[外语类试卷]大学英语四级(阅读)练习试卷2及答案与解析.doc
《[外语类试卷]大学英语四级(阅读)练习试卷2及答案与解析.doc》由会员分享,可在线阅读,更多相关《[外语类试卷]大学英语四级(阅读)练习试卷2及答案与解析.doc(15页珍藏版)》请在麦多课文档分享上搜索。
1、大学英语四级(阅读)练习试卷 2及答案与解析 一、 Part II Reading Comprehension (Skimming and Scanning) (15 minutes) Directions: In this part, you will have 15 minutes to go over the passage quickly and answer the questions attached to the passage. For questions 1-7, mark: Y (for YES) if the statement agrees with the infor
2、mation given in the passage; N (for NO) if the statement contradicts the information given in the passage; NG (for NOT GIVEN) if the information is not given in the passage. 0 Types of Climate Climate is the combination of temperature, moisture, wind, and sunshine at a place over a period of many ye
3、ars. Weather is made up of atmospheric conditions during a few hours or days. The weather may be rainy on a certain day. But that place may usually have a warm, dry, sunny climate. We learn about the climate of a place by studying its temperature, moisture, wind, and sunshine from season to season a
4、nd year to year. Temperature and the amount of rainfall are the two most important elements of climate. Others are humidity (air moisture), cloudiness, fog, sunshine, wind, storms, and air pressure. There are many different types of climate on earth. Climates of the world can be classified according
5、 to their latitudes and the plants that grow there. Different kinds of plants need different amounts of heat and moisture for growth. The vegetation of a region tells us about temperature and rainfall conditions over a long period of time. Tropical Climates Tropical climates are found in regions bet
6、ween 35N and 35S latitude. In the tropical rain forest (nearest the equator) conditions are warm and rainy all year long, and there is a thick cover of trees. Places farther north and south of the equator have a tropical wet-and-dry climate. There the forests are not so dense, and many trees lose th
7、eir leaves in the dry season. Along 23.5N and 23.5S latitude there are vast regions of tropical desert climate, where very little vegetation can grow. Subtropical Climates Subtropical climates are usually found between 30 and 40 North and South latitudes. The subtropical western coasts of the contin
8、ents have a Mediterranean climate. Summers are hot and dry; winters are mild and wet. On the subtropical eastern coasts of continents the climate is humid subtropical. Summers are hot, and winters are mild. There is enough rainfall in all seasons for forests. Mid-latitude Climate Mid-latitude climat
9、es occur between 40 and 60 NS latitudes. Strong westerly winds blow in the mid-latitudes. The climate of the west coast of North America is mild and rainy most of the year. It helps the growth of fine timber forests. Some places in the mid-latitudes do not receive moisture because of mountain barrie
10、rs or their great distances from the oceans. Humid continental climates cover large mid-latitude area in eastern parts of the continents. They are forest climates with cold winters and warm summers. Most of the rainfall comes in the summer. High-latitude Climates High-latitude climates occur from 60
11、 to the poles, North and South. In the high latitudes it is very cold in winter and cool in summer. The short summers are warm enough for forests of evergreen trees. Greenland and Antarctica have a polar climate, where great ice caps exist because of year-round freezing. High-altitude Climates Highl
12、and climates are cooler than the surrounding lowlands because of the effects of altitude. Highland climates are found on the high mountains of the world, even on the equator. In the tropics and mid-latitudes different kinds of vegetation grow in zones up the slopes of mountains to the permanent snow
13、fields. The Causes of Different Climates The differences in the climate from place to place are caused by climate controls. The major climate controls are latitude, altitude, land and water bodies, ocean currents, and storm centers. Latitudes make climates colder toward the north and south poles (hi
14、gh latitudes) than at the tropics near the equator (low altitudes). Low-latitude regions remain warm throughout the year. At higher latitudes there are greater differences between winter and summer temperatures. Altitude affects climate by lowering temperatures as the height above sea level increase
15、s. At high altitudes the air is less dense and does not absorb and hold as much heat. On the average, the temperature drops about 2 degrees Celsius for each 300 meters of altitude (about 3.5 degrees Fahrenheit for each 1,000 feet). Thus snow can remain on mountainlike Fujiyama when nearby lowlands a
16、re warm. Land and water bodies influence climate. Land warms up rapidly in summer and cools off rapidly in winter. But large bodies of water change temperature slowly, with the seasons. Mid-continental places in middle and high latitudes have a continental climate. Summers are warm and winter cold.
17、Island and seacoasts usually have milder winters and cooler summers because of the water surfaces nearby. Ocean currents affect climate in many parts of the world. Some currents carry warm water to cool regions; others carry cool water to warm regions. The Labrador Current is cold. The Gulf Stream i
18、s a warm ocean current. It carries warm water from the tropical Atlantic toward the coasts of northwestern Europe. As a result, winters in the British Isles and in Westam Europe are warmer than other regions in the same latitudes. Winds carry heat and moisture and therefore affect climate. Winds tha
19、t come from lands in high latitudes are cold and dry. Some winds change direction with the seasons. In southern Asia winds called monsoons are dry and cool in the winter, when they blow from the land. In the summer they blow from the ocean and produce heavy rainfall. Climate and the Water Cycle Wate
20、r enters the atmosphere by evaporation from land and water surfaces. Winds carry water vapor and clouds to other areas. There the moisture is returned to the earth in the form of rain or snow. Much of the water falls on land and runs off to the sea in rivers. But some moisture enters soil. It helps
21、growing plants or builds up the groundwater supply. The constant movement of water from land to sea to air and back again is called the water cycle. The amount of water available for farming, industry, and many other uses differs from one climate to another. People try to overcome these differences
22、by using water resources wisely. The water cycle can be controlled in part for a short time by storing water in reservoirs, irrigating land, draining wetlands, or pumping water from wells. Climate and People Climate influences peoples comfort, well-being, and activities in many ways. Most people do
23、not work as well in a hot, moist climate as in a cooler, drier climate. Extremely high or low temperatures are uncomfortable. Certain diseases are more common in some climates than in others. It is difficult to determine what is the best or ideal climate for human beings. People differ in their reac
24、tions to climate because of their individual characteristics and attitudes. The amount and kind of clothing people wear is determined partly by climate. Clothing for cold climates gives protection against wind and cold. Less clothing is needed in warm climates. There are many types of special clothi
- 1.请仔细阅读文档,确保文档完整性,对于不预览、不比对内容而直接下载带来的问题本站不予受理。
- 2.下载的文档,不会出现我们的网址水印。
- 3、该文档所得收入(下载+内容+预览)归上传者、原创作者;如果您是本文档原作者,请点此认领!既往收益都归您。
下载文档到电脑,查找使用更方便
2000 积分 0人已下载
下载 | 加入VIP,交流精品资源 |
- 配套讲稿:
如PPT文件的首页显示word图标,表示该PPT已包含配套word讲稿。双击word图标可打开word文档。
- 特殊限制:
部分文档作品中含有的国旗、国徽等图片,仅作为作品整体效果示例展示,禁止商用。设计者仅对作品中独创性部分享有著作权。
- 关 键 词:
- 外语类 试卷 大学 英语四 阅读 练习 答案 解析 DOC