染雾名师曹其军精讲MBA英语阅读理解的短文 篇一
在名师曹其军的精讲下，MBA英语阅读理解变得更加容易了。曹其军老师以其丰富的教学经验和深厚的学术背景，为学生们提供了一种全新的学习方法，帮助他们更好地理解和应用英语阅读理解技巧。
对于MBA学生来说，英语阅读理解是一项重要的技能。在商业领域中，大量的信息和数据需要通过阅读来获取和分析。然而，由于时间和学习压力的限制，许多学生往往只能匆匆浏览文章，导致对文章的理解和分析能力不足。曹其军老师通过他的教学方法，帮助学生们提高阅读速度和理解能力，使他们能够更好地应对MBA英语阅读理解考试。
曹其军老师强调了对文章结构和主旨的理解。他教导学生们如何通过快速扫描文章的开头和结尾，抓住文章的主题和重点。此外，他还教授了一些常见的阅读技巧，如查找关键词、理解上下文以及推理判断等。这些技巧帮助学生们更好地理解文章的含义，并能够准确回答问题。
除了技巧和方法，曹其军老师还注重培养学生们的阅读兴趣和积累词汇量。他鼓励学生们多读英文材料，包括新闻、杂志和学术文章，以提高他们的阅读速度和理解能力。同时，他还推荐了一些经典的英文小说和商业书籍，帮助学生们拓宽视野，增加词汇量。
通过曹其军老师的指导和激励，学生们在MBA英语阅读理解方面取得了显著的进步。他们的阅读速度和理解能力得到了提高，能够更好地应对考试和实际工作中的阅读任务。曹其军老师的教学方法不仅仅是教给学生们解题技巧，更重要的是培养了他们的独立思考和批判性思维能力，使他们成为了真正的MBA英语阅读理解专家。
名师曹其军精讲MBA英语阅读理解的短文 篇二
曹其军老师是一位备受推崇的MBA英语阅读理解教师，他的教学方法让学生们受益匪浅。在他的指导下，学生们不仅提高了阅读理解能力，还培养了批判性思维和独立思考的能力。
曹其军老师的教学方法注重实践和互动。他鼓励学生们积极参与课堂讨论，提出自己的观点和见解。通过与老师和同学们的互动，学生们能够更好地理解文章的含义，并学会运用正确的表达方式来表达自己的观点。这种互动式教学方法帮助学生们在阅读理解方面取得了更大的进步。
曹其军老师还强调了词汇的重要性。他教授学生们如何通过词根、前缀和后缀来推测词义，以及如何运用上下文来理解词语的意思。同时，他还鼓励学生们背诵和运用常用的商业词汇和短语，以提高他们的词汇量和阅读能力。
除了词汇和阅读理解技巧，曹其军老师还注重学生们的思维训练。他教授学生们如何分析和评估文章的逻辑结构和论证方式，以及如何对文章中的观点和论据进行批判性思考。通过这种思维训练，学生们能够更好地理解和评价文章，并能够在实际工作中应用这些技能。
在曹其军老师的精心指导下，学生们的MBA英语阅读理解能力得到了显著提升。他们能够更快速地阅读和理解文章，准确回答问题，并能够独立思考和分析复杂的商业问题。曹其军老师的教学方法不仅仅是为了帮助学生们在考试中取得好成绩，更重要的是培养他们的终身学习能力和职业发展能力。
名师曹其军精讲MBA英语阅读理解的短文 篇三
名师曹其军精讲MBA英语阅读理解的短文
Text 1
The recent, apparently successful, prediction by mathematical models of an appearance of El Nino-the warm ocean current that periodically develops along the Pacific coast of South America-has excited researchers. Jacob Berknes pointed out over 20 years ago how winds might create either abnormally warm or abnormally cold water in the eastern equatorial Pacific.
1) Nevertheless, un
2) It has long been known that during an El Nino, two conditions exist: A) unusually warm water extends along the eastern Pacific, principally along the coasts of Ecuador and Peru, and B) winds blow from the west into the warmer air rising over the warm water in the east. These winds tend to create a feedback mechanism by driving the warmer surface water into "piles" that block the normal rising of deeper, cold water in the east and further warm the eastern water, thus strengthening the wind. The contribution of the model is to show that the winds of an El Nino, which raise sea level in the east, simultaneously send a signal to the west lowering sea level. According to the model, that signal is generated as a negative Rossby wave, a wave of depressed sea level, that moves westward parallel to the equator at 25 to 85 kilometers per day.
3) Taking months to travel across the Pacific, Rossby waves march to the western boundary of the Pacific basin, which is modeled as a smooth wall but in reality consists of quite irregular island chains, such as the Philippines and Indonesia.
When the waves meet the western boundary, they are reflected, and the model predicts that Rossby waves will be broken into numerous coastal Kelvin waves carrying the same negative sealevel signal. These eventually shoot toward the equator, and then head eastward along the equator propelled by the rotation of the Earth at a speed of about 250 kilometers per day. When Kelvin waves of sufficient amplitude arrive from the western Pacific, their negative sealevel signal overcomes the feedback mechanism tending to raise the sea level, and they begin to drive the system into the opposite cold mode. This produces a gradual shift in winds, one that will eventually send Rossby waves westward, waves that will eventually return as cold cycleending Kelvin waves, beginning another warming cycle.
1．It was not until the appearance of mathematical models that
A．El Nino was defined as unusually warm or cold ocean currents.
B．the occurrences of E1 Nino were inaccurately predicted.
C．the cause of regular El Nino was correctly interpreted.
D．the shifts in ocean currents were linked to atmospheric conditions.
2．Which of the following best describes the organization of the first paragraph?
A．A model is described and its value assessed.
B．A result is reported and its importance explained.
C．A phenomenon is noted and its significance debated.
D．A hypothesis is introduced and contrary evidence presented.
3．According to the model, which of the following signals the disappearance of an E1 Nino?
A．The arrival in the eastern Pacific of negative Kelvin waves.
B．A shift in the direction of the winds produced by an antiEl Nino.
C．The reflection of Kelvin waves reaching the eastern border of the Pacific.
D．An increase in the speed at which negative Rossby waves cross the Pacific.
4．Which of the following would most seriously undermine the validity of the model?
A．El Nino extends much farther along the coasts of Ecuador and Peru during some years.
B．The rising of cold water in the eastern Pacific depends on the local characters.
C．The variations in the time for Rossby waves to cross the Pacific rely on the wind power.
D．The Pacific irregular western coast hinders most Kelvin waves from heading eastward.
5．The primary purpose of the text as a whole is to
A．introduce a new explanation of physical phenomenon.
B．explain the difference between two natural phenomena.
C．illustrate the limits of applying mathematics to complex problems.
D．clarify the distinction between an old explanation and a new model.
