The authors of the study seek to make other researchers more aware of human bias when using Storm Data, one of the largest publicly available storm databases. The study, published in a recent issue of Journal of Applied Meteorology and Climatology, uses a large-scale statistical analysis of information from the database to investigate how much storm reporters’ estimates of wind speeds differ from measurements.
Potential for Bias?
Storm Data is an enormous set of measurements characterizing more than 50 years’ worth of geophysical events, from tidal waves to tornadoes, compiled by the National Centers for Environmental Information (NCEI) in Silver Spring, Md. People from blizzard climatologists to insurance company adjustors make use of the data—and, thanks to a thorough collection and vetting process, the storm reports the database generates are generally considered reliable.
However, because Storm Data aims to collect as many data as possible, not all of the information comes from weather stations with calibrated instruments. Many of the entries in the database come from trained—or even untrained—storm reporters. These reporters must rely on environmental cues to make estimates of wind speeds and other measurements.
“When you’re estimating it, there has to be some sort of basis for that estimate…whether a tree limb snapped, or whether there was siding ripped off a house,’” said Brenton MacAloney, the Storm Data program manager at NCEI. “There has to be something other than, ‘uh, I thought it was something around 50 knots.’” The database asks its reporters to make narrative accounts of the events, to check that their numbers are within the realms of probability.Still, many researchers have long doubted the accuracy of Storm Data’s human reporters. “Everyone had assumed that [Storm Data was unreliable], but nobody had actually shown it,” said Peter Miller, the lead author on the study and a meteorologist at the University of Georgia in Athens, Ga.
Testing Storm Reporters’ Accuracy
To test the accuracy of human-generated wind gust reports, the researchers compared Storm Data wind speed entries from storm reporters who didn’t use anemometers with wind data from automated weather stations. In the study, which appeared online on 19 April, the authors also used instrumental data from the Global Historical Climatology Network as a comparison for the human-reported gusts.
The researchers focused on windstorms without rain, lightning, or other phenomena that could frighten observers, accidentally inflating their estimates of the storm’s intensity. They also eliminated news media reports from consideration as human observer data, because news reporters might have relied upon instrumental data from local weather stations.
Even with those potential biases removed, the comparisons revealed that storm reporters overestimated the speeds of wind gusts—on average, by about one third of the gusts’ actual speeds.
These inflated estimates could have introduced inaccuracies into any study that relied on Storm Data for climatological or storm modeling information, Miller said.
Overestimation: Consequences and Cures
Inflated estimates can have real consequences for society. If people hear that winds are stronger than they actually are, they may alter their behavior—for example, evacuating their homes unnecessarily during a hurricane.
That leads to another sort of trouble. “People who choose to evacuate eat up resources for people who truly need to evacuate,” said Gregory Webster, a psychologist at the University of Florida in Gainesville, who was not involved with the study. “It causes extra traffic congestion, and can sometimes result in even more severe food hoarding,” when frightened residents buy out all the water and nonperishable food they can find, leaving less for those who might truly need it.
Fixing the problem may prove difficult, said Miller. Many different factors contribute to overestimations—for instance, outdated storm reporter training, he noted.Storm reporters learn, in training, to use the Beaufort Wind Force Scale, which relies on environmental cues to determine how fast the wind is blowing. According to Miller, the Beaufort Scale is flawed. As an example, the scale indicates that trees blow over at wind speeds of 58 miles per hour and above. However, Miller said his research shows that trees can fall over at much lower speeds, in the low 40-mph range.
“Wind speeds are hard to estimate, especially when you’re talking about trees,” said Storm Data’s MacAloney. “We’re meteorologists, not arborists.”
The value of Storm Data lies in its scope, which includes remote areas without on-the-ground weather stations, MacAloney maintained. Despite their potential biases, human reports from such locations provide vital information such as narratives about highly localized events—for example, tornadoes and hail—that weather stations miss.
The authors of the new study agree, saying that Storm Data remains a valuable resource but needs a better system for flagging wind reports generated from people’s observations alone.
Citation: Deatrick, E. (2016), Humans misread wind speeds, skewing a major hazards database, Eos, 97,doi:10.1029/2016EO053709. Published on 06 June 2016.
I’ve often wondered if volunteer weather observers might potentially and purposely skew high and low temperature records. For example, let’s say you are within a degree of breaking a 100 year old temperature record at your NOAA COOP station. Only you know the real high or low reading on that thermometer, and after you reset it, all evidence of it is erased, forever. You can write down the number you want in the B91 form, or phone it in using the weathercoder, and nobody can prove you wrong, unless of course your exaggeration is quite large and doesn’t fit into a regional pattern, inviting scrutiny.
Meanwhile, you get some notice in the press for “breaking a record”, which is some recognition for a mostly thankless volunteer job done 24/7/365.
Exaggeration in temperature records seems quite plausible to me, because the human element can easily be skewed, whether it is wind or temperature.
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Just change kilometers per hour into miles per hour and it’s job done.
Several years ago, during a hurricane, the BBC and most of the UK media changed a wind speed of 270 kilometers per hour into 270 miles per hour.
I really hate wind speed measurements in New Hampshire. We have 2 meter (height) wind speeds, 10 meter height speeds, heights chosen because they were convenient, trees that massive impact 2 and 10 meter speeds due to their foliage, trees that do the same even after shedding their leaves in the fall, and most of the NWS readings are from airports where the nearest tree is hundreds of meters away. Something about trees and turbulence not playing nicely with airplanes.
Besides, I see the reports and forecasts for 30 mph winds – and I get sustained winds of about 5 mph. In the winter.
http://wermenh.com/wx/wind.png
Oh – today’s forecast: Partly sunny, with a high near 66. Northwest wind around 15 mph, with gusts as high as 30 mph.
200 years ago today we were between killing freezes both nights adjacent to today, an event we still marvel at. 🙂
The descriptions of Effects at Sea are much easier to differentiate than those on land, especially once you get 20 or 30 miles or more away from land. The Beaufort Scale works wonderfully when wind blows over water, it’s all the same as opposed to trees and such. Still not a perfect way to report the wind speed though.
Force Wind(Knots) WMO Classification Appearance of Wind Effects On the Water
0 Less than 1 Calm Sea surface smooth and mirror-like
1 1-3 Light Air Scaly ripples, no foam crests
2 4-6 Light Breeze Small wavelets, crests glassy, no breaking
3 7-10 Gentle Breeze Large wavelets, crests begin to break, scattered whitecaps
4 11-16 Moderate Breeze Small waves 1-4 ft. becoming longer, numerous whitecaps
5 17-21 Fresh Breeze Moderate waves 4-8 ft taking longer form, many whitecaps,
some spray
6 22-27 Strong Breeze Larger waves 8-13 ft, whitecaps common, more spray
7 28-33 Near Gale Sea heaps up, waves 13-19 ft, white foam streaks off breakers
8 34-40 Gale Moderately high (18-25 ft) waves of greater length, edges of
crests begin to break into spindrift, foam blown in streaks
9 41-47 Strong Gale High waves (23-32 ft), sea begins to roll, dense streaks of foam,
spray may reduce visibility
10 48-55 Storm Very high waves (29-41 ft) with overhanging crests, sea white
with densely blown foam, heavy rolling, lowered visibility
11 56-63 Violent Storm Exceptionally high (37-52 ft) waves, foam patches cover sea,
visibility more reduced
12 64+ Hurricane Air filled with foam, waves over 45 ft, sea completely white with
driving spray, visibility greatly reduced
Back in the days of the old Soviet Union. Fuel subsidies were based on how cold the previous winter was.
The colder the winter, the more money your region got.
Unsurprisingly, when the Soviet Union ended and these subsidies stopped, the temperature being measured at these stations suddenly rose by several degrees.
Here in Texas on the High Plains if our weather reporters named every storm that had a gale force wind, we would run out of names.
“According to Miller, the Beaufort Scale is flawed. As an example, the scale indicates that trees blow over at wind speeds of 58 miles per hour and above. However, Miller said his research shows that trees can fall over at much lower speeds, in the low 40-mph range.” If that were true, there wouldn’t be a tree standing in Wyoming. (It does say “can” fall over so he has wiggle room.)
People do over-estimate wind speed, especially if they are not used to high winds. I have a wind gauge and I can’t consistently judge wind speeds, even with practice. Plus, where the gauge is sighted matters. I moved mine further out in the open and the speeds went up 5 mph or more.
Very plausible. The exaggeration may also be no more than innocent human error. Understandable.
For me, Mr. Layman, the takeaway is that the further back the records go, the more scratched they are.
Modern computer adjustments to past records only add more scratches.
There’s no way in H a computer model can know what happened then.
Where does that leave us?
Admit we don’t know (and act accordingly) or get Professor Trelawny’s nephew to read our tree rings.