Beyond the Data Blog
It’s early February, and many of us just dug out—literally and figuratively—from the blizzard of January 2016. We got 6-12 inches here in Asheville; the totals varied from mountain to mountain, like they always do. The snowstorm also buried me under 25 feet of snow-related paper, and that’s what inspired this week’s blog.
Putting today’s big weather events into perspective is one of our responsibilities here at NCEI. People and businesses are naturally curious about whether today’s Big Event is dwarfed by history, repeats history, or makes history. This helps us map it out in our minds and in our strategic plans, and that helps shape our actions going forward.
We need&nbs…
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Welcome back—belatedly—from the holidays. For those of us east of the Mississippi, it didn’t feel like the holidays. Well, it did feel like a holiday—Memorial Day, maybe. In fact, for some of us, the weather felt a lot more like Memorial Day than the holidays we celebrate as the year closes.
The year ended with an unprecedented warm run in the United States. The last 5-6 weeks of 2015 were very warm east of the Rockies. But how unusual was it?
Just how warm, nationally?
On a national scale, December was both the warmest and wettest December on record for the contiguous United States, or CONUS. That in itself is a feat. It’s the first time since the CONUS record reached statistic…
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This week, Beyond the Data looks at one of the more well-grounded “rules of thumb” for understanding climate change. This one is pretty simple to put your thumb on: on average, cooler places and cooler times are warming more quickly than warmer places and times.
But first, let’s clarify–and emphasize–what we mean by a “rule of thumb.” Just like in its common usage, a rule of thumb here refers to something generally true often enough to be useful and informative, but not universally reliable–kind of a “two-out-of-three” or “three-out-of-four” kind of situation.
So, it's nothing to thumb your nose at, because it’s true more often than not. But it’s also not the case everywhere. &nb…
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Many factors contribute to the climatology of a given location, including how close to the equator you are, proximity to the ocean, and elevation. But when it comes to what causes climate to vary over seemingly short distances, few things can compare to the influence of topography.
Take my city, for example. I live in Asheville, in western North Carolina, a small city in the heart of the Southern Appalachians. I can drive ten minutes and be in one of the driest locations east of the Mississippi, or drive an hour and be in one of the wettest. That the temperature and precipitation patterns that we experience here can be so different from somewhere just a few miles away is due not just to e…
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Let’s face it: El Niño is the life of the party. He’s the Most Interesting Child in the World. The good folks over at The ENSO Blog have filled up a whole blog, and still there are enough leftovers for Beyond the Data, where we don’t always blog about teleconnections, but when we do, we prefer El Niño.
We’ve already written about how El Niño will push the needle toward 2015 being the warmest year on record. But thinking a little more directly about the state of the climate in the U.S., how might a strong El Niño impact things here? Will it put a dent in the Western U.S. drought, one of the defining climate events of the decade? What about the rest of the country?
If you’ve been followi…
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