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Berkeley Earth Surface Temperature Study: “The effect of urban heating on the global trends is nearly negligible”
Posted on 21 October 2011 by Andy Skuce
A paper submitted for peer review by the Berkeley Earth Surface Temperature study (BEST) finds that urban heating has an influence on global temperature trends that is “nearly negligible” and that what effect has been observed is even slightly negative, which is to say that temperature trends in urban areas are actually cooler than the trends measured at rural sites, and that the Earth's land surface has warmed approximately 1°C on average since 1950.
The Urban Heat Island Effect
It has long been observed that temperatures in cities are higher than in the surrounding countryside, caused, in part, by human structures that reduce albedo and evapo-transpiration, as well as by the effects of waste heat emissions, McCarthy et al 2010. Even though most (99%) of the Earth’s surface is not urbanized, some 27% of the Monthly Global Historical Climatology Network (GHCN-M) temperature stations are located in cities having populations of more than 50,000. Since urbanization has grown dramatically over the past few centuries, it seems reasonable to ask how much of the observed rise in global temperatures is due to urbanization. For example, McKitrick and Michaels claimed in 2007 that about half of the recent warming over land is due to urban heat island effect, although this result was disputed by Schmidt in 2009.
Several studies have looked in depth at possible heat island contamination of land temperature records. For example, Hansen et al in 2010 used satellite measurements of night lights to remove possibly affected urban sites from the temperature records. Allowing for urban effects reduced the global temperature trend over the period 1900-2009 by 0.01°C. Menne et al performed an analysis on US surface temperature records and found only very small effects due to poor siting of temperature stations. They reported that poorly-sited stations did show some small positive bias in recorded minimum temperatures but there was a small, but slightly larger, negative bias in recorded maximum temperatures, resulting in an overall small residual cool bias.
The BEST project
"Our aim is to resolve current criticism of the former temperature analyses, and to prepare an open record that will allow rapid response to further criticism or suggestions."
The BEST project has the goal of merging all of the world’s temperature data sets into a common data set and of using new algorithms to analyze and filter the data. The BEST archive has 39,300 stations, some five times the 7,280 stations incorporated in the GHCN-M data set.
Early results of the study were released in March 2011:
"A preliminary analysis of 2% of the Berkeley Earth dataset shows a global temperature trend that goes up and down with global cycles, and does so broadly in sync with the temperature records from other groups such as NOAA, NASA, and Hadley CRU. However, the preliminary analysis includes only a very small subset (2%) of randomly chosen data, and does not include any method for correcting for biases such as the urban heat island effect, the time of observation, or other potentially influential biases."
The BEST study has been fiercely criticized for accepting funding from the Koch Foundation, for the allegedly biased views of the project’s founder Richard Muller and the choice of the controversial Judith Curry as the sole climatologist on the scientific team.
The 2011 BEST urban heating paper
The BEST paper reported on here focuses on urban effects on the temperature record . It was authored by Charlotte Wickham, Judith Curry, Don Groom, Robert Jacobsen, Richard Muller, Saul Perlmutter, Robert Rohde, Arthur Rosenfeld, and Jonathan Wurtele and is titled Influence of Urban Heating on the Global Temperature Land Average Using Rural Sites Identified from MODIS Classifications.
The temperature stations were sorted into two sets: a complete set and a set comprising only stations located far from urban areas. The authors used a satellite-imagery derived map made by the MODIS project that can distinguish between urbanized areas and rural and undeveloped areas. In order to allow for the imprecise coordinates of some of the temperature stations compared to the fine resolution of the MODIS map, the BEST authors defined the stations as either “very-rural” or not. Very-rural sites are located at least one tenth of a degree of latitude or longitude (about 11 km) away from the urban areas defined on the MODIS map.
The BEST study performed two analyses. The first looked at simple trend analysis on their raw temperature data, with the seasonal effects removed.
Figure 1: Temperature trends for all 39,028 temperature stations (left) and for the 16,132 “very-rural” sites (right). About one third of the stations showed cooling and the rest warming over their periods of record length.
The histograms all show similar average warming trends and the stations with the longest measurement durations show the least dispersion of temperature trends. The median trends for all the sites range from 0.98°C per century for sites with more than two months of observations and to 0.97°C per century for stations with record lengths greater than 30 years. The rural stations medians are 1.08 and 1.09°C per century respectively. The rural stations therefore show more median warming, about one tenth of a degree Celsius per century, than the complete data set. This result is counter-intuitive and is at odds with previous studies that showed a small but positive urban effect in the range of 0.01 to 0.1°C per century. The BEST team offers no convincing explanation of why this should be so.
One third of the records lie to the left of the zero warming line. Figure 2 illustrates how the warming and cooling sites are distributed over part of North America.
Figure 2: Locations of temperature stations with more than 70 years of data. Red dots show a warming trend and blue dots cooling. The map illustrates the importance of having multiple records to detect climate trends.
BEST’s first approach does not account for unevenness in station distribution, nor is consideration given to the different time periods over which the data were acquired. In their second approach, the BEST team performed a global land temperature reconstruction with their own methodology, using all the data and the very-rural sites only. The details of the methodology used are described in a draft paper by Robert Rohde and others.
The results (Figure 3) show very little difference in the post-1950 period between the very rural stations and the rest. In fact, in the most recent few decades, the rural sites have become slightly warmer than the full data set, and show a trend of -0.19 +/- 0.19°C per century over the 1950-2010 time period, roughly consistent with the trends reported in the first method. The observed warming since 1950 is 1.9 +/- 0.1°C per century, ten times larger than, and of opposite sign to, the urban-rural effects.
Figure 3: The Berkeley Earth global temperature averages, normalized to zero mean for the period 1950 to 1980.
Significance
The main result of this study, that the influence of urban areas on the global land temperature data set is very small, corroborates the consensus view among climate scientists, including, for example, the recent paper by Souleymane Fall and others. To the extent that the BEST work resolves "current criticism of the former temperature analyses" it succeeds, even if the results come as no surprise. Nevertheless, initial reactions from certain quarters indicate, also unsurprisingly, that they are unhappy with the outcome of this and other recently released BEST studies. For example, Roger Pielke Sr comments that: "The nearly identical trends is no surprise as they draw from mostly the same raw data!" The BEST studies however, as mentioned earlier, have used all available temperature data, 39,300 stations, some five times the 7,280 stations used in the GHCN-M data set. The results of the BEST study are indeed unsurprising because the previous data sets sampled all the data adequately.
Other objections have been raised that the BEST studies were released prior to peer-review. That is indeed true and it will be interesting to see if the methodology and conclusions in these draft papers are significantly modified during the review process.
It's worth emphasizing that the study looked at the effects of urbanization on the global land temperature trend. Once ocean temperatures are considered the small urban influence on temperatures will be further diluted.
The take-away points from this study are:
- once again, the accuracy of the land surface temperature record is confirmed;
- the BEST study used more data than previous studies but came to essentially the same result;
- the influence of the urban stations on the global record is very small and, if present at all, is biased on the cool side.
[DB] When posting graphics it is considered good form to also link to the paternity of the graphic. Please provide such for your above graphics. Else I will delete this comment as this is going too far off-topic.
[DB] "No agenda here, just would be good to correct any misleading graphics."
When you say "misleading graphics" do you refer to that of the IPCC...or yours? FYI, "misleading" is a favorite toy of the fake-skeptic contingent, being used liberally like milk with cereal. As such, it is a term that can contravene the Comments Policy here, depending upon the context used.
Lassesson at 18:25 PM on 21 October, 2011
What happened around 1865-1870 in figure 3 and where did the huge peak around 1880 come from?
I don't see the answer posted. The answer to your inquiry is almost certainly the very large, perhaps largest in recent history, El Nino Event, 1876-78.
https://www.insidescience.org/news/historys-greatest-el-ni%C3%B1o-may-have-caused-severe-19th-century-famine
YTeddy @45,
You are correct in that there are no satisfactory answers posted for Lassesson @2.
I'm not sure what is being asking regarding 1865-70 but the "huge peak arond 1880" was the 1877-78 El Niño which appears in the extended MEI record, its impact on the global temperature records (both BEST & HadCRUT cover back to 1850) being excentuated by the preceding and succeeding La Niñas.
The article you link-to is describing the work presented at the 2017 AGU Fall Meeting ' El-Niño Grande and the Great Famine (1876-78) '. Looking at the citations the paper gained here, I don't see any response to the paper from climatologists although it does receive attention for its analytical method.