Archive for August, 2011

ENSO and US Climate/Weather Revisited

August 25, 2011

I was curious what would happen if I used my “Invariant ENSO Index” to look at ENSO impacts in the US. So here is El Nino versus La Nina temperature composites:


And Now El Nino Versus La Nina Precipitation:


So now let me go out on a limb here and say that, what with usĀ  just having come out one La Nina and going into another one, having had a warm summer across most of the Central and Eastern US and dry conditions in most of the South Central US as a result, it looks like we will be in for more of the same for this next La Nina. This is bad news for Texas and Florida, as it means that we will have a repeat of the drought conditions just when we thought we were out of the woods.

Of course, one can be sure that typical, predictable weather patterns will be played for all they are worth in the media as somehow evidence of our evil human ways, even though years just like the last one and what will likely happen in the coming year, have happened throughout the recorded history of climate in the US, and undoubtedly longer than that. The observational record offers us many opportunities to identify past patterns of weather and the conditions that gave rise to them. What the record tells us is often that the weather we can expect looks a lot like weather we have had in the past. Sometimes that past weather was quite nasty. We better listen and be ready.

The Truth about Extreme Average Temperatures In the US Region

August 5, 2011

One of the common concerns about the alleged doom and gloom from Anthropogenic Global Warming, is that the climate will become more “extreme” in terms of temperature, with both more extreme cold events and extreme warm events. At least when averaged over the region of the world that encompasses the contiguous US, I have just done an extensive analysis that shows that this idea is flat out wrong. In seeking to test the hypothesis that extremes of both warmth and cold would increase in the region of the US during warming, I decided I first needed daily data covering the region. This is available from the NCEP reanalysis dataset, and that data downloadable at the KNMI Climate Explorer. Now, reanalyses have their problems but there performance in characterizing weather and climate should be quite good in a region like the US wherein there are extensive observations to determine their behavior. I would be much more circumspect about using this if A) I were examining a more sparcely observed area and B) the result seemed inconsistent with other observational datasets in the region. Investigations I have done so far suggest that the NCEP data is consistent with other data in the region. Anyway, to define the US region, I’ve had to pretend that the US has annexed small parts of Canada and Mexico, and also this region will include some of the Atlantic and Pacific Oceans, as well as parts of the Gulf. The region is defined as from 24 N latitude to 49 North Latitude, just a little to the South of Western Dry Rocks, Florida, the Southernmost point in the contiguous 48 states that is occasionally above water, and just South of Northwest Angle/Angle Township in Lake of the Woods, Minnesota, Northernmost point in the contiguous US, and from 235 E longtitude to 293 E longtitude, these approximate the longitudes of Cape Alava, Washington and Sail Rock, Maine.

Anyway, after getting daily data averaged over this whole region, I separated data out into calendar years, and ranked each day in each year from coldest to warmest. Subsequently, for leap years, I copied the 183 coldest day (183 warmest in those cases, as well) to be a fake 184 coldest day, so that leap years would have the same number of days as non leap years. I am not entirely satisfied with doing things this way, but it matters very little, from what I’ve been able to tell. I will try to redo the analysis with any other method people suggest if they are interested. Anyway, I then calculated trends for day ranks over the last 32 years (approximately one half the length of the dataset) from 1979-2010 as this corresponds to the satellite period, the period when anthropogenic warming is supposed to be strongest, and in the thirty previous years the global climate appears to have changed little and temperatures cooled in the US. I will also calculate the trends for the first thirty two years for anyone interested if they ask (of course, those trends will have the central year in common in this dataset) but my primary interest is in the satellite period for now. So what did I find? Well, if the temperatures were getting more extreme in both cold and warm days, the coldest days should be slightly cooling and the warmest days strongly warming. If there is even just a net increase in extremes of warmth with no loss of cold extremes, then there should be more hot day warming than cold day, and if there is no change in over all extremes, then all days should show about the same trend. In fact, what I’ve found is that the most warming occurs on the very coldest days of the year, indicating that any increase in warm extremes is more than offset by much larger loss of cold extremes!


The X axis the rank of temperature within each year, y axis the slope of the linear trend line for that set of days from 1979-2010, in degrees Celsius per year.

This finding is consistent with earlier work by Knappenberger et al. Who came to the same conclusion examining different data (temperature stations, as opposed to mainly radiosonde derived products from the reanalysis) and slightly different periods of time. If this cold day warming is a signature of anthropogenic warming, it seems like a pretty nice thing to me. It certainly doesn’t support ideas about the US climate getting more extreme, at least in terms of temperatures. Once again, the results of testing a hypothesis about climate doom and gloom result in the reality being revealed: the world isn’t coming to an end. That’s information worth knowing, I think.