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PCE Deutschland anemometer PCE-EM 890
SKU: T-909989
293,80 € (vč. 19% daň, Bez dopravy)
246,89 € (bez DPH, Bez dopravy)
380,69 € Výrobcem doporučená malobchodní cena.
Skladem,připraveno k odeslání do 48h
Obsah:
1 Kus
Doprava:
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Údaje o výrobku
Výrobce:
PCE Deutschland GmbH
Stav:
Nový
SKU:
T-909989
SKU výrobce:
PCE-EM 890
GTIN kód (EAN):
4250348719478
Hmotnost:
0,04 Kg
Všechny informace týkající se produktů od PCE Deutschland GmbH. Technické a optické úpravy výrobce a chyby vyhrazeny.
This page has been machine-translated, the original german version can be found here, please also note the Zřeknutí se odpovědnosti za překlad.
Popis výrobku
The climate-weather meter PCE-EM 890 is an instrument for measuring environmental conditions. The climate-weather meter allows you to make accurate measurements in the shortest possible time. Due to its small size and light weight, this climate-weather meter is an easy-to-use information system about the weather condition. You can switch between the measurement functions with just one push of a button. Thus, this climate-weather meter is ideal for technicians, sailors, farmers and many other people who depend on the weather or whose activities are significantly affected by the weather.
With just one meter, you can easily determine wind speed, temperature, wind chill (perceived temperature), dew point, relative humidity, heat index, barometric pressure, and altitude pressure against N.N. The climate weather meter provides you with the functions of single reading, minimum value, maximum value measurement.
Explanation of different environmental conditions:
Wind Chill The wind chill describes the difference between the measured air temperature and the felt temperature depending on the wind speed. Some of our anemometers can measure the Wind Chill and other parameters.
Air Pressure
The air pressure at any location in the earth’s atmosphere is the hydrostatic pressure of the air prevailing at that location. This pressure coincides with the weight force of the column of air standing on the Earth’s surface or a body located on it. The average atmospheric pressure at sea level is 101325 Pa = 1,013.25 hPa = 101.325 kPa, which is part of the normal conditions. Dew point / dew point temperature Air can absorb more water vapor with increasing temperature. When the temperature of a building material or the air at which the relative humidity of 100% is reached drops, the excess water vapor then precipitates in the form of condensation. The boundary area is called the dew point. Buildings should be constructed in such a way that the temperature on the inside of the airtight layer does not fall below the dew point. This prevents the formation of condensation water and the resulting structural damage or mold growth. Air currents through the airtightness layer are particularly damaging. In this case, the temperature must always be expected to fall below the dew point. The wet bulb temperature, which plays an important role in air conditioning technology, for example, is also a very important parameter in many other areas.
With just one meter, you can easily determine wind speed, temperature, wind chill (perceived temperature), dew point, relative humidity, heat index, barometric pressure, and altitude pressure against N.N. The climate weather meter provides you with the functions of single reading, minimum value, maximum value measurement.
Explanation of different environmental conditions:
Wind Chill The wind chill describes the difference between the measured air temperature and the felt temperature depending on the wind speed. Some of our anemometers can measure the Wind Chill and other parameters.
Air Pressure
The air pressure at any location in the earth’s atmosphere is the hydrostatic pressure of the air prevailing at that location. This pressure coincides with the weight force of the column of air standing on the Earth’s surface or a body located on it. The average atmospheric pressure at sea level is 101325 Pa = 1,013.25 hPa = 101.325 kPa, which is part of the normal conditions. Dew point / dew point temperature Air can absorb more water vapor with increasing temperature. When the temperature of a building material or the air at which the relative humidity of 100% is reached drops, the excess water vapor then precipitates in the form of condensation. The boundary area is called the dew point. Buildings should be constructed in such a way that the temperature on the inside of the airtight layer does not fall below the dew point. This prevents the formation of condensation water and the resulting structural damage or mold growth. Air currents through the airtightness layer are particularly damaging. In this case, the temperature must always be expected to fall below the dew point. The wet bulb temperature, which plays an important role in air conditioning technology, for example, is also a very important parameter in many other areas.
Související výsledky
Kompletní katalóg
Nabídka je zaměřena výhradně na firemní zákazníky, společnosti, veřejné instituce a živnostníky. Všechny ceny v katalozích jsou bez DPH, poštovného a příplatků, pokud li existují.
Výrobce je výhradně zodpovědný za obsah, cenu a detaily produktů a nabídek uvedených v katalozích. Technické a optické změny výrobce a chyby jsou vyhrazeny.
Výrobce je výhradně zodpovědný za obsah, cenu a detaily produktů a nabídek uvedených v katalozích. Technické a optické změny výrobce a chyby jsou vyhrazeny.
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PCE Deutschland anemometer PCE-EM 890
The climate-weather meter PCE-EM 890 is an instrument for measuring environmental conditions. The climate-weather meter allows you to make accurate measurements in the shortest possible time. Due to its small size and light weight, this climate-weather meter is an easy-to-use information system about the weather condition. You can switch between the measurement functions with just one push of a button. Thus, this climate-weather meter is ideal for technicians, sailors, farmers and many other people who depend on the weather or whose activities are significantly affected by the weather.
With just one meter, you can easily determine wind speed, temperature, wind chill (perceived temperature), dew point, relative humidity, heat index, barometric pressure, and altitude pressure against N.N. The climate weather meter provides you with the functions of single reading, minimum value, maximum value measurement.
Explanation of different environmental conditions:
Wind Chill The wind chill describes the difference between the measured air temperature and the felt temperature depending on the wind speed. Some of our anemometers can measure the Wind Chill and other parameters.
Air Pressure
The air pressure at any location in the earth’s atmosphere is the hydrostatic pressure of the air prevailing at that location. This pressure coincides with the weight force of the column of air standing on the Earth’s surface or a body located on it. The average atmospheric pressure at sea level is 101325 Pa = 1,013.25 hPa = 101.325 kPa, which is part of the normal conditions. Dew point / dew point temperature Air can absorb more water vapor with increasing temperature. When the temperature of a building material or the air at which the relative humidity of 100% is reached drops, the excess water vapor then precipitates in the form of condensation. The boundary area is called the dew point. Buildings should be constructed in such a way that the temperature on the inside of the airtight layer does not fall below the dew point. This prevents the formation of condensation water and the resulting structural damage or mold growth. Air currents through the airtightness layer are particularly damaging. In this case, the temperature must always be expected to fall below the dew point. The wet bulb temperature, which plays an important role in air conditioning technology, for example, is also a very important parameter in many other areas. 4250348719478-4147 4250348719478 https://www.toolteam.com/cs-CZ/pce-deutschland-anemometer-pce-em-890-t-909989-4250348719478?dc=CZ&cu=EUR 2024-11-20 293.8 DE 14
With just one meter, you can easily determine wind speed, temperature, wind chill (perceived temperature), dew point, relative humidity, heat index, barometric pressure, and altitude pressure against N.N. The climate weather meter provides you with the functions of single reading, minimum value, maximum value measurement.
Explanation of different environmental conditions:
Wind Chill The wind chill describes the difference between the measured air temperature and the felt temperature depending on the wind speed. Some of our anemometers can measure the Wind Chill and other parameters.
Air Pressure
The air pressure at any location in the earth’s atmosphere is the hydrostatic pressure of the air prevailing at that location. This pressure coincides with the weight force of the column of air standing on the Earth’s surface or a body located on it. The average atmospheric pressure at sea level is 101325 Pa = 1,013.25 hPa = 101.325 kPa, which is part of the normal conditions. Dew point / dew point temperature Air can absorb more water vapor with increasing temperature. When the temperature of a building material or the air at which the relative humidity of 100% is reached drops, the excess water vapor then precipitates in the form of condensation. The boundary area is called the dew point. Buildings should be constructed in such a way that the temperature on the inside of the airtight layer does not fall below the dew point. This prevents the formation of condensation water and the resulting structural damage or mold growth. Air currents through the airtightness layer are particularly damaging. In this case, the temperature must always be expected to fall below the dew point. The wet bulb temperature, which plays an important role in air conditioning technology, for example, is also a very important parameter in many other areas. 4250348719478-4147 4250348719478 https://www.toolteam.com/cs-CZ/pce-deutschland-anemometer-pce-em-890-t-909989-4250348719478?dc=CZ&cu=EUR 2024-11-20 293.8 DE 14