Police Brutality Becoming A United States - 1784 Words

Mariana Garcia Mr. Lyons English 4 CP 30 October, 2015 Police Brutality: Becoming More Frequent in the United States â€Å"The rights of every man are diminished when the rights of one man are threatened† (John F. Kennedy). Police Brutality is a violation to the Federal Civil Rights Act. If cruelly beaten, kicked, and thrown by a person who is supposed to ensure the law, will you then trust them afterwards? Will your rights be valid then? Officers wear the badge and uniform which will make them feel superior making them think the law is in their hands and can twist and change it as they please. Jessica Watson-Crosby comments on the police brutality history and says, from the point of view of its victims, police were seen as protecting the upper classes. Police violence only came under scrutiny when â€Å"decent† people became victims, usually accidentally. As you see the chaos created by officers has been in the United States for a long time and has worsened over time. â€Å"Police are guaranteed a steady living. Unlike other workers , they typically are not threatened by layoffs or pay cuts† (Watson-Crosby). All who did not give their opinion over the authority were left unharmed and for the ones who spoke to let their rights be known were not as lucky. â€Å"Many police see themselves as part of the upper classes â€Å"the enforcers of social value† even while the upper classes see them as ignorant brutes. As a rule, the upperShow MoreRelatedPolice Brutality And The United States Essay1408 Words   |  6 PagesPolice brutality in the United States has escalated in recent times. To develop a peaceful environment amongst human beings, one of the main topics to look at is human rights. While more often than not, police brutality violates the concept of human rights it is still a very important task to discuss the topic and create possible solutions to such a concerning and threatening issues in the United States. In this case, statistics is a very important factor that is required to display how serious ofRead MorePolice Brutality Has Increased T hroughout The United States Essay1307 Words   |  6 PagesPolice brutality has increased rapidly over the past few years. In fact, 19.4 percent of cases between officers and suspects tend to tie into police brutality. It takes men and women 21 weeks to train and graduate as a police officer. These same people take an oath to ensure they will never use their badge for harm, but now the trust that the citizens have with the police are depleting. 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I wanted to do more investigating on this topic, since more cases of police brutality which have been recorded have been surfacing on new outlets, to enlightenRead MorePersuasive Essay On Police Brutality1079 Words   |  5 Pagesnot even want to encounter a policer officer. The reason why? Police brutality. The article Police Brutality by gale defines police brutality as: The use of unnecessary, excessive force by police in their encounters with civilians. The force used is beyond what would be considered necessary in the situation at hand. (Police Brutality). The same individuals who are supposed to protect and serve the citizens of the United States have instilled fear into the hearts of those that are a part ofRead MorePolice Brutality Is Not A New Occurrence930 Words   |  4 Pageswhen someone says the word â€Å"police† they will picture a clean cut officer in uniform serving to protect their community from harm. 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This occurred because police officers failed to put a seatbelt onRead MoreArgumentative Essay : Police Brutality1561 Words   |  7 Pageshas been an overwhelming amount of police brutality in recent years. Police brutality can be defined as, when a police officer uses more force than necessary. This issue has spread throughout the United States of America, and is putting the lives of our citizens in great danger. Police brutality is not only physical, but it can also be verbal attacks; and, in most cases, it is caused by false arrest and racial profiling due to police corruption. Police brutality has been and continues to be a majorRead MoreLaw Enforcement Is Not The Public Safe1675 Words   |  7 Pagesabiding by the regulations se t in place in the United States of America. However, with such responsibility comes power and this often goes to one’s head. Some officers take advantage of the authority that they have over the public. People are becoming more and more aware of the police brutality that occurs in this country as more cases are brought to the attention of the media. It is becoming increasingly common for people to film interactions with the police, especially the cases where there is misconduct

Combined Gas Law Definition and Examples

The combined gas law combines the three gas laws: Boyles Law, Charles Law, and Gay-Lussacs Law. It states that the ratio of the product of pressure and volume and the absolute temperature of a gas is equal to a constant. When Avogadros law is added to the combined gas law, the ideal gas law results. Unlike the named gas laws, the combined gas law doesnt have an official discoverer. It is simply a combination of the other gas laws that works when everything except temperature, pressure, and volume are held constant. There are a couple of common equations for writing the combined gas law. The classic law relates Boyles law and Charles law to state: PV/T k where P pressure,  V volume,  T absolute temperature (Kelvin), and  k constant. The constant k is a true constant if the number of moles of the gas doesnt change.  Otherwise, it varies. Another common formula for the combined gas law relates before and after conditions of a gas: P1V1 / T1 P2V2 / T2 Example Find the volume of a gas at STP when 2.00 liters is collected at 745.0 mm Hg and 25.0 degrees Celsius. To solve the problem, you first need to identify which formula to use. In this case, the question asks about conditions at STP, so you know youre dealing with a before and after problem. Next, you need to understand  STP. If you havent memorized this already (and you probably should, since it appears a lot), STP refers to standard temperature and pressure, which is 273 Kelvin and 760.0 mm Hg. Because the law works using absolute temperature, you need to convert  25.0  degrees Celsius to the Kelvin scale. This gives you 298 Kelvin. At this point, you can plug the values into the formula and solve for the unknown. A common mistake some people make when theyre new to this kind of problem is confusing which numbers go together. Its good practice to identify the variables. In this problem they are: P1   745.0 mm HgV1   2.00 LT1   298 KP2   760.0 mm HgV2   x (the unknown youre solving for)T2   273 K Next, take the formula and set it up to solve for the unknown  x, which in this problem  is  V2: P1V1  / T1   P2V2  / T2 Cross-multiply to clear the fractions: P1V1T2   P2V2T1 Divide to isolate  V2: V2   (P1V1T2) / (P2T1) Plug in the numbers and solve for V2: V2  Ã‚  (745.0 mm Hg  · 2.00 L  · 273 K) / (760 mm Hg  · 298 K)V2 1.796 L Report the result using the correct number of significant figures: V2   1.80 L Applications The combined gas law has practical applications when dealing with gases at ordinary temperatures and pressures. Like other gas laws based on ideal behavior, it becomes less accurate at high temperatures and pressures. The law is used in thermodynamics and fluid mechanics. For example, it can be used to calculate pressure, volume, or temperature for the gas in clouds to forecast weather.

A Palaeo Environmental Assessment Of Sediments Free Essays

string(129) " and beginning of deposits Table 3: Summary of Proxies measured and how they can be used for palaeoenvironmental Reconstruction\." This palaeo-environmental Reconstruction is based upon utilizing a multi-proxy attack to analyze lake deposits. The lake of Wuxu-hai prevarications in the Province of Yunnan, southwest China ( figures 1 and 2 ) and consists of a individual basin mensurating 1.7km2 situated at an height of 3630m a. We will write a custom essay sample on A Palaeo Environmental Assessment Of Sediments or any similar topic only for you Order Now s.l. It is thought that Wuxu-hai Lake was formed by glacial procedures during the Last Glacial Maximum ( LGM ) . At present, the catchment lies in a sub-alpine flora belt situated at 250m below the current treeline. The flora is chiefly comprised of cone-bearing wood ( Pinus, Picea and Abies ) , deciduous and evergreen Quercus. The country above the current treeline is dominated by grassland steppe. 1.2. Materials, Methods and Techniques In 2008 a 6.5 m nucleus was extracted from the Centre of Wuxu-hai Lake and sub-sampled at a declaration of 2cm, utilizing a multi-proxy attack, affecting a assortment of lithological and biological techniques. Vegetation screen Reconstruction within the lake catchment is inferred from alterations in the pollen concentrations of species over clip ( Pinus, Quercas, Artemisia and Poaceae ) . Loss on Ignition ( LOI ) has been carried out to find the organic content of the nucleus. Furthermore, Mineral Magnetic Analysis ( Xlf ) has taken topographic point in order to find the entire magnetic composing of the majority deposit. Finally, Micro Charcoal analysis ( grains/cm3 ) has been used to uncover counts of micro wood coal, supplying a record of past fire events within the catchment. Figure 1: Map exemplifying the Figure 2: Detailed map of Yunnan States of China. Province ( approx 380,000km2 ) . 2. ) Chronology Radiocarbon dating was carried out on 12 equally separated subdivisions of the nucleus utilizing a assortment of different stuffs. The natural 14C ages can non be straight used as a calendar day of the month. This is because the degrees of atmospheric 14C have non remained changeless during the span of clip that can be radiocarbon dated. Therefore, the natural 14C ages BP have been calibrated at 1 sigma and expressed as a mid point value ( Cal yr BP ) to give accurate calendar old ages. ( table 1 ) . Depth Material 14C Age ( uncalibrated ) Cal year BP ( 2 sigma ) Standard Error Median Age ( Cal yr BP ) Calender Year 72.25 Wood 8001 Â ± 50 8698 – 9011 0.979567 8854.5 Â ± 50 6904.5 80.25 Shell 7899 Â ± 65 8587 – 8987 1 8787 Â ± 65 6837 130.5 Wood 9211 Â ± 39 10253 – 10443 0.858516 10348 Â ± 39 8398 142.5 Leaf 9555 Â ± 55 10702 – 11109 0.991144 10905.5 Â ± 55 8955.5 151.5 Leaf 10018 Â ± 27 11329 – 11629 0.959505 11479 Â ± 27 9529 225.5 Majority 8742 Â ± 125 9535 – 10160 1 9847.5 Â ± 125 7897.5 268.5 Seed 13571 Â ± 33 15800 – 16546 1 16173 Â ± 33 14223 307.5 Leaf 14258 Â ± 54 16618 – 17438 1 17028 Â ± 54 15078 359.5 Wood 14723 Â ± 67 17285 – 18083 1 17684 Â ± 67 15734 431.5 Wood 16216 Â ± 41 19228 – 19484 1 19356 Â ± 41 17406 501.5 Shell 12321 Â ± 78 13994 – 14734 1 14364 Â ± 78 12414 629.5 Majority 18921 Â ± 102 22238 – 22638 1 22438 Â ± 102 20488 Table 1: Chronology tabular array exemplifying calibrated 14C AMS day of the months for WX1-08 nucleus. On-line standardization was calculated utilizing Calib Executive Version 5.0.2 package ( Stuiver and Reimer, 1993 ) . The tabular array besides illustrates the carbon 14 ages, standard mistake values, deepnesss of stuffs dated, type of stuff, uncalibrated and graduated day of the months. 3. ) Age-depth Model Figure 3: Age-depth theoretical account covers the period from 22.438 cal year BP – nowadays. Age deepness theoretical account Using the information illustrated in table 1, an age-depth theoretical account was created for the nucleus. However, it is necessary to province that when making the age-depth theoretical account, two of the original informations points were removed ( Table 2 ) . Depth Material 14C Age ( uncalibrated ) Cal year BP ( 2 sigma ) Standard Error Median Age ( Cal yr BP ) Calender Year 225.5 Majority 8742 Â ± 125 9535 – 10160 1 9847.5 Â ± 125 7897.5 501.5 Shell 12321 Â ± 78 13994 – 14734 1 14364 Â ± 78 12414 Table 2: Table exemplifying the 2 values that were considered anomalousnesss. The majority and shell stuffs, which were at deepnesss of 225.5 and 501.5 within the nucleus sample represented significantly lower median ages than the information points above them. This instantly became apparent when plotting them on the age-depth theoretical account as their average ages ( Cal yr BP ) represented obvious anomalousnesss. These values were removed from the age-depth theoretical account. Figure 4: Four zones have been interpreted from the magnetic susceptibleness values. These values indicate mineral magnetic belongingss which can be used to set up alterations in rates of deposit which can so deduce alterations in clime or alterations is the energy of the clime around the catchment ( Dearing, 1986 ) . The four zones stretch across all placeholders leting a multi-proxy probe in which palaeo Reconstruction is based on the integrating of grounds from all the beginnings. Entire organic C Pinus Quercus Artemisia Poaceae Loss-on-Ignition Charcoal Magnetic Susceptibility Percentage ( % ) Percentage ( % ) Percentage ( % ) Percentage ( % ) Percentage ( % ) Grains Per Gram Xlf 9517 13371 16376 19033 20827 22105 Entire organic Silicate Zone 1 Zone 2 Zone 3 Zone 4 5. ) Data reading 5.1. ) The undermentioned subdivision is an reading of the dataset in order to bring forth a paleoenvironmental history for Wuxu-hai Lake. Comparisons to local and regional datasets will be made throughout to measure larger-scale forms that could be related to climatic alterations. Proxy Inference Pinus Tree ( Pine ) Coniferous Grows at High heights ( Upland tree ) Cool conditions, precipitation Poor, coarse textured dirts pollen-analytical oscillations Temporal alterations in flora screen ( vegetation belt displacements ) Treelines: climatically sensitive transitional zones Ecological alterations Not all workss produce same measures of pollen Quercus Tree ( Oak ) Deciduous and Evergreen Grows at lower lifts than Pinus ( Valley braid ) Better dirts than Pinus Artemisia Herb/Shrub Grows at lower lifts than Pinus Warm conditions, prohibitionist Steppe environment Gramineae Grass Occurs in a broad assortment of environments Chiefly grassland steppe ( above treeline ) Loss on Ignition Organic content of sample Charcoal Record of past fire events Magnetic Susceptibility Geology, dirt procedures, deposit tracts, pollution, biological conditions ( Thomas and Goudie, 2000 ) Erosion rates and beginning of deposits Table 3: Summary of Proxies measured and how they can be used for palaeoenvironmental Reconstruction. 5.2. ) Zone 4: ( 635.75cm-500cm ) 22,500 Cal yr BP-20,000 Cal year BP ( approx ) At the beginning of this period Artemisia concentrations experience a big addition and disconnected lessening which is so followed by a steady overall addition to the terminal of this period. This steady overall addition is besides apparent from the Poaceae concentrations. However, the Pinus concentrations, which continually fluctuate during this period, illustrate an overall lessening. The Quercus concentrations fluctuate but remain at a relatively low degree throughout this period. These pollen concentrations suggest that the treeline was sing a progressive diminution in height during this period, leting an increased growing in highland grasses above the treeline. This causes increased Artemisia and Poaceae concentration which, in bend, would show that the catchment country was sing ice chest temperatures than antecedently. Yu et al. , ( 2003 ) survey utilizing a digest of lake records across China illustrated that cold, wet conditions were experienced in western China, before the LGM, produced by a lessening in vaporization due to a low temperature on land and an addition in precipitation. Towards the terminal of the zone the Pinus concentrations experience a rapid lessening to much lower values than old. The degrees of wood coal besides lessening. At this point the Poaceae and Artimisia concentrations demonstrate a rapid addition. This suggests that the treeline retreated to even lower heights within the catchment country, where it was sing even colder conditions than earlier and increased precipitation. During this clip Yan et al. , ( 2007 ) illustrated glacial-induced downward migrations of alpine species ( Pinus ) in cardinal and west of Yunnan Province. The magnetic susceptibleness signal demonstrates multiple fluctuations throughout this period. However, more specifically, it is apparent that the signal high spots a autumn in the mineral magnetic belongingss of the deposit at the terminal of this period. This lessening in the mineral magnetic signal indicates a alteration in the rates of deposit, perchance due to reduced rates of dirt eroding within the catchment. 5.3. ) Zone 3: ( 500cm-360cm ) 20,000 Cal year BP -18,000 Cal year BP ( approx ) All pollen concentrations fluctuate greatly during this period showing the environmental volatility that was being experienced within the catchment. The Pinus pollen diagram demonstrates that several periods of rapid reduced concentrations take topographic point, in between several periods of rapid increased concentrations. This suggests that during this period of environmental volatility the treeline height was continually fluctuating as a consequence of a series of cold stages within the catchment. These continual fluctuations in treeline height are besides apparent from the Artemisia and Poaceae concentrations. As the Pinus concentrations quickly decrease due to a decrease in treeline height and hence tree screen, the Artemisia and Poaceae concentrations quickly increase, due to an expansion of grassland countries situated above the treeline. Therefore, it is clear that this period represents an unstable clime which was continually switching between cold and warm stages. Throughout this period there is a continued fluctuation in the magnetic susceptibleness signal. However, the fluctuations occur at lower values than antecedently seen in zone 4. It is apparent that at the terminal of this zone there is a sudden important autumn in the magnetic susceptibleness signal. It appears that this lessening may be associated with the Last Glacial Maximum ( LGM ) . The timing of the LGM in China is problematic. However many writers place the LGM at 18,000 BP. Equally good as the autumn in the magnetic susceptibleness signal, it is evident from the pollen diagrams that at this clip there are immediate big lessenings in Artemisia and Poaceae concentrations and, after a lag period, big additions in Pinus and Quercus concentrations. This big addition in tree pollen within the catchment demonstrates that the treeline increased in height as a consequence of clime betterment leting a short lived enlargement of forest countries. Walker ( 1986 ) explains that after the LGM, the flora began to react really shortly after or every bit shortly as deglaciation left surfaces available. 5.4. ) Zone 2: ( 360cm-210 ) 18,000 Cal yr BP-13,700 Cal year BP ( approx ) At the beginning of this period the treeline was at its topmost bound, about 18,000BP. However, after 18,000BP terrible diebacks of treeline occur, this is apparent when the concentrations of Pinus and Quercus all of a sudden experience a important lessening. The Er Yuan lake dataset from Yunnan provides grounds to propose that average one-year temperature, at about 18,000-17,000 BP, may hold been 4’C below current temps ( Walker,1986 ) . The cold conditions experienced at Er Yuan may hold besides been experienced at Wuxu-hai which would explicate the terrible dieback of the treeline. From this point onwards the concentrations of Pinus and Quercus fluctuate until about 11,500 BP. Poacea concentrations remain between 0 and 20 ( grains/gram ) but besides fluctuate until about 11,500. A lake nucleus dataset from Xi Hu, Yunnan, highlighted a period between 15,000-10,500 BP which demonstrated a fluctuating clime with periods of intense seasonality ( Shaomeng et al 1986 ) . The fluc tuations in all pollen concentrations evident in the nucleus may so correlate to this period of intense seasonality experienced at Xi Hu. However, a high declaration spelethem record from two caves in sou’-west Yunnan demonstrate that the Indian Monsoon varied significantly during the period of last deglaciation, resembling other East Asiatic monsoon records, such as those from Hulu and Dongge Caves ( Cai et al. , 2006 ) . Therefore, the fluctuations in all pollen concentrations evident in the nucleus during this period could be related to the fluctuations in Monsoonal strength. Artemisia concentrations experience a important extremum at about 15,600 BP. This extremum may be attributed to the same cold-semi humid conditions which were experienced at Xi Hu between 17,000-15,000 BP ( Shaomeng et al 1986 ) . The Artimisia concentration so diminish where they excessively continue to fluctuate until about 11,500 BP. These fluctuations highlight a period after the LGM but before 11,500 BP during which short lived but complex vegetal alterations were taking topographic point. Walker ( 1986 ) highlights a similar fluctuation period within the Er Yuan lake dataset, between 14,000-10,500 BP, and states that this was the most vegetationally complex period. However, these fluctuations have no antagonistic portion in the Kunming lake dataset exemplifying the complexness of local clime alterations in Yunnan. Directly after the LGM the magnetic susceptibleness signal increases back to similar values that were present during zone 4. A strong extremum in the magnetic susceptibleness signal is apparent within this zone, about 16,700 BP. This may bespeak a alteration in deposit such as an inflow of tephra into the catchment country or Aeolian dust from desert parts in the North. However, this strong extremum in the magnetic susceptibleness signal is matched with reduced degrees of Pinus and Quercus concentrations which may bespeak that the environment within the catchment became unstable, impacting tree growing. 5.5. ) Zone 1: ( 360cm-0cm ) 13,700 Cal yr BP-Present ( approx ) This zone demonstrates a important extremum in wood coal concentrations at a deepness of 144cm, about 11,000BP. This addition is likely to stand for a big fire event within or around the catchment country. At the same clip there is a lessening in Quercus, Artimisia and Poaceae concentrations which imply that these countries within the catchment were affected by the fire. Around this clip Xi Hu experienced multiple vegetal and climatic events which were attributed to the Pleistocene-Holocene passage ( Shaomeng et al 1986 ) . However, this appears to hold no resemblance in Wuxu-hai, perchance due to the effects of the fire event. The Quercus, Artimisia and Poaceae concentrations so continue to worsen until 120cm, about 10,300, when Artimisia and Poaceae concentrations within the catchment addition. The pollen diagrams besides indicate that, at about 9,500 BP, the flora within the catchment begins to make a period of comparative stableness. No more rapid fluctuations in flora screen occ ur. The Xi Hu dataset besides illustrates the fact that after 10,500 there is no grounds of climatic alteration ( Shaomeng et al 1986 ) . Vegetation alteration after this period is largely of the order of accommodations within units. At a deepness of 100cm, about 9600 BP, the pollen diagrams demonstrate a gradual addition in concentrations of all pollen types. Menghai, Er Yuan and Kunming lake datasets attribute this addition, by about 10,000 BP, to the clime nearing modern values ( Walker, 1986 ) . At a deepness of 50cm, about 7,400BP Artemisia and Quercus concentrations demonstrate a steady lessening whereas Pinus and Poaceae concentrations remain stable. These comparatively stable concentrations demonstrate a displacement towards a new balance, closely similar to that of today and highlight the terminal of the environmental volatility which was apparent in the old zones. The Er Yuan and Kunming dataset besides indicate that by 10,500-7500 average one-year temperature and rainfall had reached degrees similar to today ( Walker, 1986 ) . The entire organic C concentration within this period indicates a important addition at a deepness of 50cm, about 7,500 BP, bespeaking a rapid inflow of organic affair into the lake at this clip. 6. ) Decision Having described climatic alterations at Wuxu-hai catchment which history for the proxy accommodations it is apparent that the period between about 22,500 BP – nowadays, is by and large dividable into, a clip before 13,500 BP when the clime form was complex, through a move towards progressively simplicity taking to a new stableness. However, it is indispensable to understand that this is a simplification of the many complex alterations that were taking topographic point throughout this period. Comparisons with other local and regional datasets have highlighted the fact that the paleoenvironmental history at Wuxu-hai has several comparings with the Er Yuan and Xi Hu lake datasets. However, the Kunming dataset comparings are non as clear. As Xiwen and Walker ( 1986 ) explain, there is a great assortment of local climes bring forthing vegetal differences, sometimes even on opposite sides of the same vale. How to cite A Palaeo Environmental Assessment Of Sediments, Essay examples

Leading and Managing People Innovation Skills

Question: Discuss about the Leading and Managing People for Innovation Skills. Answer: Introduction The following assignment has evaluated significant aspects of the leadership style of Alan George Lafley who is considered for his remarkable contribution as CEO of Protector and Gamble (PG). The analysis has found several major facets such as ethics, theories, evolution and psychology of leadership in context to the leadership style of A.G Lafley. The assessment has tried to understand whether the leadership style of the mentioned persona matches with the concept of multicultural leadership or not. Leadership style of Alan George Lafley Alan George Lafley who has performed as CEO, president and chairperson for several years started his career by joining PG after his graduation from the business school of Harvard in the year 1977. After giving ten years of leadership as the CEO in PG, unfortunately, he was replaced by Robert McDonald due to having rapid complaints from the investors and constant decrease in sale. It has been Lafleys credible performance that PG called him back even after his retirement in 2000. According to the Journal report of Wall Street, his leadership doubled the sale rate and the company earned near about $84 billion (Tuna 2016). The consumer is the ultimate boss- has been the fundamental concept of Lafley that boosted him to become a wise and progressive CEO. According to A.G Lafley, a leader should perform as a bridge to the world outside. Additionally, he believes that an efficient leader should focus on a businesss structural charisma, a companys strategic curriculum about its core competency and its current position comparing with the rival enterprises (Tuna 2016). As per Lafleys point of view, robust and creative leadership is required to establish an organization's vision. Hence he stated that a leader cannot ignore his values and standards which have been shaped by him for the fellow subordinates. Leadership ethics A person should be called an effective leader when he would be found concentrating on what is right and promote positive influence upon subordinates by helping them to choose the right. According to Rice (2013), an efficient and fruitful business leader prefers to minimize the indulgence of negative interpersonal attitude and always considers taking other's opinions in the case of making any ethical decisions. It is essential to value other's point of view and show respect while serving as a leader. Lafley acquired the position of CEO in PG when the company has been suffering from the rapid downfall in the Asian market (News.pg.com 2016). Lafleys initiative to reinforce a management full of ethical values, principles and concrete purposes leading to the company's success for decades is indicative of the fact that he has considered following the basic leadership ethics. There has been a time when PG has been criticized for being ignorant about the laws and regulations. Lafley fought out all such criticism by defining the fact that the company has conducted its operations by following what is right. His leadership helped the enterprise to do business by giving fair treatment and priority to all (Wade 2013). Moreover, following his leadership the company concentrated upon not only their achievement, rather they focus on to investigate whether the success has been earned legally. Leadership Evolution The concept of leadership has gone through a rapid evolution over years as the idea of a directive and oppressive and autocratic leadership has now shifted to Democratic leadership (Rice 2013). In the current business scenario, leaders in business consider taking possible participation which in a way supports them in providing motivation which a possible aspect of leadership. CCL (Center for Creative Leadership) has identified that 83% of the survey upon leadership proves that the autocratic concept of leadership has gone through a rapid evolution over past few years. Lafley is among one of those leaders who have changed the concept of top-down management concept to a progressive and individual thinking oriented management. Lafleys innovative leadership skills like understanding consumer's feelings and point of views. He spent years to visit countries and going directly to the customers to get information about their demands (Bloomberg.com 2016). His leadership progressed from being a mere employee to the chairman to ultimately the CEO of PG. Leadership theory Evolution in leadership has changed from Great man, trait theory to Participative, Contingency, transformational, transactional and Situational leadership. According to Great Man and trait theory, histories are made by great men who have in born heroic traits like intelligence, charisma in behavior. As per participative theory, leaders should engage their fellow subordinates in time of decision making (Smith 2014). Based on contingency theory decisions and action by the leaders should be taken base on individual situation and their importance. Following Lafleys leadership pattern, it seems that he believes in taking decisions based on individual situation and therefore his leadership style changes rapidly. For instance, his initial role as a leader has been to visit Asian countries to have full control over the market of that domain finally. Later his leadership transformed to his return to the United States to take over PG's business operations for beauty products. On the other hand, in the time of the crisis in the year 2000, he changed his strategy and started to break and rebuild the company to keep RG's position secure in the market (News.pg.com 2016). Thus it seems that his leadership style matches with the Transformational theory of leadership. According to the theory, leaders interact with subordinates to provide a proper amount of motivation which enhances employee productivity (Smith 2014). Psychology of leadership and its multicultural trend Over years the psychological concept of leadership has changed as unlike previous time leaders now prefers to give ear to the values and point views of the subordinates rather than using intelligence and charisma. A.G Lafley is one significant example of it. Lafley believes that leadership should not be limited to the thinking that leaders are born and not made, and leadership only depends on traits like charisma, intellectual capabilities (Lafley and Charan 2014). According to Lafley, he grew to become a successful leader and his intensity to win helped him to gain that. It is, therefore, indicative of the fact that Lafley has followed the newly emerged psychology of leadership. Lafley specifically visited Japan and other parts of South East Asia and had good amount of interaction with the customers to acquire data about individual demand and desire regarding their products (Lafley and Martin 2013). As per multicultural leadership, leaders are driven to make geography oriented performance and should move outside their comfort zone. Conclusion From the above assessment, it can be deducted that A.G Lafley's leadership style matches with the transformational theory of leadership as he prefers to transform the behavior of his fellow subordinates by motivating them. Furthermore, it is understandable from the analysis that his steps and contribution to PG are an example of multicultural leadership trend. Reference Bloomberg.com. (2016).A.G. Lafleys Innovation Skills Will Weather PGs Storm - Bloomberg. [online] Available at: https://www.bloomberg.com/news/articles/2013-06-03/a-dot-g-dot-lafley-s-innovation-skills-will-weather-p-and-g-s-storm [Accessed 2 Sep. 2016]. Lafley, A.G. and Charan, R., 2014.PG's innovation culture. Strategy+ Business. Lafley, A.G. and Martin, R.L., 2013. Playing to win.Foreign Affairs,73. News.pg.com. (2016).A.G. Lafley Rejoins Procter Gamble as Chairman, President and Chief Executive Officer | PG News | Events, Multimedia, Public Relations. [online] Available at: https://news.pg.com/press-release/pg-corporate-announcements/ag-lafley-rejoins-procter-gamble-chairman-president-and-chi [Accessed 2 Sep. 2016]. Rice, G., 2013. Book ReviewKeeping It Real: The Role of Authenticity in Leadership and High Performance.Global Business and Organizational Excellence,32(5), pp.105-110. Smith, E.B., 2014. The Effect of Critical Optimism on Transformational Leadership.Leadership Organizational Management Journal,2014(1). Tuna, C. (2016).A.G. Lafley's Advice for Future Leaders. [online] WSJ. Available at: https://www.wsj.com/articles/SB124451772932297029 [Accessed 2 Sep. 2016]. Wade, J., 2013. Procter Gamble's former CEO on risk and strategy.Risk Management,60(2), pp.16-18.