1. Outline Further Reading: Chapter 06 of the text book - what is a cloud? - cloud classifications - clouds and precipitation Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (1 of 11)

2. Introduction Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (2 of 11) Previously, –We learned that when air is displaced vertically, it cools due to adiabatic processes –Discussed causes of vertical motion Convection Orographic lifting –We also discussed what happens once the temperature cools to the dew point temperature, namely, we expect clouds to form as water vapor changes to liquid Today, –We want to discuss what forms these clouds take Classify cloud formations Discuss characteristics that allow us to identify different types of clouds

3. Cloud Type by Form Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (3 of 11) Clouds: –Optically thick mass of suspended water drops or ice crystals Clouds can be classified by some simple, but subjective, criteria that also provides information on the atmospheric conditions One form of classification is based on appearance or form Cirrus: Thin wispy cloudsStratus: Layered clouds with fairly continuous coverage Cumulus: Individual clouds characterized by heaped, puffy appearance Have vertical extent, from 1-3km up to tropopause

4. Cloud Type by Altitude-01 Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (4 of 11) Can also classify them based on their altitude “Cirro” “Alto” “Strato” “Fog” Cirro High clouds (7-18) km Cold (<-25 C) with exclusively ice crystals Cirrocumulus: high, puffy cloudsCirrus: high, wispy clouds

5. Cloud Type by Altitude-02 Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (5 of 11) Altostratus: thin, layered clouds Altocumulus: individual or “rolls” of clouds Alto Middle level clouds (2-7 km) 0-25 C composed of both water and ice crystals

6. Cloud Type by Altitude-03 Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (6 of 11) Stratus: Dense, uniform gray layers Stratocumulus: groups of dense, puffy clouds Strato Low level clouds (0 - 4 km) > 5 C composed of water

7. Cloud Type by Altitude-04 Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (7 of 11) Fog Clouds at ground level Radiation fog: forms at night when cold ground cools the air above it (in valleys) Advection fog: forms when warm, moist air moves over colder surface and cools (in coastal areas)

8. Cloud Type by Rain Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (8 of 11) Finally, we can classify them based on the presence of rain Nimbus: any cloud that rains Cumulonimbus: vertical clouds that produce rain Nimbostratus: low, flat clouds that drizzle

9. Thunderstorms Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (9 of 11) –Thunderstorms form when we have an unstable, moist atmosphere resulting in strong vertical motions –Actually composed of many individual circulation “cells” Updraft region is where the upward motion is intense and where the rain typically falls Downdraft region is associated with downward motion which can also be intense -> leads to downbursts Cells are typically 10-20km across and circulation within them occurs over 20 minutes or so, i.e. new cells can form in 20 minutes –Can produce hail: this is when an ice particle is continuously cycled through the convection cell before becoming heavy enough to fall out –Can also produce lightening: as water is moved within the cell, it develops a fictional charge; the discharge occurs through a spark, i.e. lightening

10. Clouds and Precipitation-01 Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (10 of 11) Rain (or any precipitation) –Requires Vertical motions -> cooling Presence of condensation nuclei -> something for the rain drops to form on –Condensation does not necessarily mean rainfall; could just form clouds –In order to form precipitation, the drops must be large enough to fall against the upward motion of the air This requires that the aggregation (or coalescence) of lots of water molecules into drops Cloud droplets are typically 50-100 micro-meters in diameter In contrast, rain drops are typically 500 micro-meters before they begin to fall (drizzle) At 1000-2000 micro-meters, they are considered rain drops

11. Clouds and Precipitation-02 Natural Environments: The Atmosphere GG 101 – Spring 2005 Boston University Myneni Lecture 15: Clouds Feb-28-05 (11 of 11) There are also other forms of precipitation Snow - crystallized water formed by the aggregation of frozen water Sleet - rain falling through a colder lower layer and freezing Hail - the aggregation of liquid water onto frozen water and subsequent freezing Note that precipitation does not necessarily fall straight to the ground - it might start to fall then get caught in an updraft and cycle through; during this process more aggregation occurs and we get very large rain or hail falling out (i.e. ‘golf-ball size hail’)