Transcript Slide 1
1. Clouds are made up of: A. B. C. D. Liquid water droplets Ice Crystals Water Vapor A combination of liquid water, ice, and water vapor 2. The liquid water droplets and ice crystals which make up clouds are denser than the surrounding air molecules. Why don’t they fall to the ground? A.They are attracted to each other by electrical forces and water tension. B.They are far enough apart that the density is not actually greater C.Upward movement of air keeps them aloft D.It is too warm at ground level 5. Why does upward movement of air create clouds (and precipitation)? A. B. C. D. E. Air cools as it rises Relative humidity decreases as air cools Cooling of saturated air results in condensation of water vapor A, and C A, B, and C 3. What “lifting mechanism” occurs when rising air remains warmer (less dense) than the surrounding air? A.Convection B.Orographic Lift C.Convergence D.Weather Fronts 4. Air converging towards an area of _______________ is forced upward, often creating clouds and precipitation. A. B. C. D. Warm temperature Low pressure High pressure Cold temperature Precipitation Processes: Growth of Cloud Drops •A raindrop is 100 times larger than a cloud droplet. •A cloud droplet is 100 times larger than a condensation nucleus. •1,000,000 cloud droplets = 1 raindrop Two Important Precipitation Processes • Collision and Coalescence (warm cloud) Process – Strictly liquid cloud droplets • Ice-Crystal (Bergeron) Process – ice crystals and liquid cloud droplets both must co-exist at temperature below freezing Collision & Coalescence Process Warm Cloud Raindrop Formation Processes •Collision and coalescence operates in warm clouds to produce rain, and is affected by the: •1) clouds liquid water content (LWC) •2) droplet sizes •3) cloud thickness •4) updrafts •5) drop electrical charges. Ice Crystal (Bergeron) Process “important precipitation process in the middle and high latitudes” •Cloud droplets are still composed of liquid water below the freezing level (supercooled). COLD CLOUDS •The pure water in a small amount has a lower freezing temperature. (small cloud droplets) •Cold clouds may drop below -40° C before small droplets freeze into ice embryos that can serve as condensation nuclei (ice nuclei). more water droplets than ice crystals WARM CLOUDS Molecules from Water to Ice Ice crystals have lower saturation vapor pressures than liquid droplets, creating a gradient of high to low water molecules from liquid to ice that encourages ice growth. Ice Particle Changes Accretion or Riming Aggregation Graupel •As ice crystals fall and collide with super cooled drops, they get bigger by accretion. •Falling icy matter is called graupel (snow pellet), and aggregation describes the joining of two ice crystals into snowflakes. •If the snowflake melts while falling, it continues down as a raindrop. •Much of the rain, even in the summer, in the middle and northern latitude falls as snow initially. Precipitation Types • Rain • Snow • Sleet and Freezing Rain • Snow Grains and Snow Pellets • Hail Rain • A falling drop must have a diameter 0.5 mm to be considered as rain. • Uniform drops with diameter < 0.5 mm are called drizzle. • Showers are considered intermittent precipitation, usually short in duration but often heavy. Evaporating Rain Rain falling into low humidity air below will cause the drops to decrease in size, possibly evaporating into streaks of dry air as in this virga. Snow • Can fall as much as 300 m (1000 ft) below the freezing level before melting completely. • In a drier environment, snowflakes can reach the ground even if the surface layer temperature is above freezing due to evaporative cooling effect. • It is never “too cold” to snow. Average Annual Snowfall Sleet & Freezing Rain For each case, determine whether the air will be above or below freezing at each level in order that precipitation of the selected type will occur. There may be more than 1 possible answer. Try this based on how each precipitation type was described in class, rather than using your book. RAIN 3000m SNOW SNOW * * * * * * 3000m (Below Freezing) SNOW * (Below * * Freezing) * * * FREEZING RAIN SLEET 3000m SNOW * (Below * * Freezing) * * * 3000m SNOW * * * * * * (Below Freezing) 2000m 2000m 2000m 2000m 1000m 1000m 1000m 1000m Surface Surface Surface Surface Hailstones & Damage Radar Rainfall •Doppler radar uses microwave transmission and reception to measure backscatter intensity, or reflectivity for large geographic areas. •This signal is converted into maps of precipitation intensity, while phase shift data provide information on storm movement.