Adjusting for the "Rural Cooling Effect"

I spent quite a bit of time today ploughing through USHCN station data, doing a lot of grunt work. For example, I spent time aking a concordance of 1221 USHCN identification numbers with GHCN id numbers (they aren’t the same) and I haven’t seen a concordance anywhere. Most of it could be done through matching lat-long neighborhoods and common name starts. I got all but 3 matched through 3 fairly ad hoc rules. It was actually easier than the smaller Jones China concordance because the latitudes and longitudes were all correct or correct within a very close rounding error. One of the reasons for doing this is that Hansen et al have arrchived their lights value for GHCN id #, but not for USHCN id #. I’ve collated a data file for all USHCN stations which also looks up the GHCN metadata: lights, vegetation, topography. They have a lot of codes and metadata, but they don’t appear to have a code for parking lot or for whether an electric light is in the box with the thermometer. The data file is here.

In the Hansen temperature calculation, he says that the long-term trends are defined by “rural” stations, defined in Hansen et al as having lights=0 according to their brightness index. Having collated the lights information with USHCN identifications, I then extracted the California stations with lights=0.. Details (excerpted from the larger file above) are here. There were 17 such stations, a couple of which we’ve discussed over the past few days, courtesy of Anthony Watts: BRAWLEY 2SW, CEDARVILLE, CUYAMACA , DEATH VALLEY, ELECTRA PH, FAIRMONT, FORT BRAGG 5N, HAPPY CAMP RS, INDEPENDENCE, LAKE SPAULDING, LEMON COVE, NEEDLES FAA AP, ORLEANS, SUSANVILLE AP, TEJON RANCHO, WILLOWS 6W, YOSEMITE PARK HEADQUARTERS.

Lake Spaulding is one of the 17. It’s the one with the weather station attached to the boat in the parking lot. It turns out that until recently there was a much better location for the station, but it was recently changed to a site that is worthless. One wonders why IPCC has never stated that sites like the old Lake Spaulding are valuable for long-term weather keeping and at the total mismangement of the system in which Jones and Hansen have failed to oppose such changes.

I’ve collated 7 different versions for each site: the three USHCN versions (areal, time-of-obs adjusted, filnet (Which is mainly Karl’s Station History Adjustment), 2 GISS versions: raw and adjusted and two GHCN versions: raw and adjusted. By and large the threefold adjusted USHCN version is approximately the GISS raw version. In each case, I plotted out the impact of the various adjustments from USHCN raw to GISS “raw” to GISS adjusted.

A few patterns seem to emerge. First, in the majority of these “best” sites, there is a warm 1930s. The net impact of the several adjustment stages is to reduce the 1930s relative to the end of the 20th century. Probably the largest contributor to this was the USHCN Station History Adjustment, which is done according to a procedure of Karl and Williams 1987. (Karl, T. R., and C. N. Williams, Jr. 1987. An approach to adjusting climatological time series for discontinuous inhomogeneities. Journal of Climate and Applied Meteorology 26:1744-1763. Whatever the “good” reason for this adjustment, the main practical effect seems to be the lowering of past high temperatures. It also seemed that GISS was very likely to exclude past high temperatures from their collation, but were like a dog on a bone for past low temperatures. I’ll show one station to give a flavor of what I was doing.

The first plot is a simple spaghetti graph of the 7 different annualized versions as shown below, showing warm 1930s in this case.

Figure 1. Spaghetti graph of 7 versions of station history (1961-1990 anomaly basis)

The next is a plot showing 3 stages from USHCN raw to GISS adjusted: from USHCN raw t0 USHCN filnet (adjusted); from USHCN filnet to GISS raw (these tend to be very close) and from GISS raw to GISS adjusted. In this case, the USHCN adjustments collectively increased the trend by about 1 deg C and the GISS adjustments another 1 deg C.


The next figure disentangles the USHCN adjustments by type. The time-of-observation adjustment makes little difference, but the Station History Adjustment makes a large difference.


USHCN station history information is described here , while the station histories are at . This file is extremely hard to read as it uses lots of indicators in Fortran punch card format.

begin_date dist_prev_loc conf_dist_move dir_move elev_chg hgt_chg CRS DT MN MX MMTS
05 01 1894 NA 0 999 NA NA 1 0 1 1 0
02 01 1914 0 0 0 0 0 1 0 1 1 0
10 01 1937 0 0 0 0 0 1 0 1 1 0
04 28 1938 0 0 0 0 0 1 0 1 1 0
03 01 1949 0 0 0 0 0 1 0 1 1 0
04 01 1950 0 0 NNE 0 -2 1 0 1 1 0
04 20 1957 0.1 0 S -3 2 1 0 1 1 0
02 12 1959 0.2 0 N 0 0 1 0 1 1 0
03 20 1960 0 0 NW -2 0 1 0 1 1 0
07 24 1969 0.2 0 NNW 0 0 1 0 1 1 0
08 16 1974 0 0 0 0 0 1 0 1 1 0
09 12 1975 0 0 E 0 0 1 0 1 1 0
11 02 1977 0 0 W 0 0 1 0 1 1 0


  1. Andrey Levin
    Posted May 29, 2007 at 3:04 AM | Permalink

    I got a heretic idea.

    May be it would be vise to let weather stations to predict, well, weather, and for climate ‘€” both regional and global ‘€” use satellite measurements?

  2. Hans Erren
    Posted May 29, 2007 at 4:13 AM | Permalink

    Compare the giss “adjustment” of De Bilt, with mine and local Expert Arjan van Engelen (KNMI)

  3. Posted May 29, 2007 at 7:15 AM | Permalink


    I have the Cedarville site on my list to visit in early September when I will be in the area, unless it gets real important and then I can make a special trip. Here is some information and photos on the Susanville Airport, which I have a full set of pictures. Here are some samples:

    General Photo

    Looking West

    Former Shelter Location

    The site was automated and moved to the end of the airport runway in 1996 from an area south of a hanger, west of the airport office behind the service area. See the photo of yellow fire truck sitting on the former site location. The temperature sensor is in the PVC pipe, with a fan to draw the air over the sensor. According to the site manager, they only use the station data for local air operations. To his knowledge, none of the data has been reported since the site was automated in 1996. However, the equipment does include a modem and can be called by weather reporting agencies, although the site manager did not know if this was normal operations. The shelter used before 1996 was not painted, only white washed, according to the retried station manager in a phone call.

  4. Hans Erren
    Posted May 29, 2007 at 7:32 AM | Permalink

    Beware that GISS uses the meteorological year Dec-Nov

  5. Steve McIntyre
    Posted May 29, 2007 at 8:24 AM | Permalink

    #2. Hans, did you ever figure out how GISS made their adjustment to the De Bilt data.

    #3. Russ, do you have any information on the Independence CA site, also in the GISS 17.

  6. JerryB
    Posted May 29, 2007 at 8:31 AM | Permalink


    FWIW, it appears that Susanville airport data is collected, usually each day:

  7. Don Keiller
    Posted May 29, 2007 at 8:31 AM | Permalink

    Steve, What do RC have to say about this and other “adjustments”?

  8. Posted May 29, 2007 at 8:45 AM | Permalink


    Not at this time, but will put it on the schedule. I am going to Blue Canyon today. Pictures later this evening.

  9. Hans Erren
    Posted May 29, 2007 at 8:46 AM | Permalink

    re 5:

    It looks like GISS cannot handle jumps properly and puts a gradient in place.
    Look at Uccle, Sneyers is the local (KMI) expert, but he doesn’t adjust for UHI change.

  10. Murray Duffin
    Posted May 29, 2007 at 8:49 AM | Permalink

    I don’t understand. The spaghetti graph shows a GHCN adjustmet up prior to 1910, down from 1910 to 1970, and then up again from 1970. Can some one explain to me how the adjustments are made? Why is 1910 to 1970 history adjusted down? what is the logic/reasoning/data? Murray

  11. Murray Duffin
    Posted May 29, 2007 at 8:54 AM | Permalink

    Pardon me. Should be GISS not GHCN. Murray

  12. Gaudenz Mischol
    Posted May 29, 2007 at 9:01 AM | Permalink


    to fit the data to the theory of AGW

  13. steven mosher
    Posted May 29, 2007 at 9:37 AM | Permalink


    Just for grins I had a look at some tree ring data a while back just to see
    if anyone had looked at Mount Lassen ( about 70 miles from susanville)It’s last
    eruption was in 1915. I was just curious. It’s a lovely place As I’m Sure Anthony
    and Russ will attest.

    its located at 40.27N 121.30W

    And Sure enough somebody had used Lassen Mountain Hemlock. A guy named Briffa.

    So, I wondered what climate data he used. quincy station is nearby, Chico,
    Susanville, and some other less well known sites Mineral, Manizinta Lake, chester.
    I couldnt find out.

    I did find some other dendro who used Briffa Lassen Data.

    Click to access hemlock.pdf

    its a quick read and has some inteesting things to say about normalzing Hemlock
    He also notes a difficulting with finding Lassen Climate data

    For climate data, he used the Entire Sacramento Drainage Division Data!!
    I think NCDC has a map. huge area and includes the stuff you’ve been looking at. It made me laugh.

    Makes me even more curious about what Climate data Briffa Used to analyze
    the Lassen Mountain Hemlock.

    For What its worth

  14. Bob Koss
    Posted May 29, 2007 at 9:44 AM | Permalink

    Something had to be done about those pesky 1930’s.

  15. Steve Sadlov
    Posted May 29, 2007 at 9:52 AM | Permalink

    Based on the names of the supposed “zero light” California sites, my skeptic alarm was set off. A number of the names are good sized towns / small cities (examples – BRAWLEY, FORT BRAGG, INDEPENDENCE, NEEDLES, SUSANVILLE, YOSEMITE PARK HEADQUARTERS). I included Yosemite HQ since the Yosemite Valley’s east end, where HQ is located, is essentially a suburban area for all intents and purposes. Unless the sites are like 10 or 15 miles from the named town, they are not zero light. A number of the remaining names are at least small towns of a few hundred to a few thousand. Interesting that other than Death Valley, none of what I consider to be California’s most desolate areas are represented – sort of makes sense, no towns or airports in such places. Just to name a few – the roadless areas of the coastal range uplands between San Francisco and the Oregon border, the high plains north and east of Susanville, the High Sierra, various portions of the Mojave and other eastern desert areas, the Carizzo Plain, the coastal range and transverse range uplands between San Francisco and Los Angeles.

  16. JerryB
    Posted May 29, 2007 at 11:33 AM | Permalink


    Most of those adjustments were made in the USHCN, i.e. before GISS
    got the data.

    USHCN adjustments are supposed to compensate for various changes such
    as: times of observation, equipment changes, location changes, etc.

    USHCN stations are usually splices of different stations operated by
    different people at different locations. Trying to compensate for the
    changes can be iffy. At Cedarville, there were various changes that
    corresponded with the changes of the adjustments, which is not to
    say whether the adjustments were good, or not good.

    One way to attempt to gauge such adjustments might be to compare adjusted
    numbers of “nearby” stations. I placed a few comparisons of station
    pairs at in three cases, Cedarville is one
    of the pair. The fourth pair was of two stations which are quite close
    to each other, and at similar altitudes. The key numbers for a quick
    look are the rightmost numbers of the Avg lines. The temps are in
    degrees Fahrenheit, and the rightmost column is the annual difference
    including adjustments.

    In one comparison, for an 18 year period, the average differences differed by 2.25
    Avg 18 yrs: 65.45 0.00 -0.06 65.39 63.35 -0.21 0.00 63.14 2.10 2.25
    but in a later period, a 10 year average differences differed by only 1.05
    Avg 10 yrs: 61.55 0.01 0.00 61.56 61.37 -0.85 0.00 60.52 0.18 1.05
    and those two stations are rather close to each other.

    The breaks between periods are do to some change, and you will see many.
    The cryptic abbreviations are described in COMPARE.TXT, but that may
    not be a very readable document.

  17. MrPete
    Posted May 29, 2007 at 11:52 AM | Permalink

    With relatives living near Ft Bragg until recently, I know that area well. It’s a great example of microclimate sensitivity. Move a very short distance and the weather changes drastically, from foggy-cool-moist year round to sunny-warm most of the time. Ft Bragg has also seen dramatic urbanization shifts over the years, as the lumber and fishing industries ebb and flow.

    It will be interesting to hear the dynamics of the measuring station there!

  18. bender
    Posted May 29, 2007 at 2:17 PM | Permalink

    #14 Funny about those warm 1930s. Hansen et al. (2007) specifically go out of their way to point out that the the GISS GCM fails to simulate the level of “pesky” Arctic warming observed in the 1930s-40s. This *despite* the fact that they’ve already cooled it down by adjusting the numbers. Summary: They don’t know what caused that warming; but they’re certain it’s not internal chaotic variability in global/regional circulation patterns.

  19. Steve McIntyre
    Posted May 29, 2007 at 2:43 PM | Permalink

    I’ve figured out how to extract station histories from their very non-userfriendly format. The total adjustment between USHCN and GISS for this rural site since 1960 is 1.5 deg F, or an amount greater than estimated global warming since that time. There were no time-of-observation changes in that period (TOBS changing in 1957) and the station moves are supposedly 0.2 miles in 1959 and another 0.2 miles in 1969, with a total change in elevation of 2 feet. This was held to be sufficient to require an adjustment exceeding 0.8 deg C (downwards in the early temperatures.)

    This is in one of the “best” sites in the entire network.

    Taken at face value, this show the kind of migration that would be involved in order to accommodate to a change of 0.8 deg C at Cedarville – at least 0.4 miles and up to 2 feet in elevation. It’s a daunting prospect.

  20. Anthony Watts
    Posted May 29, 2007 at 3:28 PM | Permalink

    WTH? 0.8 degrees C for 2 feet of elevation change? Hell I may just drive up there tomorrow to see what could possibly require an adjustment of this magnitude.

    This is starting to look like cooked books for an embezzlement scheme.

  21. Posted May 29, 2007 at 4:12 PM | Permalink

    Urban cooling in Sweden?
    February 1st, 2006 by Lars Kamél

  22. bernie
    Posted May 29, 2007 at 4:54 PM | Permalink

    Steve #19:
    If the site just moved with no change in altitude then aren’t we looking at a proxy for possible UHI effects (UHI being a function of site characteristics and man made impacts – buildings, heat sources, asphalt, etc). If the correction is .8C then surely the UHI effect has to be of a similar order of magnitude.

  23. jae
    Posted May 29, 2007 at 4:56 PM | Permalink

    20, 21: One team makes hockeysticks, while another team puts points on the scoreboard.

  24. John F. Pittman
    Posted May 29, 2007 at 5:06 PM | Permalink


    The only thing I know would be close to that would be if it was on the adiabatic warming side and went to the adiabatic cooling side. But to do that the “hill” between the two points, to be at .2 miles apart, would have to rise out of the ground like the Eiffel Tower. Better take a helicopter and a good telephoto lens.

  25. Posted May 29, 2007 at 5:19 PM | Permalink

    Re 13

    I visited the Qunicy Station and have pictures and some station history. I was there on a Sunday and the Tech responsible for the site was off, and I have sent an e-mail with some questions. The site was automated in 1988 or 1989.

    Here is the general view

  26. Posted May 29, 2007 at 5:24 PM | Permalink

    OK, let try a link to the photo:

    General View at Quincy

  27. David Smith
    Posted May 29, 2007 at 5:59 PM | Permalink

    Re #25 Russ, I remain gobsmacked, agape, aporetic and agog at the close proximity of shrubs and trees to these stations.

    Trees and bushes create microclimates and, as they grow or die, those microclimates change. Whether its a cooling or warming depends on many factors but my guess is that a station placed, say, 10 meters from the drip line of a growing tree will on average become warmer over time.

    Nearby shrubs and trees may be OK for weather observations but they are poor neighbors for a climatological-quality site.

  28. Anthony Watts
    Posted May 29, 2007 at 6:03 PM | Permalink

    RE27 When I’m doing my Stevenson Screen tests on paint, maybe I could haul in some portable shrubbery in pots and do a second run to do a second run.

    “Nearby shrubs and trees may be OK for weather observations but they are poor neighbors for a climatological-quality site.” Well they didn’t start thinking about climatology until 1941, and by then a good portion of the network had already been established.

    Maintenance of the entire network has always been ad hoc, and left to the local observer. The observers in the CWO are not paid, so the old adage of “you get what you pay for” applies here.

  29. Steve Sadlov
    Posted May 29, 2007 at 6:06 PM | Permalink

    At least the Quincy site is not right next to suburban development (as is the case with Tahoe City).

  30. steven mosher
    Posted May 29, 2007 at 6:47 PM | Permalink

    Wait until you guys have a look at the Quincy data.

    I tried to compare USHCN data ( monthly mean, un adjusted )
    To GISS homogeneity. lots of missing months, missing years, and the
    years missing from each file were of course different.

    But for those years where you could compare, (1965 and on) GISS was warmer , in the .2C + range..larger
    past and then tapering to nothing in the present day.

    The weird thing is with all the missing data Quincy makes it on the GISS list.

    Somebody who has more time and patience can try to figure this one out.

  31. Pat Frank
    Posted May 29, 2007 at 7:04 PM | Permalink

    #28 — “RE27 When I’m doing my Stevenson Screen tests on paint, maybe I could haul in some portable shrubbery in pots and do a second run to do a second run.

    With that, we finally understand what the Knights who say Ni were about with their requests for shrubbery in Monty Python and the Holy Grail. Obviously, they were early-type climatologists from the Medieval CRU at East Anglia, setting the ground for their precision thermometry. I wonder if Phil Jones has an old suit of armor in his closet.

  32. Paul Linsay
    Posted May 29, 2007 at 7:15 PM | Permalink

    Re 25 & 26, Quincy station. Ever stand close to a telephone pole? They’re hot, the tar soaks up heat.

  33. David Smith
    Posted May 29, 2007 at 7:30 PM | Permalink

    I noticed this college student investigation of the effect of structures, including trees, on temperature. They compared near-ground temperatures of a plant 16 inches from a structure and then again 40 feet from that structure.

    The effect of proximity on temperature is rather dramatic. If the nearby structure is moving (as in growing taller and wider) then that proximity effect conceivably could appear as a trend in long-term temperature.

  34. Anthony Watts
    Posted May 29, 2007 at 9:39 PM | Permalink

    RE32 Paul, the Quincy station was at the CA Dept of Transportation lot for awhile, and next to an incinerator. yes you read that correctly. This was documented by former California State Climatologist, Jim Goodridge. Here is a photo he took of the Quincy incinerator and the small max/min thermometer shelter/hut some years ago.

    I suspect the data gaps may have more to do with “burn days” when they couldn’t comfortably get close to the thermometer. 😉

    The surface temperature record is a vortex of weirdness.

  35. DaleC
    Posted May 29, 2007 at 9:40 PM | Permalink

    re #25, 26, 29, 30,

    Here are some Quincy plots aggregated from USHCN Daily. Plotting from the daily data set allows the frequency of missing observations to be simultaneously indicated.

    TMAX Weekly, 10 year window moving average, observations per week on Y2: here
    TMAX, TMIN Annual, observations per year on Y2: here

    It seems to me that the large number of missing observations makes most of the data from 1973 to 1999 climatologically useless.

  36. Anthony Watts
    Posted May 29, 2007 at 9:48 PM | Permalink

    Oh forgot to mention, “gobsmacked” may not fully equate the feelings associated with the above picture, perhaps a new word is needed

  37. steven mosher
    Posted May 29, 2007 at 10:57 PM | Permalink

    So how does quincy make it into high quality sites? Hansen uses it but jones does not.
    Then again Gavin has said that 60 good sites are all you need.

  38. Brooks Hurd
    Posted May 29, 2007 at 11:17 PM | Permalink

    RE: 37

    Gavin’s comment about “good sites” takes on a whole new meaning; doesn’t it?

    I wonder who came up with the axiom that pre 1970 station data prior should be adjusted down, and post 1970 station data should be adjusted up?

  39. Posted May 29, 2007 at 11:26 PM | Permalink

    Another brush covered site at Blue Canyon.

  40. Posted May 29, 2007 at 11:53 PM | Permalink


    I wonder who came up with the axiom that pre 1970 station data prior should be adjusted down,

    Brohan2006 might help to answer the question:

    The distribution of known adjustments is not symmetric ‘€” adjustments are more likely to be negative than positive. The most common reason for a station needing adjustment is a site move in the 1940-60 period. The earlier site tends to have been warmer than the later one ‘€” as the move is often to an out of town airport. So the adjustments are mainly negative, because the earlier record (in the town/city) needs to be reduced [Jones et al., 1985, Jones et al., 1986].

    Refs to

    [Jones et al., 1985] Jones, P.D., Raper, S.C.B., Santer, B.D., Cherry, B.S.G., Goodess, C.M., Kelly, P.M., Wigley, T.M.L., Bradley, R.S. and Diaz, H.F. (1985) A Grid Point Surface Air Temperature Data Set for the Northern Hemisphere, U.S. Dept. of Energy, Carbon Dioxide Research Division, Technical Report TRO22, 251 pp.

    [Jones et al., 1986] Jones, P.D., Raper, S.C.B., Cherry, B.S.G., Goodess, C.M. and Wigley, T.M.L. (1986) A Grid Point Surface Air Temperature Data Set for the Southern Hemisphere, 1851-1984, U.S. Dept. of Energy, Carbon Dioxide Research Division, Technical Report TR027, 73 pp.

  41. Paul
    Posted May 30, 2007 at 3:21 AM | Permalink

    The earlier site tends to have been warmer than the later one ‘€” as the move is often to an out of town airport.

    But I thought the UHI effect was negligible..???

  42. MarkW
    Posted May 30, 2007 at 4:43 AM | Permalink

    The team does acknowledge that UHI exists. There claim is that the change in UHI is negligible, even as cities grow bigger.

  43. David Smith
    Posted May 30, 2007 at 4:59 AM | Permalink

    I think that Natchez MS US shows the effect of a station relocation in the late 1950s, when the station moved from the center of a small town out to an airport. About a 1C drop, which indeed needs to be adjusted from the record.

    But, should the city later encroach on the airport, some of the effect will return. In this case there was no return of UHI, because the town failed to grow. I’m familiar with this airport and, as best as I can recall, the station is away from vegetation, so there’s no vegetation effect either. Result – no temperature trend over the last 40+ years.

  44. gladys
    Posted May 30, 2007 at 5:11 AM | Permalink

    What a crock! “Trust us” say the ‘climate scientists’, yet they come up with all of this unubstantiated, and very likely manipulated data. Refuse to allow examination or replication of it.

    Here at the nursing home, ‘climate scientists’ now have about the same credibility as politicians, and Jimmy Swaggart and his mates.

  45. bernie
    Posted May 30, 2007 at 5:36 AM | Permalink

    UHI effects.
    If the photos and comments about individual stations mean anything it is that UHI has both a micro and macro component. Clearly any encroachment of buildings, asphalt, roadways, heat sources will have a local (+) effects (so also growth (-) and removal (+) of vegetation, irrigation (-)) while at the macro level there are the less proximate but potentially large effects of the surrounding densiity of buildings, asphalt and heat sources. The micro UHI effects are important because so many of the stations in the Arctic regions are in small settlements, where even small scale development can lead to measurable UHI effects.

    I assume there have been models built that include all these possible site effects. Can satellite readings be used as a source of “true” local temperature readings for areas around these sites? Does anyone have some good references on the estimation of all these site effects?

  46. Barclay E. MacDonald
    Posted May 30, 2007 at 2:31 PM | Permalink

    Good for you and the folks at the nursing home Gladys! Suddenly, retirement and ageing is looking much more entertaining. I must be sure to find a “home” with high speed internet and wireless access. I only hope Anthony Watts and SteveM can keep up this lively pace.

    As always, nice work gentlemen. My addiction to this blog is never satiated.

  47. Steve Sadlov
    Posted May 30, 2007 at 4:15 PM | Permalink

    RE: #39 – Consider maximum snow depth. That’ll ruin the readings, since snow actually limits how low temperature can go within its mass.

  48. Steve Sadlov
    Posted May 30, 2007 at 4:18 PM | Permalink

    RE: #43 – Should it return due to growth, it will vastly exceed what was experienced mid town during the period prior to the 50s move. If it returns, it will return with big screen TVs, ubiquitous AC systems on the buildings, track/recessed lighting, PCs, gadgets, etc. Energy flux is much higher per capita than it was 50 years ago.

  49. Phil B.
    Posted May 30, 2007 at 6:13 PM | Permalink

    Re #5 Steve M, I would certainly consider Independance, CA. a rural site, especially if the weather station is at the airport. The town is about 8 blocks by 8 blocks and covers about a half a mile on HWY 395, with a population of about 800. The airport is north of town. More important is that most of surrounding land is undeveloped Los Angeles DWP property that was acquired during the early 1900’s. Re #15, Steve S might be thinking of Bishop or Lone Pine which have recent development. Russ would probably do a better job, but I could take some photos and inquire, if urgent this weekend. If not urgent, I will be in that area in a month or two.

  50. Steve McIntyre
    Posted May 30, 2007 at 6:50 PM | Permalink

    #49. As we see more of these sites, just because a site is “rural” seems to have little to do with microsite effects and the microsite issue seems to be completely awol in Team literature. I’m sure that urban airport sites are not as screwed up as the Marysvile site. It seems that many rural sites have big microsite problems and I suspect that this is one reason why there’s not as much difference between urban and rural sites. Rural microsite screwup effects sort of match urban heat island effects. Of course there are some decent rural sites, but USHCn and the Team seem to have made no effort whatever to identify these sites and worse, they’ve made no effort to preserve sites that are decent. Lake Spaulding is rural, but the present site is a mess and the screwup occurred in the past few years, under the IPCC watch.

    THe Independence site has a different pattern than some of the sites that seem to be pretty clean, and my guess is that there are some warts on it. It’s just a guess, but I’ll be interested in how it turns out.

  51. bernie
    Posted May 30, 2007 at 7:57 PM | Permalink

    Phil, I’ve no idea where the ws actually is at the airport, but the google earth picture indicates a cluster of buildings and plenty of asphalt. Site pictures and immedite site history would be in order before any
    pronouncements on the temperature record.

  52. Posted Aug 19, 2008 at 9:18 AM | Permalink

    Interesting stuff here.

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