MindMap Gallery College Entrance Examination Geography-Atmosphere Topic
Regarding the college entrance examination geography-atmosphere topic mind map, the second round of college entrance examination review summarizes the structure of the atmosphere, heating process, climate type, Weather systems, atmospheric movements, etc.
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This is a mind map about bacteria, and its main contents include: overview, morphology, types, structure, reproduction, distribution, application, and expansion. The summary is comprehensive and meticulous, suitable as review materials.
This is a mind map about plant asexual reproduction, and its main contents include: concept, spore reproduction, vegetative reproduction, tissue culture, and buds. The summary is comprehensive and meticulous, suitable as review materials.
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Atmospheric topics
Atmospheric structure
Division basis
Change patterns with altitude
category
troposphere
Origin of name
Hot below and cold above
Thermal expansion - density becomes smaller, cold contraction - density becomes larger
Features
The air flow is relatively unstable and the weather is changeable
Uncertain thickness
The temperature near the ground determines
Low latitude (<30)
17-18km
Mid-latitudes (30-60
11-12km
High latitude (60-90)
8-9km
Temperature decreases with increasing altitude
Heat source: ground radiation or ground
The temperature decreases by 0.6 for every 100 meters of elevation?
limitation
temperature vertical lapse rate
average
actual
Effect of moisture in the air
inversion layer
What is it?
in the troposphere
H rises and T rises or H rises and T falls but is less than 0.6
type
frontal inversion
cold front
warm front
Warm and cold air masses meet
冷气团在下,暖气团在上
advection inversion
At the seaside, when warm and cold air meet softly, the warm air slowly rises above and the cold air falls below.
topographic inversion
In valley areas, cold air sinks to the valley bottom and gathers, and the air at the bottom of the valley is pushed upward.
Radiative inversion
born after sunset
The ground is programmed from a "heat source" to a "cold source"
Who is closer to the ground and who has the lower temperature?
Inversion layer last
before sunrise
weaken to disappear
after sunrise
Generate conditions
A region with higher dimensions, Northeast my country
sunny
Influence
favorable
low altitude flight
Equivalent to the stratosphere
factory chimney height
unfavorable
It affects air convection, concentrates pollutants, and easily produces "haze" weather.
stratosphere
Origin of name
hot at the top and cold at the bottom
Mainly advection motion
Features
The airflow is relatively stable and the weather is mainly sunny
Uneven thickness
As altitude increases, temperature and height
airplane flight
upper atmosphere
1Heating process
The sun shines on the earth
Sun radiation
UV zone
UV rays
X-ray
Visible light area
0.4um-0.75um
Infrared area
infrared
FM
Sun radiation
upper atmosphere
stratosphere
ozone layer
UV rays
troposphere
carbon dioxide and water vapor
Absorb infrared rays
clouds
Reflection without selectivity
little dust
Scattering of blue and violet light with shorter wavelengths
red yellow green
car tail light
It's already dawn before the sun rises
blue sky
About 30% of solar radiation
地面反射
新雪
冰面
地面吸收
The earth warms the atmosphere
Ground radiation
troposphere
water vapor and carbon dioxide
infrared
stratosphere
few
upper atmosphere
almost 0
The atmosphere returns to the earth
atmospheric reverse radiation
troposphere
long wave radiation
Ground insulation
upper atmosphere
atmospheric radiation
Insulation
温室大棚
全球气候变暖
二氧化碳
温差的问题
晴天温差大
晴天,云层少,对太阳辐射的削弱作用弱,到达地面的太阳辐射量大,地面吸收的多,释放的地面辐射量大,气温高。
夜晚,云层少,大气逆辐射作用弱,气温低。
海陆分布
Atmospheric movement
Movement style
vertical movement
Uneven hot and cold conditions on the earth's surface
thermal reasons
horizontal movement
horizontal pressure gradient force
dynamic reasons
Common types
thermodynamic circulation
Isobars
feature
Similar to contour lines
application
B>A=D>C
Near ground conditions
judgment hemisphere
wind direction wind force
principle
Evenly heated
The isobaric surface is parallel to the ground
calm state
Under uneven heating conditions
vertical movement
thermal reasons
horizontal movement
dynamic reasons
application
sea and land breeze
valley wind
heat island effect
Air pollution factory layout
Suburban areas outside the heat island effect
Greenbelt
between suburbs
Three circles of circulation
Assumption 1: The earth’s surface is uniform and unfair
single circulation
Assumption 2: The earth’s surface is uniform and unfair
There is rotation and geostrophic deflection force
4 air pressure belts
thermal reasons
equatorial low pressure belt
rainy
polar high pressure zone
clear
dynamic reasons
subtropical high pressure zone
clear
subpolar low pressure zone
rainy
3 wind belts
Northeast trade wind belt
clear
prevailing westerlies
rainy
polar easterly belt
clear
Assumption 3: The surface is uniform
The air pressure and wind belts move between the Tropic of Cancer and the Tropic of Cancer as the direct sun shines.
In the Northern Hemisphere, summer moves north and winter moves south
Hypothesis 4: Distribution on land and sea
The air pressure belt is cut
Monsoon circulation
东亚季风
夏季东南风
冬季西北风
Differences in thermal properties between sea and land
南亚季风
夏季西南风
东南信风带北移越过赤道受向右偏转力影响
冬季东北风
海陆热力性质差异
拓展:如考查区域在南北纬30附近,大多考查全球气压带风带的移动造成风向的转变。
climate type
form
west and central
east
热带雨林气候
全年高温多雨
赤道低气压
热带草原气候
全年高温,有明显的干湿两季
赤道低气压带与信风带交替控制
热带沙漠
全年高温干燥
信风
信风与副高交替
副高
Trade wind or sub-high control
地中海气候
夏季炎热干燥,冬季温和多雨
副高与西风带交替
温带海洋性气候
全年温和湿润
西风带
热带季风气候
全年高温,有明显的旱雨两季
气压带和风带移动和海陆热力性质差异
亚热带季风
夏季高温多雨,冬季温和少雨
温带季风
夏季高温多雨,冬季寒冷干燥
East Asian monsoon (differences in thermal properties between sea and land)
Rain and heat in the same period
温带大陆性气候
降水少,温差大
深居内陆,远离海洋
Interpretation
positional method
indicator method
1 To stabilize the ball
Look at the temperatures in July and January
2 Set the zone with the (lowest) temperature
15 and above
tropical
desert
Low rainfall throughout the year
20mm/M
rainforest
Rainy all year round
200mm/M
Monsoon
summer rain type
grassland
summer rain type
Comparative analysis
年降水量
季风(1500mm)>草原(1000mm)
降水变率
季风(旱雨两季)>草原(干湿两季)
分布情况
南半球无热带季风气候
0-15
subtropical
Mediterranean
Winter rain type
Monsoon
summer rain type
temperate ocean
Annual rain pattern
Below 0
temperate zone
Monsoon
750mm
mainland
350mm
3 Set the shape with water
Determine climate type based on precipitation characteristics
recitation method
particularity
Equatorial savanna climate
East African Plateau
Savanna-tropical rainforest
east side of madagascar
describe
General description
Mediterranean climate – hot and dry summers, mild and rainy winters
rational description
General description data to combine
specific description
temperature
Average annual temperature
Variety
daily variation
seasonal changes
Interannual variability
precipitation
annual precipitation
Variety
seasonal changes
Interannual variability
weather system
frontal cyclone
frontal system
horizontal movement
warm front
Before transit
Controlled by a single cold air mass, sunny, cold and high pressure
in transit
continuous precipitation
in front of the front
after transit
Single warm air mass control, sunny, warm and low pressure
cold front
Before transit
Single warm air mass, sunny and warm
in transit
Rain, snow, hail, significant cooling, strong winds, sandstorms
behind the front
after transit
Single cold air mass control, sunny, low and high
The inclination angle of the front (cold front > warm front)
冷锋的雨区<暖锋的雨区
quasi-stationary front
evenly matched
Jianghuai quasi-stationary front
June rainy season
empty plum
super plum
Terrain blocking
Kunming quasi-stationary front
winter
freezing rain
Prison Feng
Cyclonic and anticyclonic systems
vertical movement
cyclone
low pressure
anticyclone
high pressure
北-气-逆,每次变俩
Schematic diagram
Judgment of cold front and warm front: left cold front, right warm front;
Judgment of precipitation area: behind cold front, in front of warm front, cyclone center;
Weather changes before and after the front passes: consistent with cold and warm fronts
Interpretation of wind direction
Interpretation of wind force: The wind speed is high when isobars are densely packed, and vice versa;
Determine the Northern and Southern Hemispheres