Transcript Lecture Packet#11

Chapter Thirteen
Global Climate
What we are going to learn?
We are going to learn the answers to the following
questions
–
–
–
–
What are the factors that regulate global climate?
How are climates are classified?
What are the different types of climate?
What are micro-, macro- and meso-climates?
Climate
•
•
•
•
•
•
•
Climate: Average of the day-to-day weather over a long duration
Microclimate: Small climatic region near or on the ground
Mesoclimate: Climate of a small area of the earth’s surface
Macroclimate: Climate of a much larger area (state or a country)
Global Climate: Climate extending over the entire earth
Two important weather elements: temperature & precipitation
Climate Controls are:
–
–
–
–
–
–
–
Intensity of sunshine and its latitudinal variations
Ocean currents and thermohaline circulation systems
Relative distribution of land and water
Wind intensity and direction
Position of high- and low-pressure areas
Mountain barriers
Altitude
Global Temperatures
Global temperatures – (cont.)
• Isotherms are oriented East-West (same latitude locations
receive same amount of solar energy)
• Bending of isotherms along the coastal margins is partly
due to the unequal heating & cooling of land & water
• Variation in temperature between summer and winter will
be far greater over continental interiors than along the
west coastal margins of continents; climates of interior
continental regions will be more extreme (higher summer
temp and lower winter temp) than their counterparts in the
west coast; west coast climates are typically quite mild for
their latitude
• Highest mean temperatures do not occur in the tropics,
but rather, in the subtropical deserts of the Northern
Hemisphere
Global Temperatures – (cont.)
• Lowest mean temperatures occur over large land
masses at high latitudes; coldest area of the world is the
Antarctic
– Snow and ice reflect ~80% of the sunlight that reaches the
surface; much of the absorbed solar energy is used to
transform the ice and snow into water vapor
• Southern Hemisphere is cooler than Northern
Hemisphere because:
– Cold Antarctic
– Polar regions of the Southern Hemisphere reflect more
incoming sunlight
– Less land area found in the tropical and subtropical areas
Global Precipitation
• Global distribution of precipitation is closely tied to the
general circulation of the atmosphere and to the
distribution of mountain ranges & high plateaus
• Equatorial regions are typically wet, while the subtropics
and the polar regions are relatively dry
• Precipitation is most abundant where the air rises; least
abundant where it sinks
• In tropical regions, the trade winds converge along the
ITCZ producing rising air --- heavy precipitation all year
long; near 30 deg, the sinking air of the subtropical highs
produces a ‘dry belt’ around the globe – presence of
Sahara Desert of North Africa in this region
Annual global pattern of precipitation
Global Precipitation – (cont.)
• In the cold air of the polar regions there is little moisture --winter storms drop light, powdery snow that remains on the
ground for a long time because of the low evaporation rates;
in summer a ridge of high pressure tends to block storm
systems that would otherwise travel into the area --precipitation is low in the arctic
• Heaviest precipitation is concentrated in the eastern states,
as moisture from the Gulf of Mexico moves northward;
cities on the plains receive more rainfall in summer ; those
on the west coast have maximum precipitation in winter
• Cities in the midwest and East usually have abundant
rainfall all year long
Vertical cross section along a line running N-S
illustrating main global regions of rising and sinking air
Global climate – (cont.)
Hottest places on earth generally occur in the subtropical
deserts of the Northern Hemisphere, where clear skies
and sinking air produce clear skies and scorching heat
Coldest places on earth tend to occur in the interior of highlatitude land masses; The coldest areas of the Northern
Hemisphere are found in the interior of Siberia and
Greenland; coldest area of the world is Antarctic
Wettest places in the world are located on the windward
side of mountains where warm, humid air rises upslope
Driest places in the world are located on the leeward
(downwind) side of mountains where air parcels undergo
drying and compressional heating [rain shadow]
Variations in annual precipitation for three
Northern Hemisphere cities
Pacific Northwest, U.S.
Effect of topography on average annual precipitation
along a line from the Pacific Ocean through CA and
western Nevada
Key to map of precipitation records thoughout
the world
• Key
Some precipitation records
.
Climatic Classification – The Köppen System
• Similarity in climate (temperature and precipitation) in an
area forms the basis for classification
• Köppen related distribution & types of vegetation to
climate; five major climatic types designated by A
(tropical moist Climate), B (dry climate), C (moist midlatitude climates with mild winters), D (moist mid-latitude
climates with severe winters) & E (polar climates)
• Tropical Moist Climate (A): Monthly average temp
above 18°C; no real winter season and year around warm
temp.; abundant rainfall (>150 cm); extends from equator
to ~15-25 ° N or S;
• Examples: Amazon lowland of South America, the Congo
River Basin of Africa, and the East Indies from Sumatra to
New Guinea;
Major Climate Regions of the World
Köppen System
Type – A Climatic zone – (cont.)
• High temperature and abundant rainfall --- dense,
broadleaf, evergreen forest – tropical rain forest with
vegetation; abundant sunlight allows for the growth of
tangled shrubs forming impenetrable jungle
• Major types are tropical wet (Af) and tropical monsoon
(Am) and tropical wet and dry (Aw);
• Tropical wet climate: seasonal temperature variations are
< 3° C; greater variation in temperature between day &
night (diurnal, average high ~32°C & average low
~22°C) than annual temperature variation;
– towering cumulus clouds form every day to produce heavy,
localized showers in the afternoon; annual rainfall > 150 cm
(windward side can exceed 400 cm/yr);
– high humidity & cloud cover tend to keep maximum temp from
reaching very high values
Temperature and Precipitation data for Peru
(latitude 4°S; tropical wet climate, Af)
Climate A Type – (cont.)
• In Peru, monthly rainfall variations are more than the
temperatures --- due to migrating position of the
intertropical convergence zone (ITCZ) & associated
wind patterns
• Laterite: A soil formed under tropical conditions where
heavy rainfall leaches soluble minerals from the soils
leaving soil hard and poor for growing crops
• Tropical Monsoon Climate: When precipitation totals
drop below 6 cm for perhaps one or two months; a
tropical climate with a brief dry period of perhaps one or
two months; examples coasts of southeast Asia, India,
and in northeastern South America
Climate A Type – (cont.)
• Tropical wet and dry climate (Aw): Distinct dry season
prevails; annual rainfall >100 cm, but monthly rainfall
for more than 2 months is <6 cm --- rainforests cannot
survive to this ‘drought’ giving rise to coarse savanna
grass, scattered with low, drought-resistant deciduous
trees
• Examples of Aw climate are: western Central America,
north and south of the Amazon Basin (South America),
southcentral Asia and northern Australia
Climate data for Timbo, Guinea (11°N) – tropical
wet-and-dry climate (Aw)
Dry Climates (Group B)
• Dry Climate: Evaporation (E) + Transpiration (T) > Precipitation (P)
• Subtropical deserts extend from ~15-30° (often surrounded by
mountains)
• ~26% of land area falls in this group
• Major types: Arid (BW; 12% of the land) and Semi-arid (BS; 14%
of the land)
• Arid region is divided as follows:
– a) BWh or BSh: Climate is hot & dry with a mean annual T of above 18°C;
– b) BWk or BSk: Climate is cold (in winter) and dry with mean annual T <
18°C
• Examples for Arid region: West coast of South America, Africa and
over much of the interior of Australia
• In North America, arid climate extends from northern Mexico into
the southern interior of the US
• Most of the native plants are xerophytes (capable of surviving
prolonged periods of drought)
Rain streamers (virga) in dry climates, as falling
rain evaporates into the drier air beneath the cloud
Bushes and cactus found in the arid
southwestern American deserts (BWh)
Dry climate – B – (cont.)
• In low-latitude deserts (BWh),
– maximum daytime during the summer can >50°C (40-45°C; (104-113°F)
are more common); RH in the middle of the day 5-25%;
– minimum T can drop below 25°C
• Mid-latitude deserts (BWk):
– Summer maximum temp reaches 40°C (104°F);
– Winters are extremely cold with minimum temp below -35°C (-31°F);
– Lie in the rain shadow of an extensive mountain chain (Sierra Nevada and
Cascade mountains in North America), Himalayan mountains and Andes in
South America
• Around the margins of the arid regions, where rainfall amounts are
greater, the climate is gradually changes into semi-arid (BS);
– examples: Most of the Great Plains, southern coastal sections of California,
& northern valleys of the Great Basin; annual precipitation 20-40 cm;
examples are: Denver, Colorado
Arid (BWh) Climate – Phoenix, AZ (33.5°N)
Cumulus clouds in a semi-arid climate (BS) in
Western North America
Climatic data for Denver, CO (40°N) – a semi-arid
climate (BSk)
Moist subtropical mid-latitude climates
(Group C)
• Humid with mild winters with the average temp of the
coldest month -3°C to 18°C (27-64°F); commonly found
on the eastern and western regions of most continents,
25-40° latitude
• Major types: Humid subtropical (Cfa), marine (Cfb) and
dry-summer subtropical or Mediterranean (Cs)
• Humid subtropical climate (Cfa): Found principally
along the east coasts of continents, ~25-40° latitude;
– summer is hot and muggy; summer dew-point temp and RH
are high (exceeding 23°C or 73°F); Mobile, AL
– In winters, frost, snow, and ice storms are more common, but
heavy snowfalls are rare
• Rainfall: 80-165 cm/yr, fairly well distributed in an yr
Climatic data for Mobile, Alabama (30°N) – a
humid subtropical climate (Cfa)
Moist subtropical - Marine
• Marine (Cfb): Along western side of most continents
from 40 to 60°; winds from the oceans moderate the
climate; summers are quite cool
• Low annual temperature range in high latitude region –
ocean’s influence keeps daily temp ranges low
• Coastal Mediterranean Climate: Precipitation: 30-90
cm/yr; summer afternoon temperatures climb above
34°C(93°F) and occasionally above 40°C (104°F);
• San Francisco, CA & Sacramento, CA are only 130 km
(80 miles) apart (inland) and average July temp is 9°C
(16°F) higher at Sacramento
Climatic data for Port Hardy, Canada (51°N)
– marine climate
Comparison of a coastal Mediterranean climate
(Csb; San Francisco) with an interior
Mediterranean climate (Csa) Sacramento
Moist Continental Climates (Group-D)
• Warm-to-cool summers and cold winters [warmest
month average temp >10°C (50°F) & coldest monthly
average temp drops below -3°C (27°F)]; D climates are
controlled by large land masses; found only in the
Northern hemisphere; D climates extend across North
America and Eurasia (40° - ~70°N)
• Major types:
– Humid continental with hot summers (Dfa; long and hot
summer; mid-day temp exceed 32°C (90°F; nights are usually
warm & humid),
– Humid continental with cool summers (Dfb; less humid; temp
can exceed 35°C (95°F)) and subpolar (Dfe)
Comparison of a humid continental hot summer climate, Dfa (Des
Moines) with a humid continental cool summer climate (Winnepeg)
Subpolar climate (Dfc) – Fairbanks, AK (65°N); winters are
severe, summers are short & cool, 1-3 months exceed mean
temp of 10°C (50°F)
Polar Climate – Group E
• Year-round low temp (average temp of the warmest
month < 10°C (50 °F), but above freezing;
• Two major types: Polar tundra (ET) and Polar ice caps
(EF)
• Polar tundra: ground is permanently frozen (Permafrost)
• Annual precipitation < 20 cm (in lower latitudes, would
constitute desert, but in the cold polar regions,
evaporation rates are very low and moisture is adequate)
• Polar ice cap: Temp for every month is below freezing,
plant growth is impossible & the region is covered with
snow and ice – Greenland and Antarctica; precipitation
< 10 cm/yr
Climate data for Barrow, Alaska (71°N) – polar
tundra climate (ET)
Climatic data for Eismitte, Greenland (71°N); polar
ice cap climate; ~ 3000 m above MSL (EF)
Highland Climates (Group H)
• Varying climate with altitude – 300 m elevation is
equivalent to traveling 300 km northward (3°N)
• Ascending on a mountain, one can travel through many
climatic regions in a relatively short distance
• Elevation in the central Sierra Nevada:
–
–
–
–
Base of the mountain: semi-arid conditions;
foothills: Mediterranean and the vegetation changes;
higher elevations: subpolar and vegetation changes;
near the summit, permanent patches of ice and snow, with
some glaciers (in less than 4 km),
the climate has changed from semi-arid to polar
Vertical view of changing vegetation and climate due
to elevation in the central Sierra Nevada
Chapter Summary
•
•
•
•
•
•
•
•
•
•
Micro-, meso-, and macro-climate with examples
Rain shadow desert and rainiest places
Rainforests exist in what climatic conditions?
What is a dry summer? Explain why it is a dry summer
Lowest temperature and precipitation in the world
Köppen classification system – type A, B
Monsoon
Characteristics of tropical wet climate, wet-and-dry climate
Most abundant climate type in the planet
Humid Subtropical climate; Mediterranean climate; D-type
climate where it is found in US;
• Which climate type normally has the larges and smallest annual
range in temp; subpolar temperature; polar ice cap climate;
tundra climate;