Weather: How it Works and why it MattersPerseus Pub., 2000 - 223 pàgines |
Des de l'interior del llibre
Resultats 1 - 3 de 28.
Pàgina 17
... reached and condensa- tion or precipitation occurs . Warm and cool air have one more fundamen- tal difference : Warm air is always lighter and more buoyant than cool air and will rise whenever cool air surrounds it . The difference can ...
... reached and condensa- tion or precipitation occurs . Warm and cool air have one more fundamen- tal difference : Warm air is always lighter and more buoyant than cool air and will rise whenever cool air surrounds it . The difference can ...
Pàgina 163
... reached , in- cluding the Montreal Protocol of 1989 and the London agreement of 1991 : CFC production would be phased out entirely by 1995 , and most of the world is adhering to these agreements . Their effect will not be noticeable for ...
... reached , in- cluding the Montreal Protocol of 1989 and the London agreement of 1991 : CFC production would be phased out entirely by 1995 , and most of the world is adhering to these agreements . Their effect will not be noticeable for ...
Pàgina 204
... reaching the ground in the case of vertical incidence would be given by the solid curve just below the dashed curve in Figure A.1 ; the space between that solid curve and the dashed curve represents the energy absorbed by the air . The ...
... reaching the ground in the case of vertical incidence would be given by the solid curve just below the dashed curve in Figure A.1 ; the space between that solid curve and the dashed curve represents the energy absorbed by the air . The ...
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
Frases i termes més freqüents
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