Leadership Essay Example | Topics and Well Written Essays - 1500 words - 5

Leadership - Essay Example In light of this she is still to give recommendations to the senior management on where the ‘additional’ officers will be deployed. Kathy’s team members are aware of this move and as a result they are distressed: an aspect that as earlier stated is affecting their work performance a great deal. The main aim for Kathy is to ensure that the team members’ work performance is within acceptable levels especially during this transition period. This paper will use a leadership approach to come up with how best to solve the dilemma Kathy has. Leaders are supposed to always be able to ensure that things are done through influencing others. For a leadership process to be complete there has to be the leader followed by the task to handle and lastly the ones being led: termed as followers. Â  According to Stojkovic et al. (2008) a leader has to be visionary, good behaviour, be charismatic, have a trait and above all manifest a form of leadership style. Leaders in daily duties are faced with situations that force them to act in a certain manner. Situational variables dictate what to be done and at what time. Some of the situational factors that are of importance to consider are the style the leader opt, followers’ behaviours and capabilities among others. Contingency theories therefore play a key role in guiding leaders on how to lead more so depending on situational analysis. Contingency theories indicate that there is no particular style of leadership that can apply to any given situation. This clearly stipulates th at leaders’ approaches to a demanding situation will depend hugely on the dynamics that the situation poses. The same case applies to leaders themselves whereby if one fails to change with a situation then the chances of success in a volatile environment are slim. Decision making process is complex and can be made simple by a leader’s ability to appreciate change in the environment and by approaching

Generation X expatriates Essay Example | Topics and Well Written Essays - 2250 words

Generation X expatriates - Essay Example ter displays the outcomes in a statistical measurement fashion, with some qualitative emphasis by way of a summary of the findings from the key informants, describing significant opinions and comments. The general analytical approach was used to analyse the interviews and descriptive statistical analysis was undertaken to identify survey outcomes. This approach has contributed to some noteworthy results on the topic of The Hidden Depths of Global Ambition. When the question was asked about the number of employees worked in the organizations of participants so there were 36% respondents who respond that there are over 1500 employee in their organization, 11% respond less than 50 employees they had in their organizations. When the question were asked to the respondents regarding their studies in abroad then there were 68% respondents who respond that they studied abroad and there were 32% respondents who respond that they didn’t studied abroad. In response of the question regarding time spent abroad, there were 41% respondents who respond that they spent about 5+years in abroad, 24% respond 2-5 years, 15% respond 1-2 years and there were 14% respondents who respond that they spent less than 1 year in abroad. When it was asked to the respondents that what motivates them to go abroad, then on the option of career advancement there were 67% respondents agreed that the career advancement motivates them to go abroad, 14% disagreed with it. When it was asked to the respondents that is the seeking better future is an important factor behind their abroad visit, 68% respondents agreed with this statement and there were 13% respondents disagreed with this statement. When it was asked to the respondents who didn’t go abroad that is the reason behind not going abroad was lack of job opportunities then from the 6 respondents there were 2 respondents disagreed with this statement and 4 respondents agreed with it. From 6 respondents there were 2 respondents respond

Do Endogenic Processes Influence Global Climate Systems Environmental Sciences Essay

Do Endogenic Processes Influence Global Climate Systems Environmental Sciences Essay All processes that take place inside  Earth  (and other  planets) are considered endogenous. They make the  continents  migrate, push the  mountains  up, and trigger  earthquakes  and  volcanism. Endogenous processes are driven by the warmth that is produced in the core of Earth by  radioactivity  and  gravity. The geography and movement of tectonic plates is a key influence on global climate as it determines the form of the ocean basins, Patterns of heat ransfer in the oceans, large scale atmospheric circulation and the geometry of mountain chains. The movement and geometry of the lithospheric plates is a key long term influence on global climate and hea transfer and plae movements can be both vertical e.g the formation of the Himalayas and the Tibetan plateau or horizontal e.g sea floor spreading or the closing of the panama seaway and the development of the north atlantic gulf stream. Internal energy drives endogenic processes such as plate tectonics, volcanic activity, seismicity. The geography of the tectonic plates is a key influence on a global climate, this influences: the form and size of the ocean basins and land masses, patterns of heat transfer in the oceans thermohaline circulation, large scale atmospheric circulation and vertical heat exchange, the location and elevation of mountain chains and plateaus, the amount of elevated crust. The formation of the Himalayas and the Tibetan plateau that began 52 to 44ma key events that led to a step change in the climate system and long term global cooling. Horizontal crustal movement the closing of the panama seaway around 4 ma and the development of the north atlantic gulf stream taking warm water to higher latitudes a key factor in the formation of ice sheets in the northern hemisphere. The closing of the panama seaway around 4ma and the development of the north atlantic gulf stream taking warm water to higher latitudes. The movement and geometry of the lithospheric plates is a key longterm influence on global climate and heat transfer, vertical crustal movements are most rapid at plate boundaries and we will be exploring their potential impact on weathering rates and carbon cycle. Location and elevation of mountain chains and high plateau landscapes across the earths surface is a key influence on climate over a range of timescales. The essay is about the last 65 million years, so the Big Bang theory is not really relevant. You need a nice range of examples to show how endogenic processes can influence global climate (long and short term). We covered some in the lectures (i.e. vertical and horizonatal crustal movements). We did not really look at volcanic processes, but you need to mention them too (short and longterm impacts) we mentioned other controls too (not related to endogenic processes) so you can mention them briefly to round things off. When Mount Pinatubo erupted in the Philippines June 15, 1991, an estimated 20 million tons of sulfur dioxide and ash particles blasted more than 12 miles (20 km) high into the atmosphere. The eruption caused widespread destruction and loss of human life. Gases and solids injected into the stratosphere circled the globe for three weeks. Volcanic eruptions of this magnitude can impact global climate, reducing the amount of solar radiation reaching the Earths surface, lowering temperatures in the troposphere, and changing atmospheric circulation patterns. The extent to which this occurs is an ongoing debate.  Large-scale volcanic activity may last only a few days, but the massive outpouring of gases and ash can influence climate patterns for years. Sulfuric gases convert to sulfate aerosols, sub-micron droplets containing about 75 percent sulfuric acid. Following eruptions, these aerosol particles can linger as long as three to four years in the stratosphere. Major eruptions alter the Earths radiative balance because volcanic aerosol clouds absorb terrestrial radiation, and scatter a significant amount of the incoming solar radiation, an effect known as radiative forcing that can last from two to three years following a volcanic eruption. Volcanic eruptions cause short-term climate changes and contribute to natural climate variability, says Georgiy Stenchikov, a research professor with the Department of Environmental Sciences at Rutgers University. Exploring effects of volcanic eruption allows us to better understand important physical mechanisms in the climate system that are initiated by volcanic forcing. Stenchikov and Professor Alan Robock of Rutgers University with Hans Graf and Ingo Kirchner of the Max Planck Institute for Meteorology performed a series of climate simulations that combined volcanic aerosol observations from the Stratospheric Aerosol and Gas Experiment II (SAGE II) available from the Langley DAAC, with Upper Atmosphere Research Satellite (UARS) data from the Goddard Space Flight Center DAAC. The research team ran a general circulation model developed at the Max Planck Institute with and without Pinatubo aerosols for the two years following the Pinatubo eruption. To study the sensitivity of climate response to sea surface temperature, using data from the NASA Jet Propulsion Laboratory DAAC, they conducted calculations with climatologically mean sea surface temperature, as well as with those observed during particular El Nià ±o and La Nià ±a periods. By comparing the climate simulations from the Pinatubo eruption, with and without aerosols, the researchers found that the climate model calculated a general cooling of the global troposphere, but yielded a clear winter warming pattern of surface air temperature over Northern Hemisphere continents. The temperature of the tropical lower stratosphere increased by 4 Kelvin (4 °C) because of aerosol absorption of terrestrial longwave and solar near-infrared radiation. The model demonstrated that the direct radiative effect of volcanic aerosols causes general stratospheric heating and tropospheric cooling, with a tropospheric warming pattern in the winter. The modeled temperature change is consistent with the temperature anomalies observed after the eruption, Stenchikov says. The pattern of winter warming following the volcanic eruption is practically identical to a pattern of winter surface temperature change caused by global warming. It shows that volcanic aerosols force fundamental climate mechanisms that play an important role in the global change process. This temperature pattern is consistent with the existence of a strong phase of the Arctic Oscillation, a natural pattern of circulation in which atmospheric pressure at polar and middle latitudes fluctuates, bringing higher-than-normal pressure over the polar region and lower-than-normal pressure at about 45 degrees north latitude. It is forced by the aerosol radiative effect, and circulation in winter is stronger than the aerosol radiative cooling that dominates in summer. Man-made, or anthropogenic emissions can make the consequences of volcanic eruptions on the global climate system more severe, Stenchikov says. For instance, chlorofluorocarbons (CFCs) in the atmosphere start a chain of chemical reactions on aerosol surfaces that destroy ozone molecules in the mid-latitude stratosphere, intensifying observed stratospheric ozone depletion. While we have no observations, the 1963 Agung eruption on the island of Bali probably did not deplete ozone as there was little atmospheric chlorine in the stratosphere. In 1991 after the Pinatubo eruption, when the amount of CFCs in the stratosphere increased, the ozone content in the mid-latitudes decreased by 5 percent to 8 percent, affecting highly populated regions, says Stenchikov. NASA and the National Science Foundation have funded Robock and Stenchikov to study the Pinatubo eruption in more detail, and to conduct another model comparison with the volcanic aerosol data set. They plan to combine SAGE II data with available lidar and satellite data from various DAACs to improve their existing data set. By understanding the impact of large volcanic eruptions on Earths climate system in more detail, perhaps scientists will be in a better position to suggest measures to lessen their effects on people and natural resources. Both technological change and economic growth are seen as major determinants of future global energy demand levels, the associated carbon dioxide (CO2) emissions, and global climate impacts Until recently, however, the modelling of energy-economy-climate interactions has largely regarded technological progress as an exogenous process, rather than as endogenous technological change. Energy Economics Volume 24, Issue 1, January 2002, Pages 1-19 a momentary glance at a map of the world today to realise that the disposition of the continents has a marked effect on both local and global climate. Not the least of these effects results from the difference in the thermal properties of land versus ocean a continental region will be colder in winter and warmer in summer than an oceanic region at any given latitude. Moreover mountain belts formed as a consequence of plate tectonic activity dramatically modify rainfall through the effects of  orography   the development of a rain shadow on the leeward side of mountain belts. Global climate is also strongly controlled by ocean currents. For example, northwestern Europe is significantly warmer than other regions at similar latitudes because of the warming effects of the Gulf Stream and North Atlantic Drift. The reversal of oceanic currents in the equatorial Pacific a phenomenon known as El Nià ±o has a far-reaching effect on climate around the Pacific. Ocean currents depend on the geometry of the oceans and this is controlled by plate tectonics. Hence, over geological timescales the movement of plates and continents has a profound effect on the distribution of land masses, mountain ranges and the connectivity of the oceans. As a consequence, plate tectonics has a very direct and fundamental influence on global climate. http://openlearn.open.ac.uk/mod/resource/view.php?id=172207 The climate of modern Antarctica is extreme. Located over the South Pole and in total darkness for six months of the year, the continent is covered by glacial ice to depths in excess of 3 km in places. Yet this has not always been the case. 50 Ma ago, even though Antarctica was in more or less the same position over the pole, the climate was much more temperate there were no glaciers and the continent was covered with lush vegetation and forests. So how did this extreme change come about? The modern climate of Antarctica depends upon its complete isolation from the rest of the planet as a consequence of the Antarctic Circumpolar Current that completely encircles Antarctica and gives rise to the stormy region of the Southern Ocean known as the roaring forties. The onset of this current is related to the opening of seaways between obstructing continents. Antarctica and South America were once joined together as part of Gondwana and were the last parts of this original supercontinent to separate. By reconstructing continental positions from magnetic and other features of the sea floor in this region, geologists have shown that the Drake Passage opened in three phases between 50 Ma and 20 Ma, as illustrated in Figure 32. At 50 Ma there was possibly a shallow seaway between Antarctica and South America, but both continents were moving together. At 34 Ma the seaway was still narrow, but differential movement between the Antarctic and South American Plates created a deeper c hannel between the two continents that began to allow deep ocean water to circulate around the continent. Finally, at 20 Ma there was a major shift in local plate boundaries that allowed the rapid development of a deep-water channel between the two continental masses. The coincidence of the change in motion of the Pacific Plate with changes in plate motions between S. America and Antarctica shows how the motions of all the plates are interconnected a change in the true motion of one plate leads to changes in the true motions of many others. While these plate motions were taking place the effect on Antarctica was profound. By 34 Ma the climate cooled from the temperate conditions that previously existed. This was sufficient for glaciers to begin their advance, and was followed by a period of continued cooling until at about 20 Ma, glaciation was complete. Even though the Drake Passage first opened at 50 Ma it was not until it opened to deep water at 34 Ma that glaciation really took hold Today, the Antarctic Circumpolar Current is the strongest deep ocean current and its strength is responsible for the icehouse climate that grips the planet. The opening of the Drake Passage had both a local and a global effect, initially cooling the climate of Antarctica from temperate to cold and ultimately playing an important role in the change from global greenhouse conditions 50 Ma ago to the global icehouse of today. This example shows how plate tectonics, continental drift and the opening and closing of seaways can have a profound influence on both local and global climate. Throughout the Phanerozoic there were long periods when the Earth was much warmer than today often called a greenhouse climate and other times when it was cold called an icehouse climate. These cycles, like the Wilson cycle, occur over periods of 100 Ma, reflecting the timescale of plate movements and the growth and destruction of oceans. Given the clear link between ocean circulation and climate, and the similar timescales of global climate change and plate motions, it is inescapable that one of the chief controls on long-term changes in the global climate must be plate tectonics. Every two to seven years a climatic disturbance brings floods to California, droughts to Australia, and famine to Africa . Known as El Nino, it is essentially a warming of surface waters in the eastern Pacific near the equator. Although scientists understand the mechanics of El Nino, its origins have yet to be determined. Most believe that the interaction between the atmosphere and the sea somehow generates this climatic disturbance that wreaks havoc upon those regions of the world that lie in its path. But now a new theory on the origins of El Nino has been proposed and, surprisingly, it has very little to do with the atmosphere or the sea. The new theory suggests that the primary mover behind El Nino is hot magma welling up between tectonic plates on the Pacific sea-floor. The upwelling magma heats the overlying waters enough to affect the ocean surface, initiating the cascade of events that brings on the wrath of El Nino. Volcanic Ash Eruptions, like that pictured above, throw tons of ash into the atmosphere, and have short term affects of the climate. If the eruption is potent enough, the ash will stop some of the shortwave radiation coming in from the Sun. This, in turn, will lead to a decrease in the global temperature. The reason for this is that the shortwave radiation that comes in from the Sun and reaches the Earths surface, gets absorbed in the the Earth. About 4 to 6 hours later, the Earth reradiates that energy in the form of longwave radiation. This is where the temperature comes from. So if some of the sunlight is shut off, then this will lead to a decrease the global temperature. With the eruption of Mount Pinatubo in June 1991 (image above), about 22 million tons of ash was thrown into the atmosphere. This was enough to block a fraction of the sunlight from reaching the Earths surface, which cooled the global temperature on Earth by as much as 0.5 degrees C. The most powerful eruption in recorded his tory, the eruption of the Tambora Volcano in Indonesia in April of 1815, threw up so much ash that the global temperature on Earth fell by as much as 3 degrees C. Europe and North America know this time as the year without a summer. The volcanic ash does not keep the temperatures down for a very long period of time geologically speaking, so its impacts are on a short term basis. Rain-Shadow Effect The long term impacts of volcanoes come from a look at simple geography. Volcanoes are gigantic mountains, so their affect on climate is the same as a normal mountain. This leads to the rain-shadow effect (explained in the  Continental Movement  section), which comes into play with volcanoes just as it does with mountain building. Until that volcano can be eroded away, it will continue to have some sort of impact on climate. This can last for thousands of years. Volcanoes have quite a bit of affect on climate. And this affect can be rather short term (volcanic ash) or long term (rain-shadow effect) in nature. Again biology can be affected by this too. For example, a desert area may quickly develop on the leeward side of a new volcano. If life is not able to adjust, extinction will become a significant threat. http://www.djburnette.com/projects/volcanoes.html

Solomon vs. Socrates :: essays research papers

Solomon vs. Socrates: what they thought wisdom was, where it came from, and how it was taught. Solomon and Socrates are thought of as the wisest men in history. Solomon was a man of God who wrote Proverbs, Ecclesiastes, and Songs of Songs in the Bible. The great philosopher, Socrates, lived in the Classical Age of Greece. Their styles of teaching and perspectives on wisdom were very different, but they did have their similarities. While Solomon and Socrates had the same perspective on what wisdom was, they had contrasting understandings on where it came from. Solomon’s definition of wisdom was the knowledge of making wise choices. Proverbs 1:2-3 says, Wisdom is instruction in wise dealings with others. Wisdom is instruction in righteousness, knowing the difference between good and evil. Wisdom is instruction in justice, knowing how to do what is right. It is the simple learning shrewdness so that they are not taken advantage of. It is the young learning knowledge and prudence. For both the young and the old it is an increase in skill, understanding and knowledge. In Proverbs, he was trying to show his readers how to make wise choices. All of what Solomon wrote came straight from God, and he believed that the only way that anyone could get wisdom was if they got it from God. 1 Kings 3: 5-13 says, In Gibeon the LORD appeared to Solomon in a dream by night: and God said, Ask what I shall give thee. And Solomon said, Thou hast showed unto thy servant David my father great mercy, according as he walked before thee in truth, and in righteousness, and in uprightness of heart with thee; and thou has  Ã‚  Ã‚  Ã‚  Ã‚  t kept for him this great kindness, that thou hast given him a son to sit on his throne, as it is this day. And now, O LORD my God, thou hast made thy servant king instead of David my father: and I am but a little child: I know not how to go out or come in. And thy servant is in the midst of thy people which thou hast chosen, a great people, that cannot be numbered nor counted for multitude. Give therefore thy servant an understanding heart to judge thy people, that I may discern between good and bad: for who is able to judge this thy so great a people? And the speech pleased the Lord, that Solomon had asked this thing.

Internet and Privacy Essay

There has been a lot of controversy about the internet and its privacy. Today, some say you have no privacy with anything you do on the web. They say that the government is taking away the public’s privacy because they can monitor everything that happens on the internet. Even though most of this is true, there are plenty of good things to come from it. In this essay I will be writing about the internet and its privacy. The lack of privacy that comes with technology and the internet can and has prevented a lot of crimes to occur. It has made credit card fraud, once an easy crime much harder to get away with. They know what you’re buying schedule is like, so if someone steals your card and tries to buy something that is not something you would normally buy, you will get an alert about it. Security cameras at stores and ATM’s prevent a lot of robberies from occurring. The government states that the main reason why they monitor just about everything on the internet is to try and catch terrorist attacks before they happen. They have said that some of the terrorist plane hijackings could have been prevented if they had the internet security that they do now. Of all the good things that come with the internet, there are also some drawbacks that can be dangerous. There is just as much false information on the internet as there is true information. Hackers can create viruses that can get into your personal computer and ruin valuable data. They can also create viruses to steal personal valuable data such as identity theft. There are also people called â€Å"predators† that hang out on the internet waiting to get unsuspected people into dangerous situations. People can get addicted to the internet which can cause problems with interacting with their friends and family. As it is stated in What Matters in America, â€Å"Like any space where people gather, the virtual world is not immune to the same set of troubles we face in real life. Teens and children can be targeted be sexual predators. Kids can â€Å"cyber bully† classmates, carrying the tortures of the playground onto cell phones and computer screens at home. Illicit romances and online flirting may be taken beyond laptops, ruining relationships and destroying marriages. And, of course, cybercrime is ever present, seeking log in numbers, financial data, and credit card information†. (22) Privacy has become a big question in today’s society with all this new technology and the internet. The internet might be more secure today from hackers and viruses but we don’t really have any privacy on the web. Every purchase we make on the internet can be tracked by the government. They can also track almost every phone call that is made. The internet has become more convenient to use than it ever has been. You can perform just about any task you want with a couple mouse clicks. Your computer can remember everything you do on the internet. It will save all the sites you have been to, what you have downloaded, what you have bought online, and can even save your credit card information. When online you will see recommended web sites based on what you normally do online and even on certain sites there will be recommended products that are similar from what you have purchased before. All this personal information can be easily looked at by the government or even professional hackers. Is our privacy really being invaded or are we just putting this information out there? People say that the government is invading the public’s privacy. They say that they shouldn’t be allowed to monitor the internet. I don’t believe our privacy is being invaded because no one forces you to put this information online, even though it is hard not to in today’s society. In What Matters in America, David Plotz states, â€Å"Real privacy is what allows us to share hopes, dreams, fantasies, fears, and makes us feel we can safely expose all our faults and quirks and still be loved. Privacy is the space between us and our dearest, where everything is known and does not matter. † (70) With all this advanced technology on the internet, we need the government to monitor it or else there would be a huge amount of criminal activity and the internet would not be safe.

Pathos

â€Å"Emotional appeals (sometimes called appeals to pathos) are powerful tools for influencing what people think and believe† (Everything’s an argument 38). There are many methods that can be used to create an emotional connection with people. In the story called â€Å"The F word† by Firoozeh Dumas, the author use humor to emotionally connect the readers to her story. In some instances when writers want to get a deeper message across to the audiences they use a sadder approach. In the commercial by AT&T, they try to get the message across texting and driving and the serious consequences.A good method that some authors use to get the attention and achieve a connection with the audience is by using humor. In the story called â€Å"The F Word,† the author, Firoozeh Dumas, talks about her experience growing up in American with an Iranian name that was very difficult for people to say. She goes to talk about how it was more of a struggle fitting in with her na me than anything else. â€Å"All of us immigrants knew that moving to America would be fraught with challenges, but none of us thought that our names would be such an obstacle. (Firoozeh Dumas 751) Being so fed up with the name butchering, she decides to change her name to a much easier American name, Julie. She goes by the name of Julie for a while then decides to go back to Firoozeh. She mentions in the book that after a while she stopped caring about what people call her and responds to just about any name that begins with an F (Firoozeh Dumas 754). Dumas was successful in getting her story across to the readers and many people in this country can relate to this story coming from a different country with a long or difficult name to say.To get a message across or create awareness, some authors and the media like to use more of a deeper more relatable approach, by having people talk about their life experiences, putting up graphic pictures, even show the tragedy that is occurring because of something. In the T. V. ad by AT&T, they raise awareness of the dangers of texting while driving. In the commercial, it had one word show up in the beginning that said, â€Å"Yeah,† and you hear the voice of a girl saying, â€Å"This is the text my sister was reading from me when she crashed her car and died. It was a quick sixteen second commercial, but it was a successful way of using pathos and good message to get across to the audience with a deep emotional connection. This shows that your life can change because of a simple message and affect those who love you. It can be very relatable to those younger drivers and even parents that like to use their cell phones while driving. Pathos is used when writers or even the media want to gain an emotional connection to their audiences and use emotional appeals to influence them. In â€Å"The ‘F’ Word,† by Firoozeh Dumas, she uses humor to connect her story to her audiences.It was a very relatable story and was a good example of using pathos. Another successful form of pathos was in an advertisement by AT&T about texting and driving. It was a sad form of pathos but it was a good message to get across to the audiences that drive and like to use their cell phones. The use of pathos is widely used to influence and draw an emotional appeal to the readers. Some are successful with it and others fail to gain a connection. The story of Dumas and the advertisement by AT&T were both successful with the use of pathos.

Human-Environment Interaction Essay Example

Human Human-Environment Interaction Paper Human-Environment Interaction Paper They interact with the environment by adjusting to climate conditions and by making active changes to places around them. Let us explore what had happened when an area called Woodside was discovered by new Americans, and what Human-Environmental Interactions were initiated by the humans there. Woodside is a neighborhood in the borough of Queens, which is located in New York City. It shares borders with the towns of Astoria, Masters, Sundered, Elmhurst and Jackson Heights. The first settlers that came to Woodside in 18th century were farmers. They discovered that he sloping grounds and the climate conditions in the area were appropriate for growing crops and raising cattle. Lots of trees had to be taken down to make room for farm land. Destruction of wooded areas, created by humans, contributed to the extinction of wild life as a direct result of a natural habitat loss. At first, Woodside was a swamp in the 17th and 1 8th centuries. Later, in the 19th century settlers drained the land. The environment influenced humans by the gravity by keeping everything and us on the ground, instead of floating in the air. The storms in Woodside created blackouts and loss of power and internet. In the second part of 19th century Woodside environment took another significant change due to a large residential development. Rows of houses were built, destroying more trees and fertile soil, to accommodate new comers: families of Irish Americans. By the sass about eighty present (%) of the neighborhood population were Irish. During the 20th century farms were quickly disappearing as roads, train tracks, schools, churches, stores, and commercial buildings were erected. Less space was left for parks and green grass to grow. Some private houses were taken down to accommodate apartment buildings, making the area to be even more populated. The new people that arrived in bigger numbers and different diversities (Italians, Koreans, Chinese, Filipinos, Latino, Indians, Bangladesh and Pakistanis) were settling in Woodside and were attracted by the close proximity to Manhattan, availability of jobs at factories and the well- developed transportation routes. The amount of busses and cars needed to eve people around had to grow as well, which contributed to air pollution with toxic fumes. The Woodside that we know today is a vibrant community with many cultures mixed together. People of the neighborhood have to learn the importance of human interaction with the environment. They have to be more responsible and take actions to reduce negative impacts on the community by consuming less, recycling, choosing cleaner fuels to fill cars and heat homes, planting more trees. Each of us by contributing a small part can help to build a better and cleaner future for all, who call Woodside home.