Traditional Culture Encyclopedia - Weather forecast - What is the latitude and longitude of Mashanzi Town, Wudi County, Shandong Province?

What is the latitude and longitude of Mashanzi Town, Wudi County, Shandong Province?

3 Longitude of World Map (λ)

The meridian looks like a curved vertical line projected on the map, but it is actually

Half of the great circle. The latitude lines projected on the latitude (φ) map look like horizontal parallel lines, but they are actually circles with different radii. All the positions with the same specific latitude are at the same latitude. Latitude is a circle and longitude is a semicircle. Latitude is used to indicate the east-west direction, and longitude is used to indicate the north-south direction. The latitude of the equator is 0, which divides the earth into the southern hemisphere and

Northern hemisphere. Latitude refers to the line connecting a point with the center of the earth sphere and the earth.

The line-plane angle formed by the equatorial plane is between 0 and 90 degrees. The latitude of a point located in the north of the equator is called north latitude, denoted by N, and the latitude of a point located in the south of the equator is called south latitude, denoted by S. The area with latitude between 0 and 30 degrees is called low latitude area, the area with latitude between 30 and 60 degrees is called middle latitude area, and the area with latitude between 60 and 90 degrees is called high latitude area. Equator,

Tropic of Capricorn,

Antarctic circle and

The Arctic Circle is a special parallel. Latitude 1 s Earth length

The total length of meridian is about 40008 kilometers. Average: Latitude 1 degree = about 1 1 km Latitude 1 min = about 1.85km Latitude 1 sec = about 30.8m 4 Latitude Urban low latitude range: between 30 north and south latitudes; Mid-latitude range: 30 degrees to 60 degrees north latitude and 30 degrees to 60 degrees south latitude; High latitude range: north of 60 degrees north latitude and south of 60 degrees south latitude; 90 degrees north latitude; 70 degrees north latitude;

Murmansk 60 degrees north latitude:

Oslo, Stockholm, Helsinki,

50 degrees north latitude of St. Petersburg:

London, Paris,

Brussels, Frankfurt,

Prague, Krakow,

Kiev, Vancouver,

North latitude of Moscow

40 degrees: Madrid,

Istanbul and Ankara,

Kashgar, Beijing, Salt Lake City,

Denver, Washington,

New york, Tokyo,

Seoul 30 degrees north latitude

Degree: Cairo,

Suez canal, Kuwait city,

Keywords New Delhi, Mount Everest, Lhasa,

Sanjiang

Parallel flow,

Chengdu, Chongqing, Three Gorges of the Yangtze River,

Wuhan, Hangzhou,

Houston, New Orleans

20 degrees north latitude: Hong Kong,

Keywords Taiwan Province province, Sahara desert, Jeddah,

Mumbai, Binmana,

Haikou, Fire Slave Lu Lu badminton,

North latitude of Mexico City 18 degrees:

Sanya north latitude 10 degree: Mexico city,

Conakry, Addis Ababa, Ho Chi Minh City,

Cebu, San Jose,

Panama canal, Panama city,

South latitude of Caracas 10 degree: Luanda,

Dili, port moresby,

20 degrees south of Lima and Recife: Antananarivo,

Suva, Sucre, 30 degrees south latitude

Degree: Sydney,

Cape Town, bloemfontein,

Durban, Brisbane, Easter Island,

40 degrees south of San Diego:

50 degrees south latitude of Wellington:

Strait of magellan 60 s: 70 s: 80 s: 90 s: Amundsen, Antarctica-

Scott Station 5 Tropic of Cancer

Tropic of Cancer, that is, 23 26' north latitude (the standard is 23 26' 28 "44). This is the northernmost line where the sun shines directly on the earth. Cross the tropic of cancer

This country has Morocco,

Argilli

Asia, Libya,

Egyptians, Tunisia, Israelis,

Jordan, Saudi Arabia,

United Arab Emirates, Pakistan,

India, Bangladesh, Myanmar,

China, Mexico,

America. The Tropic of Cancer passes through Taiwan Province Province.

Chiayi, Hualien, Taiwan,

Guangdong closed, Guangdong

Guangxi Shantou Conghua

Guiping

Tropic of Capricorn, which is 23 26 ′ (23 26 ′ 28 "44) south latitude. This is the southernmost boundary line where the sun shines directly on the earth. Tropic of Capricorn passes through the following countries:

Namibia, Botswana,

South Africa, Mozambique,

Madagascar; Australia;

Chile, Argentina, Paraguay and Brazil are divided into longitude 60 degrees: by crossing

The meridian of Greenwich astronomical rooftop is 0 degrees.

The longitude of east-west 180 degrees is called the west longitude. East longitude 180 degrees coincides with west longitude 180 degrees. It is the longest.

The latitude circle, the equator, is called the 0 parallel. The latitude measured from the equator to the north is called north latitude; The south is called the south latitude. South latitude and north latitude are 90 degrees respectively. The North Pole is 90 degrees north latitude. Because longitude connects the north and south poles, all the meridians are equal in length, indicating the north-south direction. The latitude represents both east and west directions. The warp and weft are perpendicular to each other and intertwined to form.

When looking at a map, we can use the latitude and longitude net to identify the direction and also judge the latitude and longitude position of any point on the earth. Meridians and latitudes can also divide the earth into several different hemispheres. Cut the earth along the equator like a watermelon, and the hemisphere north of the equator is called the northern hemisphere; The hemisphere south of the equator is called the southern hemisphere. If the earth is cut along the longitude of 20 west longitude and160 east longitude, then the hemisphere from 20 west longitude to160 east longitude is called.

Eastern hemisphere; The western hemisphere is called

Western hemisphere.

Alexander's empire was a flash in the pan and soon collapsed. But in a city called Alexandria in Egypt, there appeared a famous library, which served as a curator for many years.

Eratosthenes is knowledgeable and proficient in mathematics, astronomy,

Geography. He calculated that the circumference of the earth was 46,250 kilometers, and drew a map with 7 meridians and 6 latitudes.

World map. A young man also studied in this ancient library in 120.

Astronomical geography. He is Claudius. ...

Ptolemy. Ptolemy integrated the previous research results, thought that maps should be drawn according to fixed points with known latitude and longitude, and put forward the concept of drawing latitude and longitude network on maps. To this end, Ptolemy measured

The latitude and longitude of important cities and strongholds in the Mediterranean region have compiled 8 volumes of geographical works. Including the latitude and longitude of 8000 places. In order to draw the longitude and latitude lines on the earth on a plane, he tried to draw them into simple sectors, thus drawing the famous Ptolemy map. /kloc-navigator at the beginning of the 0/5th century

Henry began to put "Ptolemy Map" into practice. However, after repeated inspection, I found that this map is not practical. Some of Henry's captains said with regret, "Although we admire the famous Ptolemy very much, we found that the fact is contrary to what he said." A "standard clock" is the key to correctly determine the latitude and longitude. Making accurate clocks at sea to time is obviously more important than relying on

Celestial timing is much more convenient and practical. /kloc-the progress of mechanical technology in the 0/8th century has finally created conditions for solving this long-standing problem.

There is a watchmaker in Yorkshire, England.

Harrison, he spent 42 years making five sets in a row.

Timer, each one is more accurate and perfect, and the accuracy is getting higher and higher. sequence

Five stations are only the size of pocket watches, and the error caused by longitude measurement is only 1/3 miles. At about the same time,

The sea timepiece designed and manufactured by French watchmaker Pierre leroy has also been put into use. Longitude only affects latitude. Simply put,

Longitude has little effect on climate, but it is reflected in dependence.

Other factors determined by local topography and longitude affect the climate. There are many causes of climate, including latitude,

Keywords atmospheric circulation, land and sea position,

Ocean currents, topography, etc. Unless the causes of the same latitude are similar, it is possible to form the same climate. So the climate in the world is very diverse. Latitude position,

Keywords atmospheric circulation, land and ocean distribution,

Ocean currents and topography are the main factors affecting climate. The first two are global zonal factors, while the last three are non-zonal factors. Latitude position is the basic factor affecting climate. Because the earth is a big sphere, the sun shines at different angles at different latitudes. Some places are direct, some places are oblique, and some places have not been exposed to the sun all day or for months. Therefore, the local

With different solar altitude angles, the amount and heat of sunlight are different, and the temperature is also very different. Generally, the lower the latitude, the higher the temperature; The higher the latitude, the lower the temperature. Different latitudes in different regions are the main reasons for different global temperatures.

Atmospheric circulation is a variety of

The main factors of climate type and weather change. The air in the atmosphere moves at different scales, which is collectively called atmospheric circulation. It is an important way to transport and exchange heat and water vapor in the atmosphere. The manifestations of atmospheric circulation are planetary wind system, monsoon circulation,

Land-sea breeze, valley breeze, etc. The atmospheric circulation usually refers to the planetary wind system. The influence of atmospheric circulation on climate is very significant, and the equator

The updraft in the low pressure area is strong, the water vapor is easy to condense and the precipitation is rich;

Accessory fever

High pressure zone, sinking gas and steam prevail, water vapor is not easy to condense, and rain is scarce; In trade winds, air flows from higher latitudes to lower latitudes, and water vapor is not easy to condense, so it usually rains less. But on the east coast of the mainland, the trade winds blow from the sea, and there are more opportunities for precipitation; On the west coast of the mainland, the trade winds blow from the inland, so there is less precipitation. exist

In the area controlled by the westerly belt, the wind from the west coast of the mainland blows from the sea, with abundant water vapor and precipitation. The farther inland, the less water vapor and the less precipitation. On the east coast of the mainland, the west wind blows from the inland, with less precipitation. Generally speaking, the temperature of updraft and airflow changes from high to low from low latitude to high latitude, and water vapor is easy to condense, so there are more opportunities for precipitation. In the downward flow and the airflow from high latitude to low latitude, the temperature changes from low to high, and the water vapor is not easy to condense and precipitate.

There are fewer opportunities. Therefore, in different

Under the control of pressure belt and wind belt, the climate characteristics, especially the change of precipitation, are significantly different. Plus windbreaks and

The pressure belt moves with the seasons, thus forming a variety of different

Climate type. The distribution of land and sea changes the zonal distribution of temperature and precipitation. Due to the different physical properties of the ocean and the land, under the strong sunlight, the ocean heats up slowly and the land heats up quickly; After the sun weakened, the ocean cooled slowly and the land cooled rapidly. The amount of water vapor contained in the air on the ocean surface and land is also different. Generally speaking, in the ocean or offshore areas, the daily and annual changes of temperature are small, precipitation is abundant, and the seasonal distribution of precipitation is relatively uniform and relatively formed.

Maritime climate. Therefore, at the same latitude, at the same

Due to the different locations of land and sea, the areas controlled by pressure belt or wind belt have different climate characteristics. Terrain fluctuation will destroy the zonality of climate distribution. Terrain is a non-zonal factor, and different landforms have different effects on climate. In the same latitude zone, the higher the terrain, the lower the temperature, and the precipitation increases with the height within a certain height range. Therefore, in tropical mountainous areas, from

From the foothills to the top of the mountain, there has always been an area from the equator to the polar regions.

Climate change. In addition, tall mountains will block the airflow, and the temperature and precipitation on windward and leeward slopes of mountains are obviously different.

Ocean currents also have a certain influence on the climate along the coast of the continent through which they flow. The current from low latitude to high latitude has a great influence on the flow because it contains a lot of heat energy.

Coastal areas have the function of increasing temperature and humidity; Ocean current flows from high latitude to low latitude, and the water temperature is lower than the surrounding sea surface, which is very important for the flow of ocean current.

Coastal areas can reduce temperature and humidity. Therefore, in terms of temperature, ocean currents can adjust the temperature difference between high and low latitudes. Under the action of prevailing airflow, the temperature difference between the east and west coasts of the same latitude continent is significant, which destroys the zonal distribution of temperature latitude. Naturally, the first three items are the most important. Ocean currents only affect coastal areas, and the terrain is only partial. But large topography, such as the Qinghai-Tibet Plateau, has affected the atmospheric circulation. So geography books list topography, land and sea position and latitude as the most important factors. Longitude and longitude are divided into 360 degrees, and every 15 degrees has 1 time zones, where 0 degrees is called.

The prime meridian is the first place to enter a new day, and then there is a time difference of 1 hour every 1 time zone to the west. For example, it's 5: 00 a.m., so one time zone to the west is 4: 00 a.m., and the other time zone 1 is 3: 00 a.m., and so on, and the opposite is true to the east until.

The prime meridian, which means that the difference between the two sides of the prime meridian is just 23 hours, and the latitude is getting higher and higher from the equator. The equator separates the northern and southern hemispheres.

The dividing line of latitude and longitude is 1 degree =60 minutes =3600 seconds. This hexadecimal system was customized by the Babylonians, and we still use it today, as long as the angle and circle are the same. Latitude The equatorial latitude is 0, which divides the earth into two parts.

Southern hemisphere and northern hemisphere. Latitude refers to the line-plane angle between a point and the center of the earth and the equatorial plane of the earth, and its value is between 0 and 90 degrees. The latitude of a point located in the north of the equator is called north latitude, denoted by N, and the latitude of a point located in the south of the equator is called south latitude, denoted by S. The area with latitude between 0 and 30 degrees is called low latitude area, the area with latitude between 30 and 60 degrees is called middle latitude area, and the area with latitude between 60 and 90 degrees is called high latitude area. Equator,

Tropic of Capricorn,

Antarctic circle and

The Arctic Circle is special.

Latitude Latitude 1 sec length

The total length of the earth meridian is about 40008 kilometers. Average: latitude 1 degree = about 1 1 km latitude 1 min = about 1.85km latitude 1 sec = about 30.9mm.