Weather: How it Works and why it MattersPerseus Pub., 2000 - 223 pàgines |
Des de l'interior del llibre
Resultats 1 - 3 de 86.
Pàgina 18
... temperature and the dew point temperature , always as cool as or cooler than the air temperature . The problem with the relative humidity is that , because it is not a fully independent parameter , it de- pends on the value of the ...
... temperature and the dew point temperature , always as cool as or cooler than the air temperature . The problem with the relative humidity is that , because it is not a fully independent parameter , it de- pends on the value of the ...
Pàgina 25
... temperature at which ice melts . Many temperature scales have been proposed and put into practice , all based on assigning values to two reproducible temperatures , the particular device interpolating be- tween them . The scales ...
... temperature at which ice melts . Many temperature scales have been proposed and put into practice , all based on assigning values to two reproducible temperatures , the particular device interpolating be- tween them . The scales ...
Pàgina 26
... temperature was chosen so that at the two previously used fixed points the physical temperature agreed with the temperature on the Celsius scale . Among other things , the theory led to the discovery that there is an absolute zero point ...
... temperature was chosen so that at the two previously used fixed points the physical temperature agreed with the temperature on the Celsius scale . Among other things , the theory led to the discovery that there is an absolute zero point ...
Continguts
Introduction | 1 |
The Fundamentals of Air | 7 |
Its Not the Heat Its the Heat and the Humidity | 15 |
Copyright | |
No s’hi han mostrat 15 seccions
Altres edicions - Mostra-ho tot
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abundance acid air masses altitude amount Atlantic atmos atmosphere atomic average carbon dioxide cause century clouds cold colder comet cool Coriolis Effect density dew point difference Earth Earth's atmosphere El Niño energy ENSO equator eruption Europe event feet Figure forests fossil fuels glaciers global temperature global warming greenhouse effect greenhouse gases Greenland ground Gulf Stream heat Holocene humidity hurricanes increase isotope kilometers known land latitude layers Little Ice Age major measure mechanism meters midlatitudes miles molecules Moon Niño North America Northern Hemisphere occur ocean currents orbit oxygen ozone particles percent period phere planets plankton polar poles precipitation predict present produce rain reached records regions rise satellites scale sea level seasons snow snowfall solar radiation storms stratosphere summer surface tion trees trend Tropics troposphere ture variations vegetation Venus volcanic warmer water vapor weather weather lore wind winter Zone