There are also significant positive minimum temperature biases
from urban heat islands that add a trend bias up to 0.2 C nationwide to raw readings.
When I said «There are also significant positive minimum temperature biases
from urban heat islands that add a trend bias up to 0.2 C nationwide to raw readings», I should have said «There are also significant positive minimum temperature biases
from urban heat islands, with urban stations warming up to 0.2 C faster than rural stations».
Zeke wrote «There are also significant positive minimum temperature biases
from urban heat islands that add a trend bias up to 0.2 C nationwide to raw readings.
Taken
from the Urban Heat Islands website.
Generally, the remaining uncorrected effect
from urban heat islands is now believed to be less than 0.1 C, and in some parts of the world it may be more than fully compensated for by other changes in measurement methods.4 Nevertheless, this remains an important source of uncertainty.The warming trend observed over the past century is too large to be easily dismissed as a consequence of measurement errors.
At face value, the satellite data is supported by weather balloon data, covers a much larger area of the globe than the surface - based data, and, as you pointed out, is free
from the urban heat island effect and other potential flaws of surface measurements.
I see you wrote 6 paragraphs about your supposed climate «skepticism» arising
from the urban heat island effect, but I see not a single word of explanation about why the UHI effect would turn a non-warming trend into a warming trend.
Not incidentally, City Hall's green roof absorbs storm water run - off and insulates the building from the hot sun, provides relief
from the urban heat island effect.
Secondly, as Steve Milesworthy points out, to explain Parker's null effect, you have to change
from an Urban Heat Island (UHI) effect to a Suburban Heat Island (SuHI) effect, or rather to an Urban - embedded - in - Suburban Heat Island (UeiSuHI) effect.
Not exact matches
Apart
from air pollution reduction, other benefits of
urban green infrastructure include
urban heat island mitigation, the potential reduction in energy consumption, better stormwater management, and climate change mitigation.
New research
from North Carolina State University shows that
urban «
heat islands» are slowly killing red maples in the southeastern United States.
For example, greening neighbourhoods or painting roofs lighter colours will both reduce the
urban heat -
island effect and reduce carbon - dioxide emissions through reduced air - conditioning costs, while making cities more resistant to storm damage would reduce emissions generated
from rebuilding devastated areas.»
Heat waves in cities interact synergistically with the urban heat island effect to raise temperatures more than would be expected from a simple summation calculat
Heat waves in cities interact synergistically with the
urban heat island effect to raise temperatures more than would be expected from a simple summation calculat
heat island effect to raise temperatures more than would be expected
from a simple summation calculation.
These so - called
urban heat islands result
from various factors, such as population density, surface sealing, thermal radiation of buildings, industry, and transport as well as lacking vegetation.
Urban land use creates a
heat -
island effect because asphalt, brick, and concrete absorb and conduct solar energy, while the cooling effect of evaporation
from soil and vegetation is reduced.
The field of
urban planning is gaining interest as cities around the world, including nearby Houston, are facing increased exposure to weather - related risks and hazards ranging
from sea level rise and flooding to temperature build - up and
urban heat island effect.
Some parts of the Twin Cities can spike temperatures up to 9 °F higher than surrounding communities thanks to the «
urban heat island» effect, according to a new study
from the University of Minnesota.
The more detailed understanding of
urban heat islands provided by the study can help health professionals and others target efforts to protect people and infrastructure
from heat - related problems, according to project co-leads Tracy Twine and Peter Snyder, associate professors in the College of Food, Agricultural and Natural Resource Sciences.
The phenomenon is known as the «
urban heat island» effect, and a recent N.C. State University study shows that many of North Carolina's native bee species keep away
from hot,
urban areas.
Green roofs, green streets, rainwater gardens, and bioswales can absorb storm water runoff, while also cooling city blocks suffering
from the
urban heat -
island effect during hot summers.
An international team of economists has found that large cities may shoulder a disproportionate burden
from climate change due to the amplifying effect of
urban heat islands.
This is slightly different
from the more often discussed «
Urban Heat Island» effect which is a function of the wider area (and so could be present even in a perfectly set up urban stat
Urban Heat Island» effect which is a function of the wider area (and so could be present even in a perfectly set up
urban stat
urban station).
Away
from the dense network of
heat absorbing (daytime) then heat radiating (nighttime) structures which is the Urban Heat Island and above the air with high water vapor content trapped by the valley along the river, not to mention the pall of coal dust over the city, morning low temps were much more like what the natural countryside would experie
heat absorbing (daytime) then
heat radiating (nighttime) structures which is the Urban Heat Island and above the air with high water vapor content trapped by the valley along the river, not to mention the pall of coal dust over the city, morning low temps were much more like what the natural countryside would experie
heat radiating (nighttime) structures which is the
Urban Heat Island and above the air with high water vapor content trapped by the valley along the river, not to mention the pall of coal dust over the city, morning low temps were much more like what the natural countryside would experie
Heat Island and above the air with high water vapor content trapped by the valley along the river, not to mention the pall of coal dust over the city, morning low temps were much more like what the natural countryside would experience.
The nuances: # 1) I remember when the issue of
urban heat islands there was a hue and cry
from AGW proponents that UHIs did not exist.
*
Urban Heat Island: It is well - known that the effect of heat from buildings in urban areas, as well as the thermal properties of high concentrations of concrete, raise the temperatures of Urban areas to above the surrounding
Urban Heat Island: It is well - known that the effect of heat from buildings in urban areas, as well as the thermal properties of high concentrations of concrete, raise the temperatures of Urban areas to above the surrounding a
Heat Island: It is well - known that the effect of
heat from buildings in urban areas, as well as the thermal properties of high concentrations of concrete, raise the temperatures of Urban areas to above the surrounding a
heat from buildings in
urban areas, as well as the thermal properties of high concentrations of concrete, raise the temperatures of Urban areas to above the surrounding
urban areas, as well as the thermal properties of high concentrations of concrete, raise the temperatures of
Urban areas to above the surrounding
Urban areas to above the surrounding area.
Humans have made a great number of impacts on the land stretching
from prevention of catastrophic wildfires, to
Urban Heat Islands, to denuding the land, and pollution of the air and water.
The
Urban Heat Island Effect (UHI) is a phenomenon whereby the concentration of structures and waste heat from human activity (most notably air conditioners and internal combustion engines) results in a slightly warmer envelope of air over urbanised areas when compared to surrounding rural ar
Heat Island Effect (UHI) is a phenomenon whereby the concentration of structures and waste
heat from human activity (most notably air conditioners and internal combustion engines) results in a slightly warmer envelope of air over urbanised areas when compared to surrounding rural ar
heat from human activity (most notably air conditioners and internal combustion engines) results in a slightly warmer envelope of air over urbanised areas when compared to surrounding rural areas.
In like manner, if I believe that the
urban heat island effect is responsible for AGW, why can't I just subtract the
urban temperature profile
from the global surface temperature record and «whalla», problem solved.
By taking the estimate of 0.1 degrees C per decade and multiplying by 5 to get 0.5 degrees C, or 44 %, Geoffry Smith gets a rather larger figure for his
urban heat island effect estimate than he would
from the more direct subtraction of 0.81
from 1.13 (0.32 degrees C, or 38 %).
Even the most pronounced warming, evident
from the cities of Hobart and Melbourne, is within what could be considered natural — though the trends shown here are likely to be artificially exaggerated by the method of measuring temperature since 1996 ** (electronic probes) and the
urban heat island (UHI) effect.
Aside
from the problems
urban heat islands can cause for city - dwellers, they also create an insidious problem for researchers who want to use weather station records to estimate global temperature trends.
It is why most weather stations are at airports where they became compromised by
heat from runways, jet engines, and in many cases the expanding
urban heat island (UHI).
Correcting that estimate for the millennium warming cycle, ie, the temperature recovery
from the Little Ice Age, and the
urban heat island effect gives an ECS best estimate of 1.0 °C.
Also, people will probably be more likely to want to live in the yellow areas (
from fig 4) than the blue areas, so again, maybe this signal is just an indirect measurement of land - use and
urban heat island.
«We evaluate to what extent the temperature rise in the past 100 years was a trend or a natural fluctuation and analyze 2249 worldwide monthly temperature records
from GISS (NASA) with the 100 - year period covering 1906 - 2005 and the two 50 - year periods
from 1906 to 1955 and 1956 to 2005... The data document a strong
urban heat island eff ect (UHI) and a warming with increasing station elevation... About a quarter of all the records for the 100 - year period show a fall in temperatures... that the observed temperature records are a combination of long - term correlated records with an additional trend, which is caused for instance by anthropogenic CO2, the UHI or other forcings... As a result, the probabilities that the observed temperature series are natural have values roughly between 40 % and 90 %, depending on the stations characteristics and the periods considered.»
Then the most recent explanations
from Rohde, Hausfather, and Mosher for Berkeley Earth adjustments seem to turn this issue upside down, arguing that their process for correcting the data is what results in the lowering of temperatures, not
from recent years, but
from early years when the
urban heat island and corruption of surface station sites would not have yet occurred.
Early on in my following of the global warming issue I became aware of the Surface Stations Survey, which led me to be very skeptical of the validity of the most recent temperature data trends, as I have never seen any convincing explanation as to how data
from the many
urban heat island and «corrupted» temperature monitoring sites are properly corrected.
Our UHI paper analyzing this indicates that the
urban heat island effect on our global estimate of land temperatures is indistinguishable
from zero.
Adjustments are done for many reasons: because there are gaps in the temperature recording stations, because recording stations break, because a new station differs
from the old station, because recording stations must be moved, or because the time of day they're read changes, or they shut down because of funding cuts, or the person reading it retires or dies or can't do it as often as they once did, because of
urban heat island effects, or because other stations are too close (or toop far) relative to the averge, etc.........
Urban Heat Island profile Image from Lawrence Berkeley Labs From the UNIVERSITY OF WISCONSIN - MADISON Spring comes sooner to urban heat islands, with potential consequences for wildlife Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegeta
Urban Heat Island profile Image from Lawrence Berkeley Labs From the UNIVERSITY OF WISCONSIN - MADISON Spring comes sooner to urban heat islands, with potential consequences for wildlife Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegetat
Heat Island profile Image from Lawrence Berkeley Labs From the UNIVERSITY OF WISCONSIN - MADISON Spring comes sooner to urban heat islands, with potential consequences for wildlife Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of veget
Island profile Image
from Lawrence Berkeley Labs From the UNIVERSITY OF WISCONSIN - MADISON Spring comes sooner to urban heat islands, with potential consequences for wildlife Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegetat
from Lawrence Berkeley Labs
From the UNIVERSITY OF WISCONSIN - MADISON Spring comes sooner to urban heat islands, with potential consequences for wildlife Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegetat
From the UNIVERSITY OF WISCONSIN - MADISON Spring comes sooner to
urban heat islands, with potential consequences for wildlife Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegeta
urban heat islands, with potential consequences for wildlife Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegetat
heat islands, with potential consequences for wildlife
Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegeta
Urban - dwelling plants around the globe typically get a head start on the growing season compared to their rural counterparts because of the
urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegeta
urban heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegetat
heat island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of veget
island effect, the phenomenon in which cities tend to be warmer than nonurban areas due to their plethora of built surfaces — made of concrete, asphalt and more — and scarcity of vegetation.
Nobody would intentionally adjust the data in the opposite direction
from what would be expected for an increasing
urban heat island effect.
Here we start with endlessly faulty data —
from instruments parked on
urban «
heat islands» to severely massaged data bases of daily temperature readings,
from sketchy numbers for the vast reaches of the planet where there are almost no readings, to expurgation of decades of inconvenient data.
Researchers
from Princeton University report in the journal Environmental Research Letters that they considered how future
heat waves will play into the
urban heat island effect in 50 US cities.
They would deny any role
from solar activity,
urban heat island effects, land use changes i.e. wooded areas cleared for agriculture, aerosols, or natural variability.
In my opinion, Gavin's own statement that «
urban heat island effects are corrected for in the surface records» is, to borrow a phrase
from realclimate, «disinformation».
A paper by Ross McKitrick, an economics professor at the University of Guelph, and Patrick Michaels, an environmental studies professor at the University of Virginia, concludes that half of the global warming trend
from 1980 to 2002 is caused by
Urban Heat Island.
Other groups like NASA Goddard Institute for Space Studies (GISS) and the Climate Research Unit at the University of East Anglia (CRU) take data
from NCDC and other sources and perform additional adjustments, like GISS's nightlight - based
urban heat island corrections.
When the readings
from all rural and
urban stations are taken together and adjusted for the
urban heat island effect, it's clear global average temperatures are increasing.
Here we assess the diurnal and seasonal variation of surface
urban heat island intensity (SUHII) defined as the surface temperature difference between
urban area and suburban area measured
from the MODIS.
The stations used are predominantly
urban and affected by the
urban heat island effect (UHIE), this means the temperatures
from the two regions are higher in summer and winter.