Rev those Engines and Grab your Kestrel 4250.

Friday, March 18th, 2011
Racing Season is here! Be sure you have the right weather station at the track.
As a racer, you understand the impact that environmental conditions can have on your car. By knowing exactly what weather parameters you’re up against, you can fine tune that engine for performance optimization.

Our density altitude measurement is the standard measurement which takes into consideration pressure, temperature AND humidity to determine the density of the air in comparison to a standard atmosphere.

The Altronics measures a “moistureless density altitude”. This is measuring density altitude accounting for temperature and pressure yet without humidity. Humidity has a small but measurable effect on DA.

Our pocket-sized weather instrument includes humidity precision and accuracy. The Kestrel 4250 Racing Weather Tracker costs one-tenth the price of a trailer/pager system, but provides comparable and instant results. It’s the weather instrument chosen by wildland firefighters and military Special Forces, and they have much more than first place riding on its accuracy. Plus, carry it with you for accurate weather information away from the track. Painting, spraying, hiking, construction, fishing, hunting, and agriculture – the list of uses for this powerful pocket-sized tool goes on and on!

Jeremy Waibel counts on the Kestrel 4250 for a winning bracket racing season.

PREVENT HEAT RELATED INJURY WITH A HAND-HELD WEATHER METER

Wednesday, August 4th, 2010

BOOTHWYN, PA …As summer temperatures rise, so does the risk of heat-related illness and fatality. For outdoor activities, it’s critical to monitoring the environmental conditions to prevent heat stress. Whether you’re outside for sport or for your job, Kestrel Pocket Weather Meters provide instant, accurate information to monitor conditions when safety is at stake.

Athletic trainers, hikers, bikers, and anyone engaging in exercise outdoors can prevent heat injury by monitoring heat stress index for potentially unsafe levels. Heat Stress Index is used to measure the effects of the environment on the human body. The Heat Stress Index is a calculation based on air temperature and humidity, as well as a number of assumptions, to estimate what the current conditions feel like on the human body.

Wildland firefighters must perform in extreme summer temperatures. Knowing the relative humidity right at the scene of the fire allows them to make decisions for safety and firefighting strategy.  Instantly, firefighters can get temperature, humidity, wind speed, heat index, and more. In addition to getting critical information for containing the fire, heat index provides vital data in keeping emergency personnel safe. Dave Hostler, PhD, a Research Associate Professor of Emergency Medicine at the Emergency Responder Human Performance Lab at University of Pittsburgh says, “Once we have the Heat Index in hand, we can determine the intensity of our fireground rehab practices.”

When firefighters have their heavy gear on, things can get dangerously hot quickly. “We have taken a conservative approach and decided that any temperature above 80 on the heat index requires active cooling or an air-conditioned vehicle/structure for firefighter and hazmat technician rehab,” said Hostler. “Above this temperature there is always some potential for heat injury.”

Even for those of us who won’t be spending the summer in fighting fires, its important to keep an eye on the heat index and always ensure everyone is hydrated during outdoor activities. “Prevention is always better than treatment,” says Hostler. “Even using the best practices, heat stress can take hours to correct once it occurs.  Drink plenty of fluids, rest often, and think about heat stress before it occurs.”

Every Kestrel Pocket Weather Meter is backed by a five year warranty and is designed, developed, built, tested and supported here in the USA. Nielsen-Kellerman’s Kestrel Weather division has been researching, developing and manufacturing technically advanced portable weather instruments for more than twelve years and owns multiple patents on their unique features. Kestrel Pocket Weather Meters are employed by thousands of users in hundreds of different activities around the world.

- Know Your Conditions -

For more information, contact Monica Devlin at 610.447.1555 X 306

mdevlin@nkhome.com
or visit www.nkhome.com.

Observations from a Heat Wave

Thursday, July 22nd, 2010

As the Philadelphia region is in the middle of its fifth heatwave of the year, we thought it would be a great time to track the conditions and compare two hot days worth of data. We used a Kestrel 4500 with Bluetooth on the tripod and vane mount, with the built-in data logger recording every minute. We left our setup outside during the hottest part of the day- from around noon till 4pm.

When doing these observations, we put the Kestrel setup on an island of grass out in our small parking lot. Now, most meteorologists and weather buffs may scoff at even the idea of taking weather observations that don’t meed the World Meteorological Organization’s standards (eg. temperature measured at 2 meters, wind at 10 meters, away from buildings, etc.), but we wanted to make observations of what the weather really feels like. Not the weather taken at the airport next to the tarmac, but the weather you feel when you go outside. Makes sense, right? This is why the Kestrel meters offer a more true environmental snapshot of exactly where you are- it measures the conditions right where you are- not miles away at the airport or another weather station hub.

A quick note about the thermistor (temperature sensor): at all angles, the thermistor stayed in the shade of the Kestrel unit. So while we did not measure the temperature within a Stevenson screen or within a fan-aspirated radiation shield, the temperature is accurate to what you would feel while outside, at that exact minute. This is why the temperature has so much variation on the charts below.

When first investigated the data, the first thing we looked at was what the difference between the two days was. We knew the first day was warmer, but that hardly tells the whole story.

Temperature for July 6 and 7

Recorded temperature during the afternoon on July 6 and 7, 2010 in Boothwyn, PA (just outside of Philadelphia).

In the graph, the darker line is the 6th and the brighter line is the 7th. At first glance, it looks like the temperature can really vary during the day. And in reality, it does. Most of the rises and dips in temperature can be explained by some passing clouds and winds (explained later). Even though the thermistor was not directly in the sun, when the sun went behind the clouds temperatures drifted down until the sun came back out. The high temperature recorded on the 6th was 105.5 F, while the high temperature recorded on the 7th was 104.5 F. Compare this to the local airport high’s of 102 and 103, respectively.

Now about that wind. I figured the wind had an influence on the temperature because to our west is a small woods area, and to the east is a large asphalt parking lot. I figured the temperature would become cooler with an easterly wind and warmer with a westerly wind. To investigate this, I took a day (the 7th) and plotted the temperature and wind direction on separate axes. The result is below, with wind direction in green and temperature in red.

Temperature vs. Wind Direction

Temperature vs. Wind Direction for a small period of time on the 7th.

Temperature vs. Wind Speed on July 7.

I noticed that there was a slight correlation between the direction and temperature, but it was not consistent. Also, I only took a small sample of the data where this effect looked better- in some segments of the data it was hardly noticeable. However, for times when the data did seem to align it was almost always the same. Temperatures rose with an Easterly wind, and temperatures decreased with a Westerly wind. After seeing this, I decided to compare the Temperature and Wind Speed during this same time period (below).

Now, the wind speed correlation seemed much more defined. As winds increased, the temperature reading dropped from the mixing going on in the air.

Looking closer at the data, I calculated the correlation factor for both variables with respect to temperature. (For those unfamiliar with correlation factors, -1 means a complete negative correlation, 1 means a complete positive correlation and 0 means no correlation at all.) Comparing the temperature to wind direction for the period graphed, the correlation factor was a measly -0.03. The wind speed had a much better correlation with temperature with a correlation factor of -0.69. For the entire day, temperature and wind had a correlation of -0.46 on the 6th and -0.50 on the 7th. Not an exact match, but a pretty strong observation that I wouldn’t be surprised to see during the summer.

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