Public Relations Communication Theories Essay Example | Topics and Well Written Essays - 3500 words

Public Relations Communication Theories - Essay Example According to general public or business group, communication refers to the transferring the information from one source to another source. In other words, in the general public context the communication and information are used interchangeably. Communication is considered as the small part of the big picture, which includes organizing, planning, controlling and managing ( Dainton & Zelley, 2005, p. 2). Contrariwise, the views of scholars are different regarding the concept and perception of communication. Marianne Dainton & Elaine D. Zelley, in their book on â€Å"Applying Communication Theory for Professional Life† (2005, p 2-3) described that scholars believe that the communication is believed to be the process instead of information. The kind of process, which is elaborated in the book, is referred to as the one in which people interact with each other to create the meanings and then develop the sustainability of the messages, which may lead them to organize and manage the meanings of the messages. In other words, the communication process begins with the creation and ends with the management of the meanings of messages. The concept of communication theory seems to be highly emphasized on information transmission. Claude Shanon, gave the theory of communication. His theory of communication discussed message transmission instead of information transmission (1948, pp. 379-423,623-656). Shanon used the term message instead of information. The reason to use the message as the key term to describe the communication was that he wanted to elaborate the concept of knowledge communication. Therefore, the Shanon’s theory of communication is also believed to be the theory of message. The message also includes the signs and symbols as the way to communicate. Most of the times the message and information are used interchangeably for the purpose of communications; they are similar but not identical. According to Rafael Capurro’s work on â€Å"Angelet ice, A Message Theory† (2003), the similarities that exist between message and information are as follows. Sender Dependent A message is believed to be sender dependent. The sender dependency refers to the asymmetric structure of communication, which may still require the receiver to ask for more information. For example, the sender may only send the indication to communicate through message and once the communication started, the receiver may need to ask for information to have detail knowledge for communication. Message/ Information Brings Something New This may refer to the similarity between the message and the information. The message and information are supposed to bring something new to the receiver. The receiver expects the communication may bring something relevant and new. Therefore, message and information both strike the mind of the receiver, if they are understandable. Coded/ Transmitted The message and information both are transmitted through coded forms. For exa mple in the cellular systems the message is coded in accordance with the transmission systems used. Therefore, the coded system for communication purpose exists for both message and information transmission. Expression A message and information are believed to be utterance that gives receiver selection through the mechanism, by which the message or information is released, but information may most of the time lack expression and communicate with

Writing assignment Essay Example | Topics and Well Written Essays - 750 words - 3

Writing assignment - Essay Example e offensive, its linguistic origin indicates that it is not fundamentally belligerent but merely a term used to describe a unique group of people who principally hunted for sustenance and still leading an aboriginal way of life. Eskimo language encompass a parlance continuum and is divided into two branches; Aleut and Eskimo. The Aleut dialect encompasses Pribilof, Unalaskan, Atkan, Unangan, Berring and Attuan while the eskimo dialect encompasses Inuit, Yuit and Yupik. Although our population has been fluctuating overtime due to climatic and technological changes, it currently lies at approximately 57,152, a figure that is higher as compared to other traditional hunting and gathering societies. We are very different from Indian Americans and cannot simply be designated ‘Indians transformed’ (Vakhtin, 1998). However, they are meticulously correlated with the Mongolian people from eastern Asia. Hunting was the main activity that provided sustenance to the Eskimo. However, the animals hunted varied significantly depending on the location of the group and the prevalent seasons; the animals include whales, caribou, fish, walrus, fox, birds, Dall sheep, polar and fractious bears. Hunters, especially whale hunters, subsisted in dome shaped ice cabins and dressed in hefty fur clothing (Kaplan, 1990). The hunters captured huge bowhead whales that could provide numerous tons of meat; meat that was stored in hovels in the frozen ground. Both men and women were involved in hunting for food and kept on constantly migrating following the movements of their prey. The apposite time to end a term’s whaling was agreed upon by captains of the crews, each crew consisted of 6 paddlers, a harpooners and a captain, a factor that bolstered cooperation and coordination and forestalled instances of hunger. When a whale was spotted, 4-8 hunters used umiak (a skin-covered open boat) to ventu re onto the water and capture the animal. Hunting was perceived to be an important strategy of

The counselling relationship Essay Example for Free

The counselling relationship Essay An anti-oppressive approach to counselling is essential to establish and maintain an affective working relationship between counsellors and clients. Clients must feel that they can trust their counsellor and that they may share any information without fear of judgment for their opinions, beliefs and values. Anti-oppressive practice enables clients to make informed choices surrounding the direction they wish their therapy journey to take. This essay will explore four areas that are critical to incorporate into professional counselling practice that contribute to the anti-oppressive approach to the therapeutic relationship. The ethical aspects of counselling, the importance of contracting, the importance of informed consent and the role of self-awareness will be examined. These four areas contribute to anti-oppressive practice by ensuring clients rights are respected and upheld and contribute to ensuring that the counselling relationship is beneficial and a useful part of the self-exploration You must Login to view the entire essay. If you are not a member yet, Sign Up for free  process.  Ethical guidelines are designed to encourage ethical behaviour and decision-making and they serve as safeguards to make sure high standards are adhered to by counsellors during the therapeutic sessions. They are guidelines which predominately refer to the rights and responsibilities of both the client and the counsellor during the therapeutic relationship. Ethics highlight the principles of appropriate conduct and behaviour to be adhered to by the counsellor. According to Summers (2011, p. 1), â€Å"ethical principles are the foundation of good human service practice† and it is essential that professionals understand ethical obligations and seek direction when they are unclear. Ethical principles are created to protect and prevent exploitation of clients, provide guidelines and to respect and offer protection for clients therefore contributing to anti-oppressive practice. Counseling level 3 Assignment For this assignment I will be critically evaluating the person centered model of counseling in relation to homosexual people. I will be considering the importance of anti-oppressive and  anti-discriminatory practice when working with this client group. The person centered model of counseling has its origins within Humanistic psychology and the phenomenological approach. Carl Rogers (1902-1987) was the founder of the person centered method and he drew his ideas from the humanistic and phenomenological approaches that are also associated with Abraham Maslow (1908-1970). The phenomenological approach is a philosophical assessment of the individual it was developed by Husserl (1975); the focus is on the subjective experience. The method involved requires the professional to suspend their assumptions and interpretation of the clients world. The client is viewed as a unique person and is facilitated to interpret and explore their own experiences and thoughts. Criticism of the use of phenomenology by Rogers as the basis for therapy is highlighted by Eysenck (1998), he states that it is a simplistic approach as much valuable information lies below the level of conscious awareness therefore the value of the subjective experience can be unreliable. Humanistic psychology has an optimistic perspective of human nature and the focus is on the whole person, the aim for the individual is to become what he/she is capable of becoming Rogers (1951) cited in Dryden et al (1989:10). This is also described as self-actualization, a term developed by Maslow to describe the motivating force enabling us to reach our full potential and peak experience. The humanistic approach stresses the importance of the individuals ability to direct their own life, and the counselor using the person centered method should allow the individual to choose their own pace of change and their own values and standards. However these values and beliefs may clash with those of the counselor’s and this can potentially lead to incongruity for e.g. a gay or lesbian person may be in a marriage and not disclose the fact that they are having homosexual feelings or relationship outside their marriage, to their heterosexual partner. In this situation it would be difficult for the counselor not to encourage the client to be honest with their spouse. Palmer and Laungani (1999) state that for effective communication it is essential that the counselor and client have a common set of assumptions and cultural ideology. There are 3 core conditions that Rogers identified, which are essential to a successful relationship between counselor and client, and for a therapeutic change to be facilitated; these core conditions are congruence or genuiness, the acceptance of the client with out judgment or  the provision of unconditional positive regard, and thirdly empathy. One of the core conditions that Rogers identifies is congruence or genuiness, congruence refers to the counselor’s capacity to be a real and genuine person in the counseling relationship. It also requires the counselor to be transparent so that the client can see straight through him/her. However this can be much more difficult than it seems on the surface. For e.g. if the client presents a situation where the professional does not agree with their action or beliefs, and may reserve these, it may be difficult to be honest in such a circumstance, and therefore maintain.

Patterns in River Flow Data

Patterns in River Flow Data Introduction The hydrologic response of a watershed is based on interactions between landscape characteristics and climatic characteristics input; as the soil property descriptors, geomorphologic descriptors, geologic descriptors and land use varies among different watersheds, the watersheds could respond very differently to precipitation (Mohamoud, 2004). The main aim of this coursework is to assess the impact of recent climate change on river flow; to uncover its significance in affecting river flow by analysing and comparing river flow records from National River Flow Archive, and to highlight and assess the differences in the hydrologic response to climate change of the three chosen rivers with contrasting characteristics, located in the UK. The three rivers chosen to be analysed includes the East Avon, the River Dove and the River Greta, all with natural catchments (natural to within 10% at Q95), with no known major artificial changes to the catchment that would influence the flow of the rivers, in order to attempt to focus solely on the effect of climate change (CEH, n.d.). The catchments examined all similar in size: 83000m2 for River Dove at Izaak Walton, located in central England; 86100m2 for Greta at Rutherford Bridge, located in north- east England; 85800m2 for East Avon at Upavon, located in south- west England (CEH, n.d.). Figure 1 showing the locations of the three gauging station on three separate maps of the UK (CEH, n.d.) Apart from the differences in location (figure 1.), there are also contrasting catchment characteristics. East Avon at Upavon predominantly consists of 64.5% of upper greensand and lower chalk of 27%; the remaining 8.5% consists of middle chalk, upper chalk, clay, as well as gault, plus river gravel and alluvium at the bottom of the valley (CEH, n.d.). In comparison, the Greta at Rutherford Bridge catchment is known to be steep, and it mainly consists of millstone grit (CEH, n.d.). Finally, in contrast, Dove at Izzak Walton is known to be long and narrow (CEH, n.d.). It mainly consists of mudstone, millstone grit and sandstone, with underlying carboniferous limestone forming the left hand watershed (CEH, n.d.). When looking at the catchment statistics in relation to the geology, East Avon’s catchment consists of 40.3% of high permeability bedrock, with 59.7% moderate permeability bedrock (CEH, n.d.). In contrast, Greta and Dove’s catchment consists of 100% of moderate p ermeability bedrock (CEH, n.d.). Besides the obvious difference in geology, the sites also vary differently in terms of their climatic characteristics, as shown in table 1.1, 1.2 1.3, and finally, land cover also varies among the three river catchments, as shown in table 2 (Met Office, n.d.; CEH, n.d.). Table 1.1 averages table showing climate data for the England SE Central S District, which covers period 1981-2010 (Met Office, n.d.) Table 1.2 averages table showing climate data for the Midlands District, which covers period 1981-2010(Met Office, n.d.) Table 1.3 averages table showing climate data for the England E NE District, which covers period 1981-2010(Met Office, n.d.) Table 2- Catchment statistics of Land Cover for each of the three catchments (CEH, n.d.). Methodology The river flow data obtained from these three gauging stations, between the year of 1973 and 2013 were used for analysis. In order to observe and identify flow pattern for each of the chosen sites, as well as to identify any change in the hydrological regime of the three rivers due to recent climate change at the sites, the three sets of river flow data from National River Flow Archive (NRFA) was first imported on to a spread sheet, where the flow measurement/ reading of each river were sorted in to order, according to the hydrological date of the measured flow. The data was then plotted as follows: Discharge vs. time Monthly flow vs. time A flow duration curve for flow frequency analysis Mean discharge vs. Hydrological year Julian date Next, visual inspection of the graphs was carried out, and the graphs produced for each river were directly compared to assess how seasonal and time – series patterns of flow differ across the three sites, and to determine whether all three sites showed the same pattern of flow through time. Results and Discussion In order illustrate the seasonal river flow pattern in the three catchments; figure 2 shows hydrographs for the three rivers. The location of these catchments is shown in figure 1, and characteristics are presented in the introduction. Upon inspecting the hydrographs, the following observations were made (points of reference are labelled as A on the hydrographs): East Avon’s mean discharge peaks at 1.17 m3s-1, on day 130 Greta’s mean discharge peaks at 6.81 m3s-1, on day 69 Dove’s mean discharge peaks at 3.35 m3s-1, on day 82 Figure 2-Hydrographs for three rivers, showing the mean discharge vs Hydrological year Julian date, plus a graph for comparison between the rivers’ mean discharge over days According to a study on UK river flow regimes, Hannaford et al. (2012) had suggested that UK river flow regimes can be considered temperate precipitation/evapotranspiration dominated, rather than snowmelt dominated. This means that the seasonal cycle will be mainly driven by evapotranspiration, leading to higher flows in winter and lower flows in summer, with the spring and autumn as transition seasons (Hannaford et al., 2012). When referring back to the peak discharge observations above, all three rivers conformed to the same general pattern, as day 82, 69 130- the days where the mean discharge has reached the peak for the three river all lies within the winter period, indicating that the flow will be high during winter days. Furthermore, the hydrographs also shows that, for all three rivers, the mean discharge appeared to be relatively low, and have all remained low between day 280 -320 for all three rivers (section B on the hydrographs), during the summer period. Figure 3- Monthly Discharge vs. Hydrological Year Date graph for all three rivers, with a secondary axis corresponding to the mean monthly discharge curve In terms of the consistency of the flow, figure 3 shows East Avon’s maximum minimum curve, and its mean curve look very similar- the curves are almost overlapping one another which shows a low fluctuation in flow. This suggests that the flow of the river is very consistent. In contrast, the other two rivers have less consistency. This can be observed when comparing the max, min and mean curve in Dove’s graph- the general shape of the curves are very similar to one another, yet there are a few points in the graph where there are some very noticeable differences, where the mean curve tend to have a greater fluctuation and peaks at higher discharge points compared to the other two curves, thus showing that it is generally consistent, but the consistency is lower compared to East Avon. Finally, Greta’s corresponding graph displays great fluctuation; although both max and mean curves are both similar and conforms to a similar pattern, it is clear that the min curve l ooks a lot flatter, with a pattern that is not very similar to the other two curves within the graph. This indicates that Greta’s consistency between years is relatively poor. Although all three river exhibit similar seasonal flow patterns, there are still notable difference in their response time. The occurrence of lag time and the difference between the response times of the three sites can be explained by the difference in the catchment’s physical characteristics and its underlying geology. When referring back to the peak discharge data, East Avon displays a lagged response, peaking at day 130, as opposed to peaking at days closer to 82 and 69 (days of which Dove and Greta reached its peak). This significant variation can caused by East Avon’s catchment geology, as it consists of 40.3% of high permeability bedrock, with 27% of chalk in the catchment, as opposed to 0% of high permeability bedrock in the other two catchments; the high permeability bedrock and the highly permeable chalk means that groundwater storage plays a significant role in effecting the runoff regime of the East Avon catchment, which lead to East Avon’s discharge peaking at around February, towards the end of the winter period, as opposed to peaking towards the start of the winter period, like the other two rivers have. Next, in order to illustrate the reason behind Greta’s earlier peak, in comparison to Dove’s later peak at day 82 (figure 2), the physical feature of both catchments must be examined in detail. Both catchments have an identical percentage of moderate permeability bed rock, and both are similar due to the fact that the catchments both consist of Millstone Grit. However, the topography are significant different between the two catchments. Since Greta’s catchment is significantly steeper when compared to the Dove’s catchment, as illustrated in figure 6 and table 3, Greta will have a more responsive regime compared to Dove due to a quick run- off rate of precipitation. This could also provide an explanation to why the mean discharge curve in the Greta hydrograph is subjected to a greater level of daily variation in comparison to the other two sites and their respective hydrographs. Figure 4- Flow duration curves for all three sites, with an additional graph (bottom graph) combing the Q* data (Discharge Ratio where Q*= Q/Q50) of three sites for comparison- note that scale of Q* is in Logarithmic Scale (Base:10) Figure 5- Flow duration curves for all three sites, with an additional graph (bottom graph) combing the Q* data (Discharge Ratio where Q*= Q/Q50) of three sites for comparison- the scale of Q* has been adjusted to go from 0-6 for comparison Additionally, figure 4 shows that Greta’s curve has the steepest slope, followed by Dove, and then by East Avon with the flattest slope. The observations mirrored those findings above precisely; Greta’s steepest slope indicates a highly variable river, and the flow mainly consists of direct runoff (Searcy, 1959). In contrast, curves with a flatter slope (e.g. East Avon with the flattest curve) which means they have a more constant flow, and can signify the existence of surface and/or groundwater storage – in East Avon’s case, highly permeable chalk acts as storage for water, which equalized the flow of the river (Searcy, 1959). Furthermore, in figure 5, the graph also provides information on the three rivers’ frequencies of very high flows and very low flows. When employing the parameters of Q*=5 for high flow, and Q*=0.2 for low, the curves shows that Greta exhibits a significantly lower proportion of time flow lower than the Q* of 5, whereas the c urves for Dove and East Avon are very similar, with a much higher proportion of time flow less than Q* of 5, meaning that high flows occurs a lot less frequently in Dove Avon in comparison to Greta. In terms of low flow, three rivers are all dissimilar in their frequency of low flow. Greta’s proportion of flow less than 0.5 is ≈0.02, whilst Dove’s proportion is ≈0.16, with East Avon’s proportion is ≈0.34. East Avon’s higher proportion of time flow less than 0.5 means that the occurrence of low flow is more frequent in East Avon, and in comparison, Dove has got a relatively lower frequency of low flow, and Greta with the lowest frequency of low flow over the years within the sample period. Table 3- Elevation data for Greta and Dove’s catchment (CEH, 2014) Figure 6-Elevation Map of England. This map shows the significant difference in elevation between the North of England and the South of England. (Windpower Program, n.d) As seen in figure 7, the flows of all three rivers do seem to conform to a similar pattern over time, with no significant changes in the temporal pattern and frequencies of flood/ droughts. However, upon further inspection, the graph shows that the magnitude of the floods for all three rivers had increased over time; the high flow peaks have seemed to be higher in more recent years. This phenomenon can possibly be explained by global climate change; as global temperature increase, this leads to an increase in water vaporing the atmosphere. As suggested by Milly et al. (2002 cited Das et al, 2013), Kunkel et al. (2013 cited Das et al., 2013) and Trenberth (1999 cited Das et al, 2013), storms are likely to yield more extreme peak precipitation rates, which can lead to more intense floods around the globe (Groisman et al., 2005 cited Das et al, 2013). However, although the trend identified above is consistent with climate change, it is also consistent with variability driven North Atlan tic Oscillation (Hannaford, 2013). With the significant knowledge gap in the understanding of long term multi-decadal variability in flow driven by NAO, along with the lack of long term flow data available for this report, it will be premature to attribute specific steam flow trends to anthropogenic climate change (Hannaford, 2013). Figure 7- Hydrograph showing change in river discharge between 1973- 2012 Summary Conclusion In conclusion, river flow regimes of the three assessed rivers are heavily dependent on catchment geological characteristics and climate. Climate plays a major role in effecting the flow, as the relatively temperate climate in England meant that the dominant factor in effecting flow regimes are precipitation/ evapotranspiration, which leads to the occurrence in flow variation between seasons as rate of evapotranspiration varies. In relation to climate, among the three rivers, there were observed changes in peak flow and flood magnitude over time, which global climate change might be responsible for, as it can lead to precipitation extremes, which in turns lead to more run-off and higher river flow. Besides that, variation in geology also contributes to the difference in hydrology of each river, as groundwater storage can affect the rate of run- off, which in turns affects the flow and the response of the three rivers. Finally, anthropogenic influences can affect flow regime of rivers (Schneider et al, 2013). However, there is no significant evidence to show how these had modified the flow of the rivers. Reference Centre for Ecology Hydrology (n.d) 43014- East Avon at Upavon. National River Flow Archive. [Map , Catchment Description Flow Record] Retrieved from http://www.ceh.ac.uk/data/nrfa/data/peakflow.html?43014 (Last accessed on 07/11/2014) Centre for Ecology Hydrology (n.d) 28046 Dove at Izaak Walton.. National River Flow Archive. [Map , Catchment Description Flow Record] Retrieved from http://www.ceh.ac.uk/data/nrfa/data/peakflow.html?28046 (Last accessed on 07/11/2014) Centre for Ecology Hydrology (n.d) 25006 Greta at Rutherford Bridge. National River Flow Archive. [Map , Catchment Description Flow Record] Retrieved from http://www.ceh.ac.uk/data/nrfa/data/peakflow.html?25006 (Last accessed on 07/11/2014) Groisman, P.Y.; Knight, R.W.; Easterling, D.R.; Karl, T.R.; Hegerl, G. ; Razuvaev, V.A.N. (2005) Trends in intense precipitation in the climate record. Journal of Climate, vol 18, no. 9, 1326-1350. Cited in Das, T; Maurer, E. P.; Pierce, D. W.; Dettinger, M.D.; Cayan, D.R. (2013) Increases in flood magnitudes in California under warming climates.Journal of Hydrology501, 101-110. Hannaford, J (2013) Observed long- term changes in Uk river flow patterns: a review. A climate change Report car for water. Hannaford, J.; Buys, G. (2012) Trends in seasonal river flow regimes in the UK. Journal of Hydrology, 475. 158-174. Kunkel, K.E.; Karl, T.R.; Easterling, D.R.; Redmond, K.; Young, J.; Yin, X, Hennon, P. (2013) Probable maximum precipitation (PMP) and climate change Geophys. Res. Lett., 40 Cited in Das, T; Maurer, E. P.; Pierce, D. W.; Dettinger, M.D.; Cayan, D.R. (2013) Increases in flood magnitudes in California under warming climates.Journal of Hydrology501, 101-110. Table 1. Met Office (no date) UK climate – District England SE Central S [Table/ Data] Retrieved from http://www.metoffice.gov.uk/public/weather/climate/gcneyctf3 (Last accessed on 08/11/2014) Table 1. Met Office (no date) UK climate District Midlands [Table/ Data] Retrieved from http://www.metoffice.gov.uk/public/weather/climate/gcqbgpgqh (Last accessed on 08/11/2014) Table 1. Met Office (no date) UK climate District England E NE [Table/ Data] Retrieved from http://www.metoffice.gov.uk/public/weather/climate/gcwzegx04 (Last accessed on 08/11/2014) Milly, P.C.D.; Wetherald, R. T.; Dunne, K.A.; Delworth T.L. (2001) Increasing risk of great floods in a changing climate Nature, 415 (2002), pp. 514–517. Cited in Das, T; Maurer, E. P.; Pierce, D. W.; Dettinger, M.D.; Cayan, D.R. (2013) Increases in flood magnitudes in California under warming climates.Journal of Hydrology501, 101-110. Mohamoud, Y. (2004) Comparison of hydrologic responses at different watershed scales: EPA Report EPA/600/R-04/103 Searcy, J .K . (1959), Flow-duration curves : U .S . Geological Survey Water-Supply Paper 1542-A Schneider,C.; Laizà ©,C.L.R.; Acreman,M.C.; Flà ¶rke,M. (2013) How will climate change modify river flow regimes in Europe?, Hydrol. Earth Syst. Sci., 17, 325-339 Trenberth, K.E. (1999) Conceptual framework for changes of extremes of the hydrological cycle with climate change Climate Change, 42 (1999), pp. 327–339. Cited in Das, T; Maurer, E. P.; Pierce, D. W.; Dettinger, M.D.; Cayan, D.R. (2013) Increases in flood magnitudes in California under warming climates.Journal of Hydrology501, 101-110. Figure 6. Windpower Program (no date) Estimating mean wind speed. [Map] Retrieved from http://www.wind-power-program.com/windestimates.htm (Last accessed on 08/11/2014)

The Intent Behind the Enuma Elish (Creation Epic) Essay -- Enuma Elish

The Intent Behind the Enuma Elish  Ã‚     Ã‚  Ã‚   The Enuma Elish, often known as The Creation Epic, is often considered the primary source of Mesopotamian cosmology. However, to view the Enuma Elish as a cosmological myth obscures the true intent of the epicà ­s author. The cosmological elements of the Enuma Elish are secondary to the authorà ­s effort to explain the supremacy of Marduk, to justify absolute oriental monarchy, and to defend Babylon as the axis mundi. The Enuma Elish was composed in Babylonin the early second millennium B.C.E. The decay of Sumerian civilization allowed the Old-Babylonian Empire to become the cultural and political center of Mesopotamia. Babylon was governed by absolute and despotic kings capable of wielding enough power to ensure the continued existence of massive building projects and large-scale irrigation. The harsh environment of Mesopotamia often necessitated the absolute rule by a king powerful enough to command the resources required to maintain civilization. The poet behind the Enuma Elish sought to justify the position and government of Ba...

Children of Heaven Review

Children of Heaven This movie made me very thankful for everything I have in my life, including my shoes. I found it sad that All could not Just speak up for himself. If All would have asked the man working the grocery store about the shoes, then he might not go to all the trouble in the first place. I found it sad that the children had to work, and never got to play. The quality of life for this family bothered me deeply, and it made me blessed for the childhood that I had. The kids in this movie worked almost as servants to the adults, maintained pristine manors, and showed great perseverance.I noticed most of the adults in the movie were very strict, stern, and seemed like they were not afraid to beat a child. All made some of the highest grades in his class despite his hardships, he was a responsible kid. I Just don't understand why he did not speak up about the shoes to his teacher, principle, or coach. It was sad to see kids having to stick together, and share a pair of shoes t o prevent one of them from getting a beating. All's sister should have asked the other girl wearing her shoes, where she got them.The girl may have Just given them to her in exchange for the en, or when she received her new shoes. This movie was one hardship after another, heartbreaking for me to watch. It makes me want to donate shoes for children who may not have any at all. It was sad to see people In the movie live In lavish mansion, and then compare It to All's home. All's dad was paid very good for his gardening work, this money would be a precious asset to his family. When the man at the mosque gave All's dad the tools, this showed how the Islamic community supported the others In need. Overall It seemed Like a rough situation to me.

Junior Deputy

Derick Krones Junior Deputy During Junior Deputy this year, I learned that smoking is bad for your health. And, alcohol is bad for you, too. Smoking causes tar to build up in your lungs and can lead to cancer. I know cancer is a bad disease because I have lost my grandpa and grandma to cancer. Alcohol kills brain cells. It is important to learn and if you do not have all your brain cells, you will not be as smart which means you will not do as well in life.I liked getting to wear the drunk goggles in Junior Deputy. It was fun to see how it makes you feel to try to walk with the goggles on. It was a nice break in the day to get to learn about other things in Junior Deputy at school rather than math, science, communication arts, and social studies. The part of Junior Deputy I liked the least was how long the pre/post tests were to take. There were hard questions on the test and it took time to think about the answers.I know you have to take tests to see what you do and do not know, but it was my least favorite part of Junior Deputy. Actually getting to wear the drunk goggles made you feel what it was like to be drunk so you know you do not want to drink. Junior Deputy taught me to make the right choices and not do drugs,alcohol or smoke. It is important to stay healthy and do your best in life. Junior Deputy helps explain how to make good choices and to stay healthy.