This document discusses air masses and their types. It defines an air mass as a large body of air with similar temperature and humidity that forms in stable source regions. There are two main types of air masses - continental and maritime. Continental air masses originate over landmasses and are usually dry, while maritime air masses originate over large bodies of water and are usually moist. Specific continental air masses include tropical (cT), mid-latitude (cM), and polar (cP). Maritime air masses include tropical (mT), mid-latitude (mM), and polar (mP). Each air mass has distinct characteristics depending on its source region and how it interacts with terrain as it moves across regions.
Fronts are boundaries between two air masses of differing characteristics. There are four main types of fronts: cold fronts, warm fronts, occluded fronts, and stationary fronts. Cold fronts are steep boundaries where cold air overrides warm air, bringing precipitation. Warm fronts are more gradual, with light, continuous precipitation as warm air rises over cold air. Occluded fronts occur when a cold front catches up to a warm front. Stationary fronts have little or no movement as the air masses are parallel.
There are several major air masses that influence weather patterns:
1) Continental Arctic (cA) air masses are very cold and dry, originating north of the Arctic Circle.
2) Continental polar (cP) air masses are cold and dry, originating in northern Canada and influencing northern US weather.
3) Maritime polar (mP) air masses are cool and moist, originating over the North Atlantic and Pacific and influencing the Pacific Northwest and Northeast.
4) Maritime tropical (mT) air masses are warm and moist, originating in the Gulf of Mexico and influencing the eastern US.
Mat geo 1ºem_cartografia-orientação_localização_06-02-2012daniboy7lag
O documento fornece informações sobre orientação e localização, abordando conceitos como rosa dos ventos, coordenadas geográficas, fusos horários e instrumentos de orientação como bússola e GPS. Explica como o Sol, a Lua e estrelas eram usados para orientação e como paralelos, meridianos e outros elementos formam a rede geográfica para determinar a localização exata de qualquer ponto.
Plate tectonics describes how the Earth's crust is divided into tectonic plates that move relative to each other. The movement of plates is caused by convection currents in the asthenosphere and results in major geological events at plate boundaries like earthquakes, volcanoes, and mountain building. There are three types of plate boundaries - divergent where plates move apart, transform where they slide past each other, and convergent where they push together.
This document discusses air masses and their types. It defines an air mass as a large body of air with similar temperature and humidity that forms in stable source regions. There are two main types of air masses - continental and maritime. Continental air masses originate over landmasses and are usually dry, while maritime air masses originate over large bodies of water and are usually moist. Specific continental air masses include tropical (cT), mid-latitude (cM), and polar (cP). Maritime air masses include tropical (mT), mid-latitude (mM), and polar (mP). Each air mass has distinct characteristics depending on its source region and how it interacts with terrain as it moves across regions.
Fronts are boundaries between two air masses of differing characteristics. There are four main types of fronts: cold fronts, warm fronts, occluded fronts, and stationary fronts. Cold fronts are steep boundaries where cold air overrides warm air, bringing precipitation. Warm fronts are more gradual, with light, continuous precipitation as warm air rises over cold air. Occluded fronts occur when a cold front catches up to a warm front. Stationary fronts have little or no movement as the air masses are parallel.
There are several major air masses that influence weather patterns:
1) Continental Arctic (cA) air masses are very cold and dry, originating north of the Arctic Circle.
2) Continental polar (cP) air masses are cold and dry, originating in northern Canada and influencing northern US weather.
3) Maritime polar (mP) air masses are cool and moist, originating over the North Atlantic and Pacific and influencing the Pacific Northwest and Northeast.
4) Maritime tropical (mT) air masses are warm and moist, originating in the Gulf of Mexico and influencing the eastern US.
Mat geo 1ºem_cartografia-orientação_localização_06-02-2012daniboy7lag
O documento fornece informações sobre orientação e localização, abordando conceitos como rosa dos ventos, coordenadas geográficas, fusos horários e instrumentos de orientação como bússola e GPS. Explica como o Sol, a Lua e estrelas eram usados para orientação e como paralelos, meridianos e outros elementos formam a rede geográfica para determinar a localização exata de qualquer ponto.
Plate tectonics describes how the Earth's crust is divided into tectonic plates that move relative to each other. The movement of plates is caused by convection currents in the asthenosphere and results in major geological events at plate boundaries like earthquakes, volcanoes, and mountain building. There are three types of plate boundaries - divergent where plates move apart, transform where they slide past each other, and convergent where they push together.
This document discusses the field of geology. It provides definitions and examples of key topics in geology, including the study of Earth materials and processes, as well as the history and evolution of the planet. Important figures in the field like Charles Bonnet and Reinhard Mack are mentioned. The document also outlines related fields and required education to become a geologist, noting they study applied science and work to understand Earth processes, locate resources, and advise on development and construction projects.
The document summarizes various topics relating to Earth's seasons, phases of the moon, eclipses, and tides. It explains that Earth's rotation causes day and night, while its revolution around the sun causes years. It describes how the tilt of the Earth on its axis causes seasons. It also discusses the phases of the moon and how they are caused by the relative positions of the Earth, moon, and sun. Lunar and solar eclipses occur when the moon passes between the Earth and sun. Tides are caused by the gravitational pull of the moon and sun on Earth's oceans.
Maritime tropical air masses form over warm waters and bring warm, moist air into parts of the United States. Continental polar air masses form over snow-covered northern Canada and bring cold, dry air into central and eastern portions of the country. When warm and cold air masses meet, fronts are formed. Cold fronts have steep slopes that can produce heavy precipitation like thunderstorms and hail, while warm fronts have more gentle slopes and cause lighter, longer-lasting precipitation from nimbostratus clouds. Occluded fronts occur when a cold front catches up to a warm front.
The document discusses various topics related to weather and climate, including:
1. It defines weather as atmospheric conditions in a specific place and time, while climate describes average weather conditions over many years.
2. It describes several elements that determine weather such as temperature, humidity, atmospheric pressure, wind, and cloud formation.
3. It explains weather phenomena like air masses, fronts, precipitation types, tropical cyclones, monsoon winds, and instruments used to measure weather.
4. It briefly mentions climate change topics like El Niño and the greenhouse effect.
Climate is the average weather conditions in an area over a long period of time, whereas weather is the short term conditions. There are several major climate classifications including tropical, dry, and temperate. Tropical climates are near the equator and have high temperatures year-round. Dry climates have little rainfall throughout the year. Temperate climates experience distinct seasons with warm summers and cold winters. Specific climate zones were also discussed such as savanna, cold snowy, and polar climates.
This document provides an overview of key concepts in geography. It discusses how geography allows examination of global patterns and changes. The five themes of geography are then introduced: location, place, region, movement, and human-environment interaction. Several lessons cover different geographic concepts in detail, such as the study of earth's layers and landforms, plate tectonics, and processes that change the earth's surface like weathering and erosion. Geographic tools and how geography can be used to understand various topics are also mentioned.
This is a presentation onEngineering Geology.
It contains-
>>Meaning
>>Definition
>>Objective
>>Scope in Construction;Water Resource Developement;Town and Regional Planning.
>>Age Of Earth.
---------------------------------------------------------------------------------------------------------------------------
Tropical revolving storms, also known as tropical cyclones, form over warm ocean waters and have a circular wind pattern that rotates counter-clockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere. They develop from tropical disturbances and depressions and can intensify into tropical storms or hurricanes/typhoons depending on wind speeds and location. Tropical storms typically form west of continents in tropical regions between 5 degrees north and south latitude from June to November and can cause significant damage due to strong winds and heavy rain.
The document discusses key concepts about weather including the four main atmospheric variables that influence weather: temperature, humidity, air pressure, and wind. It defines these variables and explains how they interact with and influence one another. For example, it describes how hot air is less dense than cold air and how moisture in the air can cause pressure to decrease. The document also covers cloud formation, precipitation, and other weather phenomena like wind.
This document discusses factors that influence climate, including temperature and rainfall. It describes how latitude affects average yearly temperature, with warmer temperatures near the equator and cooler temperatures nearer the poles. Altitude and proximity to water also impact temperature, with cooler temperatures at higher elevations and nearer coastal areas. Rainfall patterns are influenced by global wind belts, with more rain occurring near the equator and less in subtropical zones. Mountains can induce orographic precipitation on their windward sides. Specific climate phenomena like El Niño and lake effect snow are also summarized.
The Earth's Atmosphere Atmospheric Layers.pptssuserb1fbae
The document describes the four main layers of Earth's atmosphere - the troposphere, stratosphere, mesosphere, and thermosphere. It provides details on the temperature and characteristics of each layer, including that the troposphere is where weather occurs and temperatures decrease with height, the stratosphere temperatures increase due to ozone, the mesosphere temperatures decrease with protective properties, and the thermosphere has increasing temperatures and is where the northern lights and space shuttles orbit occur.
The document provides information about Mars' orbit, rotation, atmosphere and temperature. It then lists past Mars orbiters and landers/rovers. It discusses various geological features of Mars including volcanoes such as Olympus Mons, calderas, lava tubes, rift basins, and Valles Marinaris. Finally, it provides evidence that Mars once had an active hydrologic system through features such as drainage networks, springs, rivers, glaciers and oceans.
The document discusses the difference between climate and weather and identifies five main factors that affect climate: distance from the equator, distance from the sea, rainfall, wind direction, and altitude. It provides examples of how each factor influences temperature, such as coastal areas generally being cooler than inland areas due to the moderating effect of the oceans. Places closer to the equator are hotter and receive more rainfall, while polar regions are extremely cold. Higher altitude locations are cooler due to lower temperatures at increased elevations.
This document discusses air masses and fronts. It defines air masses as large bodies of air that extend thousands of kilometers and have uniform temperature and humidity. Air masses form over source regions and are classified as either tropical or polar, and continental or maritime. Fronts occur at the boundary between differing air masses and can be cold, warm, stationary or occluded fronts. Each front type brings characteristic weather conditions from rain to thunderstorms as the warmer air is displaced.
The document discusses weather maps and how they are used to predict weather conditions. It provides information on several key topics:
- The atmosphere helps regulate Earth's temperature and creates weather through the movement of air masses. Weather maps show current conditions.
- Weather is influenced by properties like temperature, humidity and pressure. Maps depict systems like cold fronts, warm fronts and stationary fronts to understand weather changes.
- High and low pressure areas circulate clockwise and counterclockwise respectively, affecting wind patterns and whether conditions will be clear or stormy. Weather maps are interpreted to forecast upcoming weather.
The document defines key map terminology including location, maps, globes, hemispheres, poles, the equator, prime meridian, lines of longitude and latitude, compasses, compass roses, directions, distance, elevation, grids, scales, symbols and sources. Maps are drawings that provide information about features of an area using these geographic representations and conventions.
Air masses are large bodies of air that maintain consistent temperatures and moisture levels as they move across regions. They are classified by their source location and surface, resulting in four main types: continental polar, continental tropical, maritime polar, and maritime tropical. When two air masses meet, fronts form along the boundary which can cause precipitation. The main front types are warm, cold, stationary, and occluded fronts, which differ based on the advancing air mass temperature and resulting weather impacts.
The document defines weather elements and the factors that influence them. It states that temperature depends on hours of sun, latitude, altitude, distance from the ocean, and relief. It explains that air pressure decreases with height and that high pressure causes sunny weather while low pressure causes storms. Humidity depends on temperature, and wind is caused by the movement of air masses from colder to warmer areas. Finally, it indicates that precipitation forms as water evaporates and rises into clouds, then falls as rain, snow, or hail, with more precipitation closer to the equator, sea, or mountains.
This document discusses the field of geology. It provides definitions and examples of key topics in geology, including the study of Earth materials and processes, as well as the history and evolution of the planet. Important figures in the field like Charles Bonnet and Reinhard Mack are mentioned. The document also outlines related fields and required education to become a geologist, noting they study applied science and work to understand Earth processes, locate resources, and advise on development and construction projects.
The document summarizes various topics relating to Earth's seasons, phases of the moon, eclipses, and tides. It explains that Earth's rotation causes day and night, while its revolution around the sun causes years. It describes how the tilt of the Earth on its axis causes seasons. It also discusses the phases of the moon and how they are caused by the relative positions of the Earth, moon, and sun. Lunar and solar eclipses occur when the moon passes between the Earth and sun. Tides are caused by the gravitational pull of the moon and sun on Earth's oceans.
Maritime tropical air masses form over warm waters and bring warm, moist air into parts of the United States. Continental polar air masses form over snow-covered northern Canada and bring cold, dry air into central and eastern portions of the country. When warm and cold air masses meet, fronts are formed. Cold fronts have steep slopes that can produce heavy precipitation like thunderstorms and hail, while warm fronts have more gentle slopes and cause lighter, longer-lasting precipitation from nimbostratus clouds. Occluded fronts occur when a cold front catches up to a warm front.
The document discusses various topics related to weather and climate, including:
1. It defines weather as atmospheric conditions in a specific place and time, while climate describes average weather conditions over many years.
2. It describes several elements that determine weather such as temperature, humidity, atmospheric pressure, wind, and cloud formation.
3. It explains weather phenomena like air masses, fronts, precipitation types, tropical cyclones, monsoon winds, and instruments used to measure weather.
4. It briefly mentions climate change topics like El Niño and the greenhouse effect.
Climate is the average weather conditions in an area over a long period of time, whereas weather is the short term conditions. There are several major climate classifications including tropical, dry, and temperate. Tropical climates are near the equator and have high temperatures year-round. Dry climates have little rainfall throughout the year. Temperate climates experience distinct seasons with warm summers and cold winters. Specific climate zones were also discussed such as savanna, cold snowy, and polar climates.
This document provides an overview of key concepts in geography. It discusses how geography allows examination of global patterns and changes. The five themes of geography are then introduced: location, place, region, movement, and human-environment interaction. Several lessons cover different geographic concepts in detail, such as the study of earth's layers and landforms, plate tectonics, and processes that change the earth's surface like weathering and erosion. Geographic tools and how geography can be used to understand various topics are also mentioned.
This is a presentation onEngineering Geology.
It contains-
>>Meaning
>>Definition
>>Objective
>>Scope in Construction;Water Resource Developement;Town and Regional Planning.
>>Age Of Earth.
---------------------------------------------------------------------------------------------------------------------------
Tropical revolving storms, also known as tropical cyclones, form over warm ocean waters and have a circular wind pattern that rotates counter-clockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere. They develop from tropical disturbances and depressions and can intensify into tropical storms or hurricanes/typhoons depending on wind speeds and location. Tropical storms typically form west of continents in tropical regions between 5 degrees north and south latitude from June to November and can cause significant damage due to strong winds and heavy rain.
The document discusses key concepts about weather including the four main atmospheric variables that influence weather: temperature, humidity, air pressure, and wind. It defines these variables and explains how they interact with and influence one another. For example, it describes how hot air is less dense than cold air and how moisture in the air can cause pressure to decrease. The document also covers cloud formation, precipitation, and other weather phenomena like wind.
This document discusses factors that influence climate, including temperature and rainfall. It describes how latitude affects average yearly temperature, with warmer temperatures near the equator and cooler temperatures nearer the poles. Altitude and proximity to water also impact temperature, with cooler temperatures at higher elevations and nearer coastal areas. Rainfall patterns are influenced by global wind belts, with more rain occurring near the equator and less in subtropical zones. Mountains can induce orographic precipitation on their windward sides. Specific climate phenomena like El Niño and lake effect snow are also summarized.
The Earth's Atmosphere Atmospheric Layers.pptssuserb1fbae
The document describes the four main layers of Earth's atmosphere - the troposphere, stratosphere, mesosphere, and thermosphere. It provides details on the temperature and characteristics of each layer, including that the troposphere is where weather occurs and temperatures decrease with height, the stratosphere temperatures increase due to ozone, the mesosphere temperatures decrease with protective properties, and the thermosphere has increasing temperatures and is where the northern lights and space shuttles orbit occur.
The document provides information about Mars' orbit, rotation, atmosphere and temperature. It then lists past Mars orbiters and landers/rovers. It discusses various geological features of Mars including volcanoes such as Olympus Mons, calderas, lava tubes, rift basins, and Valles Marinaris. Finally, it provides evidence that Mars once had an active hydrologic system through features such as drainage networks, springs, rivers, glaciers and oceans.
The document discusses the difference between climate and weather and identifies five main factors that affect climate: distance from the equator, distance from the sea, rainfall, wind direction, and altitude. It provides examples of how each factor influences temperature, such as coastal areas generally being cooler than inland areas due to the moderating effect of the oceans. Places closer to the equator are hotter and receive more rainfall, while polar regions are extremely cold. Higher altitude locations are cooler due to lower temperatures at increased elevations.
This document discusses air masses and fronts. It defines air masses as large bodies of air that extend thousands of kilometers and have uniform temperature and humidity. Air masses form over source regions and are classified as either tropical or polar, and continental or maritime. Fronts occur at the boundary between differing air masses and can be cold, warm, stationary or occluded fronts. Each front type brings characteristic weather conditions from rain to thunderstorms as the warmer air is displaced.
The document discusses weather maps and how they are used to predict weather conditions. It provides information on several key topics:
- The atmosphere helps regulate Earth's temperature and creates weather through the movement of air masses. Weather maps show current conditions.
- Weather is influenced by properties like temperature, humidity and pressure. Maps depict systems like cold fronts, warm fronts and stationary fronts to understand weather changes.
- High and low pressure areas circulate clockwise and counterclockwise respectively, affecting wind patterns and whether conditions will be clear or stormy. Weather maps are interpreted to forecast upcoming weather.
The document defines key map terminology including location, maps, globes, hemispheres, poles, the equator, prime meridian, lines of longitude and latitude, compasses, compass roses, directions, distance, elevation, grids, scales, symbols and sources. Maps are drawings that provide information about features of an area using these geographic representations and conventions.
Air masses are large bodies of air that maintain consistent temperatures and moisture levels as they move across regions. They are classified by their source location and surface, resulting in four main types: continental polar, continental tropical, maritime polar, and maritime tropical. When two air masses meet, fronts form along the boundary which can cause precipitation. The main front types are warm, cold, stationary, and occluded fronts, which differ based on the advancing air mass temperature and resulting weather impacts.
The document defines weather elements and the factors that influence them. It states that temperature depends on hours of sun, latitude, altitude, distance from the ocean, and relief. It explains that air pressure decreases with height and that high pressure causes sunny weather while low pressure causes storms. Humidity depends on temperature, and wind is caused by the movement of air masses from colder to warmer areas. Finally, it indicates that precipitation forms as water evaporates and rises into clouds, then falls as rain, snow, or hail, with more precipitation closer to the equator, sea, or mountains.
8. En uzun paraleldir (40.076 km)
Başlangıç paralelidir.
Dünya’yı kuzey ve güney yarım küreye
ayırır.
Çizgisel hızın en fazla, yerçekiminin en az olduğu yerdir.
Ekvator üzerinde ardışık meridyenler arası uzak 111 km'dir
10:54 8
54. 60° 50° 40° 30° 20° 10° 0° 10° 20° 30° 40° 50° 60° 70°
60°
50°
40°
30°
20°
10°
0°
10°
20°
30°
40°
50°
60°
Yarım
Küreleri
belirlemek
için dikkat
edilmesi
gerekenler
Artış
Yönü
Yukarı
Kuzey
Yarım
Küre
Artış
Yönü
Aşağı
Güney
Yarım
Küre
Artış Yönü Sağa Doğu Yarım KüreArtış Yönü SağaBatı Yarım Küre
10:55 54
55. 60° 50° 40° 30° 20° 10° 0° 10° 20° 30° 40° 50° 60° 70°
60°
50°
40°
30°
20°
10°
0°
10°
20°
30°
40°
50°
60°
C
B
D
A
10°K
50°K
60°B 20°B
10:55 55
57. Aşağıda verilen koordinatlar üzerinde yer alan yerleşim
birimlerini bulunuz.
26° 28° 30° 32° 34° 36° 38°
42°
40°
41° Kuzey 29° Doğu
40° Kuzey 33° Doğu
40° Kuzey 31° Doğu
42° Kuzey 35° Doğu
41° Kuzey 32° Doğu
41° Kuzey 30° Doğu
10:55 57
63. Balıkesir’den(40°k) bir
uçakla 28° doğu
meridyenini izleyerek
Lesoto’ya(30°g)
gitmek istesek.
Uçağın izlediği yol kaç
km. olur?
0
40
30
(40 K+ 30 G) x 111 km=
(70 )x 111 km= 7770 km
10:55 63
64. Ülkemizin en güneyinden geçen paralel ile en kuzeyinden
geçen paralel arası kuşuçuşu yaklaşık olarak kaç km. dir?
(42 K - 36 K) x 111 km= (6 )x 111 km= 666 km
10:55 64
76. Balıkesir’de(28º
doğu) yerel saat
10.40 iken,
Ağrı’da(43º doğu)
yerel saat kaçtır?
28 D0 43 D
Boylam Farkı: 43ºD-28ºD =15º
Zaman Farkı: 15ºx 4’ =60’ = 01.00 saat
Sonuç
10.40 (verilen Saat)
01.00 (zaman farkı)
11.40 (daha doğuda olduğundan
saat ileridir -toplama-)
+
10.40 ?
10:55 76
77. Ankara’da(33º doğu)
yerel saat 11.00 iken,
Balıkesir’de(28º
doğu) yerel saat
kaçtır?
28 D0 33 D
Boylam Farkı: 33ºD-28ºD =5º
Zaman Farkı: 5ºx 4’ = 20’ = 00.20 saat
Sonuç
11.o0 (verilen Saat)
00.20 (zaman farkı)
10.40 (daha batıda olduğundan
saat geridir -çıkarma-)
-
11.00?
10:55 77
78. Balıkesir’de(28º
doğu) yerel saat
10.40
iken, Lizbon’da(Port
ekiz) (9º batı) yerel
saat kaçtır?
9 B 0 28 D
Boylam Farkı: 9ºB+28ºD =37º
Zaman Farkı:37ºx 4’ = 148’ = 02.28 saat
Sonuç
10.40 (verilen Saat)
02.28 (zaman farkı)
08.12 (daha batıda olduğundan
saat geridir -çıkarma-)
-
148’/60’=
10.40?10:55 78
95. Balıkesir(28ºD) kaçıncı saat diliminde yer alır?
+1=2. saat dilimindedir
1 saat dilimi =15ºolduğundan
kalan 7,5 tan büyük olduğundan bölüm +1 artırılır
10:55 95
96. Washington(77ºB) kaçıncı saat diliminde yer alır?
24-5=19. saat dilimindedir
1 saat dilimi =15ºolduğundan
Verilen meridyen batıdaysa sonuç 24’den çıkarılır
10:55 96
106. Bu sebeple dünya üzerinde güneşi en son
gören ülkelerden Samoa’daki 186 bin
kişi, 29 Aralık 2011 Perşembe gecesi uykuya
yatıp 31 Aralık 2011 Cumartesi sabahında
uyandı. Samoa Başbakanı Tuilaepa Sailele
Malielegaoi, kararın Yeni
Zelanda, Avustralya ve Asya ile ticari
ilişkilerde saat farkından ötürü yaşanan
aksamaların en aza indirilmesi amacıyla
verildiğini açıkladı. Ülke, 119 yıl önce
Amerikalı tüccarların girişimi ile tarih
değiştirme çizgisinde taraf değiştirmişti. O
zamandan beri Avustralya’nın 21, Yeni
Zelanda’nın 23 saat gerisinde olan Samoa
bu değişiklik ile Avustralya’nın 3, Yeni
Zelanda’nın 1 saat ilerisinde olacak.
OKUMA
PARÇASI
Ülke ticarette yaşadıkları zorluklar
nedeniyle uluslararası tarih
değiştirme çizgisinin öteki yanına
geçmeye karar verdi.
10:55 106
107. Çorum'da yerel saat 16.15 iken İzmit'te kaç olur?
Güneş hangi boylamda tepe noktasına en erken ulaşır?
26° 28° 30° 32° 34° 36° 38°
42°
40°
10:55 107
108. cümlelerindeki boş bırakılan
yerlere getirilmesi gerekenler
aşağıdakilerden hangisinde doğru
olarak verilmiştir?
I II III
A) K en yakındır N
B) N belirlenemez K
C) M en uzaktır L
D) N en yakındır K
E) L belirlenemez M
Yukarıdaki şekilde 39º Kuzey paraleli
üzerinde yer alan K, L, M ve N
merkezlerinde aynı günde ve aynı anda
güneşin, gökyüzündeki konumu
gösterilmiştir. Buna göre,
Diğerlerine göre en batıda yer alan
merkez……’dir.
Diğerlerine göre K merkezinin başlangıç
meridyenine göre konumu……
Diğerlerine göre güneşin en erken
doğduğu merkez……’dir.
I
II
III
10:55 108
109. 171º Batı Meridyeni üzerinde bulunan
Samoa Bağımsız Devleti’nin başkenti
Apia, ülke meclisinin aldığı kararla;
149º Doğu Meridyeni üzerinde bulunan
Avustralya’nın başkenti Kanberra’nın 21
saat 20 dakika gerisindeyken 2 saat 40
dakika ilerisine geçmiştir.
Yeni yıla en son giren başkent iken
2012’ye ilk giren başkent olmuştur.
Bu bilgilere göre, Samoa Bağımsız
Devleti aşağıdaki kararlardan hangisiyle
yukarıdaki her iki durumu aynı anda
gerçekleştirmiştir?
A) Tarih değiştirme çizgisi olarak
Greenwich’i kabul etme
B) 31 Aralık tarihini Samoa için 21 saat 20
dakika olarak kabul etme
C) Tarih değiştirme çizgisini ülkenin
doğusuna kaydırma
D) Ülkenin batısındaki başka bir kenti
başkent olarak kabul etme
E) 28 gün olan şubat aylarını 29 güne
çıkarma
10:55 109
110. 84. Oscar Ödül Töreni, Greenwich Ortalama
Saat'ine göre 26.02.2012 tarihinde 8. saat dilimini
kullanan Los Angeles kentinde yapılmıştır. Tören
Los Angeles saatine göre 19.30’da başlamış ve
Türkiye’de de televizyon kanalları aracılığıyla canlı
olarak yayınlanmıştır. Törene katılan bir Türk
yönetmen, aynı gün Los Angeles saati ile 23.30’da
uçağa binmiş ve uçakta kendisine uçuş bilgilerini
içeren bir broşür verilmiştir. Broşürde Los
Angeles ve İstanbul arasındaki uçuş rotası aşağıda
verilen haritadaki gibi yay şeklinde gösterilmiştir.
13 saat süren kıtalar arası bir uçuşun ardından
uçak İstanbul Atatürk Havalimanı’na inmiştir.
Uçak 3 saatlik bir aktarma molasının ardından
yeni yolcuları ile birlikte Türkiye’nin ulusal
saatinden 4 saat ileri olan bir başka kente
uçmuştur.
Yalnızca yukarıdaki parçada verilen bilgiler göz
önüne alındığında,
I. Oscar Ödül Töreni’nin canlı yayınla Türkiye’den
izlenmeye başlandığı tarih ve saat,
II. Los Angeles ve İstanbul arasında uçuş yapan uçağın
Türkiye saati ile İstanbul Atatürk Havalimanı’na indiği
tarih ve saat
aşağıdakilerin hangisinde doğru sırada verilmiştir?
A) 27.02. 2012 saat 05.30 27.02. 2012 saat 12.30
B) 28.02. 2012 saat 06.30 27.02. 2012 saat 12.30
C) 27.02. 2012 saat 05.30 28.02. 2012 saat 18.30
D) 28.02. 2012 saat 06.30 28.02. 2012 saat 12.30
E) 27.02. 2012 saat 05.30 27.02. 2012 saat 22.30
Soruyu aşağıda verilen parçaya göre cevaplayınız.
10:55 110
111. 84. Oscar Ödül Töreni, Greenwich Ortalama
Saat'ine göre 26.02.2012 tarihinde 8. saat
dilimini kullanan Los Angeles kentinde
yapılmıştır. Tören Los Angeles saatine göre
19.30’da başlamış ve Türkiye’de de televizyon
kanalları aracılığıyla canlı olarak
yayınlanmıştır. Törene katılan bir Türk
yönetmen, aynı gün Los Angeles saati ile
23.30’da uçağa binmiş ve uçakta kendisine
uçuş bilgilerini içeren bir broşür verilmiştir.
Broşürde Los Angeles ve İstanbul arasındaki
uçuş rotası aşağıda verilen haritadaki gibi yay
şeklinde gösterilmiştir. 13 saat süren kıtalar
arası bir uçuşun ardından uçak İstanbul
Atatürk Havalimanı’na inmiştir. Uçak 3 saatlik
bir aktarma molasının ardından yeni yolcuları
ile birlikte Türkiye’nin ulusal saatinden 4 saat
ileri olan bir başka kente uçmuştur.
İstanbul’dan kalkan uçak, hangi saat
dilimini kullanan kente uçmuştur?
A) +6. saat dilimini
B) +7. saat dilimini
C) +8. saat dilimini
D) +9. saat dilimini
E) +10. saat dilimini
Soruyu aşağıda verilen parçaya göre cevaplayınız.
10:55 111
112. Yukarıdaki Dünya haritasında K, L, M
ve N merkezleriyle bu merkezlerden
geçen meridyen değerleri verilmiştir.
Buna göre bu merkezlerle ilgili olarak
aşağıda verilen bilgilerden hangisi
yanlıştır?
A) K - L ile M - N merkezleri
arasındaki yerel saat farkı eşittir.
B) Yerel saati en ileri olan merkez
L’dir.
C) Gurup ve tan sürelerinin en
uzun olduğu merkez N’dir.
D) K, Başlangıç Meridyeni’ne göre
Batı Yarım Küre’dedir.
E) Güneşin en geç doğduğu merkez
M’dir.
10:55 112
113. Türkiye’de, enerji tasarrufu sağlamak amacıyla yaz ve kış saati uygulanmaktadır. Bu
uygulama kapsamında yılın yaklaşık beş aylık döneminde 30º Doğu meridyeninin, diğer
dönemde ise 45º Doğu meridyeninin yerel saati ulusal saat olarak kullanılmaktadır.
Buna göre, 45º Doğu meridyeninin yerel saatinin ulusal saat olarak kullanıldığı
dönemde, Türkiye’ de, aşağıdakilerden hangisi yaşanmaz
A) Gündüz-gece süresinin eşit olduğu gün
B) Güneş ışınlarının dike en yakın açıyla geldiği gün
C) En sıcak ay
D) Öğle vakti en uzun gölge boyu
E) En uzun gündüz
10:55 113
114. Ekvatorun 4500 km kuzeyinde
bulunan X noktasının yerel saati
başlangıç meridyeninin yerel
saatinden 120 dakika ileridir.
Yalnızca yukarıdaki bilgiler
kullanılarak X noktasının,
I. matematik konumu,
II. ortalama yükseltisi,
III. bulunduğu saat dilimi,
IV. yıllık yağış tutarı
özelliklerinden hangilerine
ulaşılabilir?
A) I ve II
B) I ve III
C) II ve III
D) II ve IV
E) III ve IV
10:55 114
115. KOMİSYON, Coğrafya 9, MEB Yayınevi, İstanbul 2010
ŞAHİN, Cemalettin, Coğrafya 9, Lider Yayıncılık, Ankara, 2011
BARANAYDIN, Mehmet, Coğrafya 9, Lider Yayıncılık, Ankara, 2012
KOMİSYON, Coğrafya 9, Coşku Yayınları, İzmir 2011
ZOR, Mehmet; İLKAY, Kemal; KIZIL, Tülay; 9. Sınıf Coğrafya, Ekip Yayınları, Ankara 2011
ABAY, Cumhur, 9. Sınıf Coğrafya, Esen Yayınları, Ankara 2010
KÖROĞLU, S., KÖROĞLU, M., 9. Sınıf Coğrafya, Esen Yayınları, Ankara 2010
ATEŞ, Doğu, Coğrafya 9, Ateş Yayıncılık, Ankara, 2012
10:55 115