didn’t know a single other attendee.  I expected to feel out of place, a scientist among teachers and librarians and historians.  Boy, was I ever wrong!  I found kindred spirits there, a group of fascinating people who had woven Laura into their lives in some way, either as a common thread or as a dominating fabric.  My little weather presentation, which I thought would be more interesting to me than anyone else, ended up garnering rave reviews and inspiring me to take a little side project and create a dissertation out of it.  I made friends over late night beers and hallway conversations, folks who became Facebook friends and even house guests.

Due to the wedding of my dear friend Erin, my time at Laurapalooza was limited to only the first day and a half.  I knew I had to pack in as much as possible during that short time!  I’ll reveal more about my presentation in a later post, including stuff I didn’t have time to cover at Laurapalooza (teaser alert!), but my topics included heat, drought, the Brewster school cold snap, and the tornado from These Happy Golden Years… some of my favorite topics from the books (besides the Long Winter, of course!).  I had the pleasure of tying another presentation to Jim Hicks, and despite stumbling over what ended up being a VERY old slide that snuck into my talk (GRRRR!), found out that we had done research that once again came to the same conclusions about weather-related events!

On Thursday evening, the Bonnet Heads overwhelmed the locals at the Wine Cafe and OWNED karaoke night!  We crushed the classic prairie ballads, such as “Pour Some Sugar on Me”, “Where Have All the Cowboys Gone”, “Like a Virgin”, “Alone”, “Enter Sandman”, “Strut”, “I Love Rock and Roll”, “One Way or Another”, and “You and I”.  (I’m sure there are more, too… because by the end of the night, we pretty much sang along to everyone’s songs!)  Our performances earned us wild applause, a few raised eyebrows for our costumed sisters (Melanie and Kelly), and a round of drinks from the local softball team.

I’m sure glad we closed the place down, because by the time Cindy and I got back to the dorm and finished our post-ballad chatter, thunderstorms were moving into Mankato!  With the drought I’ve been experiencing (more on that in later posts, too!), storms have become a rare treat for me!  I tried my hardest to stay awake to watch the lightning, but I just couldn’t keep my eyes open long enough to hear the foreign sound of rain pattering on the window.

Of course, the best way to turn around from a night of karaoke fueled by adult beverages (WWLD?) is to lead a group of children in weather activities bright and early the next morning at Camp Laura!  With Cindy’s assistance, we talked about our favorite weather events in the Laura books, built weather vanes and tested them, and identified cloud types.  I left the campers with a few more weather activities to try at home and Owlie Skywarn books for some modern coloring!

My short stay at Laurapalooza 2012 was an absolute blast!  My favorite parts, other than the stuff I’ve already described :), include tasting Long Winter bread with our churned butter, conversing with the authors at the evening reception, listening to great talks about what Laura read and about Dr. Tann and about the Brewster school, and seeing all the lovely and familiar faces while meeting a few new ones!  I can’t believe we have to wait three whole years for the next Laurapalooza, but I’m already looking forward to it!