2015
DOI: 10.1007/978-3-662-43578-6
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Meteorologie

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Cited by 6 publications
(3 citation statements)
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“…Based on the height difference between 30 min of flight we calculated climb rates, and the sum of all height gains across a flight bout (only positive climbs rates). Short-term changes in air pressure within 3-h are reported to be 1–2 hPa ([ 47 ] p. 117). Therefore, we expected errors in climb rate estimates due to changes in weather conditions to be insignificant.…”
Section: Methodsmentioning
confidence: 99%
“…Based on the height difference between 30 min of flight we calculated climb rates, and the sum of all height gains across a flight bout (only positive climbs rates). Short-term changes in air pressure within 3-h are reported to be 1–2 hPa ([ 47 ] p. 117). Therefore, we expected errors in climb rate estimates due to changes in weather conditions to be insignificant.…”
Section: Methodsmentioning
confidence: 99%
“…The water vapor pressure over the IL solutions ( p H 2 O ) was calculated from the measured relative humidity (% rH), the temperature ( T ) and the saturated vapor pressure of water ( e w ) using the Magnus equation.see ref e normalw ( T ) = 6.1078 · exp ( 17.08085 · T 234.175 + T ) see ref % rH = p normalH 2 normalO ( T ) e normalw ( T ) · 100 p normalH 2 normalO ( T ) = % rH 100 · 6.1078 · exp ( 17.08085 · T 234.175 + T ) …”
Section: Methodsmentioning
confidence: 99%
“…The water vapor pressure over the IL solutions (p H 2 O ) was calculated from the measured relative humidity (% rH), the temperature (T) and the saturated vapor pressure of water (e w ) 22 using the Magnus equation.…”
Section: ■ Experimental Sectionmentioning
confidence: 99%