Term quiz 4 Crossword
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
                                                          
 
 
Down: 2) The body of land on the leeward side of a mountain range that is relatively dry and hot. This is due to adiabatic warming and drying. 4) The rate at which a saturated body of air cools as it lifts. The averate rate for this in class is 6 degrees per 1000 meters. This adjustment is not used in reverse as air wams because it is no longer saturated.5) The measureable amount of water vapor that is in a difnable body of air 6) Uplift that occurs when a flowing body of air encounters a mountain range.7) Changes in temperature that occure due to variations in air pressure. 9) Air that becoms unstable only when certain conditions are met. If the air is cooler than surrounding area and then suddenly becomes warmer that the surrounding area, then the air becomes conditionally unstable. 10) Uplift of air that occurs when bubbles of warm air rise within an unstable body of air.15) A body of air that has a relatively low envirnmental lapse rate compared to potential uplifting air, thus strong convection cannot occur. Air that is cooler than the environment around it. 22) heat that can be felt and measured with a thermometer23) heat stored in molecular bonds that cannot be measured24) Change in temperature with height. 27) When a definable body of air is holding all the water it can. Across: 1) Puf clouds. that can grow upward. mid level but grow to great heights. 3) Uplift of air that occurs along the boundary of contrasting bodies of air.8) When the hydrogen bonds are formed, loosened, broken entirely, or tightened, water can move from one state (liquid, solid, or gas) to another. 11) added moisture to air near the saturation point. Also known as condensation cloud or mixing cloud. Dryer cooler air mixed with warm moist air. Only type of fog where the dew point changes. 12) Thin and whispy high level clouds Tiny ice crystals. High in atmosphere.13) Clouds that can happen at different heights, spread out. Mostly lower level and spread out 14) cumulious nimbulous cloud, strong upward motion causes strong downword motion, water droplets rise and fall each time collecting another layer of ice. Once the ice is heavy enough it falls to the ground.16) Fog that develops at night when temperature inversion exists. Ground cools faster than the air above cooling to the dew point. 17) Fog that developes when warm air flows over cooler air. Happens more often in maritime regions. Warm air moving over cool air, cooling it to the dew point. 18) the process through which water cahnges from vapor to liquid stage.19) The temperature at which condensation occures.20) Lowest height at which condensation can begin.21) Uplift of air that occurs when large bodies of air meet in a central location. 25) the process through which water changes from the liquid to vapor stage.26) Water droplets form in cloud above freezing temperature, then hit the freezing air on the way down to the earth. 28) Rain that forms and then falls through thinner layer of freezing air, doesnt have time to freeze until it hits the surface which is at freezing temperatures cauzing the rain to freeze to the surface it hits. 29) The ratio between the specific and maximum humidity. 30) The maximum amount of water vapor that a definable body of air can hold at a given temperature. 31) The rate at which an unsaturated body of air cools while lifting or warms while decending . 10 degrees per 1000 meters. This adjustment works in reverse as air wams and decends. 32) A body of air that has a relatively high environmental lapse rate compared to uplifting air within it, thus strong convection can occur. Air that is warmer than the environment around it.
 

 

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