Counseling African Americans Essay Example for Free

Counseling African Americans Essay Sue and Sue’s Chapter 14 Counseling African Americans spends a great deal of effort exploring cultural particulars and corresponding clinical implications while working with African Americans; factors such as family dynamics, educational orientation, spirituality, and the pressures and stress of racism and marginalization. This offered me perspective through a lens much broader than my own somewhat narrow, predominantly white, and fairly privileged way of relating to the world. Before understanding culturally appropriate interventions, one must have an understanding of the cultural context or the cultural word of an individual. For me, this first means that differences must be noted, either literally in relationship with the African American client or simply as a clinical observation I make on my own. Of course the difference in the two will depend on the client, context, and general relevancy in the moment. In my own experience, noting racial difference aloud with a client has been most helpful in that it gives permission for the potentially â€Å"taboo† topic of race and differences to be considered, brought into the space at a later time, and even into the forefront of consciousness. Apart from the explicit therapeutic relationship, noting difference is a personal reminder that I am no expert on anyone’s experience but my own, I may make mistakes (and probably will), I should steer clear of assumptions, it’s ok to be curious, and to do my homework. Once a general understanding of differences is established, then one can begin to consider appropriate therapeutic interventions. Let’s take the issue of racism and discrimination; the byproduct of these atrocities oftentimes manifests as defense and survival mechanisms in Black Americans. Which can lead to a general mistrust or as it’s stated (by Sue and Sue) a â€Å"healthy cultural paranoia†, as a way of coping. This mistrust can be of individuals, entire races of people, the government, social service providers†¦ With this in mind, it’s important to determine what the client’s feelings and understandings about therapy are. To touch base and explain what kind of therapy I engage in, how it can be helpful to them, and what can be expected of our time together. Hopefully this will help to assuage uneasy feelings of fear of the unknown or mistrust, as well as set up a foundation for a healthy therapeutic alliance. Although Sue and Sue’s Afrocentric perspective can be helpful it can also simultaneously be viewed as reductive. It’s important not to discount individual differences by universalizing traits of African Americans. Self cannot be defined as a unitary concept evolving from a single defining variable, such as race or gender (Williams, 1999). For instance, not all women are nurturing, caring, and relational. Similarly, not all African Americans possess an African ethos of communalism or spirituality. Race, class, sexual orientation, and gender are all complex interactive components that make up the self. To approach a client through the lens of only one of these variables, means potentially silencing a central component of their identity. Additionally, it is also necessary to consider an internal state without regard to the social demands of each variable. Collectively, these considerations can aide to a more holistic view when working with African American clients. Part Two After spending a year in practicum at the SF county jail, I feel as though I’ve had a fairly decent introduction to working with African American females. When I began practicum I had had very little training in diversity or cross-cultural counseling. Turns out that a year in the jail was one large training in diversity and cross-cultural counseling! Now I’m able to pin my personal experience against the readings and gauge my success as a culturally competent therapist. When assessing my strengths, I find that I possess a keen and tremendously empathic understanding of how the stress of racism, sexism, and oppression can manifest in African American women. Oftentimes the byproduct of this stress is what brings the individual to jail. As a clinician, I can confidently say that I am able to enter the therapeutic relationship with a greater capacity for empathy because of this understanding and build a strong alliance as an ally as well as a therapist. I’m not afraid to make mistakes and have no attachment to being â€Å"right†; these qualities will only support me as a clinician. In addition, my upfront demeanor and willingness to self-disclose have had a remarkable impact on the therapeutic relationship. My empathy is strongly with women and their plight of identifying and addressing all the â€Å"isms† that stand between them and equality, wholeness, and health. Frequently, those â€Å"isms† are at the hands of men and I certainly have a bias towards this, and towards men in general. It’s no accident that I spent an entire year of practicum working solely with women; although it wasn’t a conscious choice, I believe on some level I chose not to work with men. I have incredible biases towards men as perpetrators and oppressors and men and their privilege, African American men as well as Caucasian. These biases keep me terrified at the thought of working with male clients. I imagine heaps and heaps of countertransference between male clients and myself; countertransference that is full of pain and rage. I’m not sure that I have much to offer men inside the therapeutic space. I don’t believe this to be my â€Å"final answer†, I just know that I have some work to do around my relationship with men before I make the leap of working with them in such sacred space. Essentially, it all comes down to two core qualities- and they are humility and flexibility; humility in all that I think I know and the flexibility to shift or discard that knowledge. My experience of working with, knowing, and reading about African American culture, difference, and oppression may or may not serve me as a therapist at any given moment. What works for and makes sense in the context of Client A, may not be so for Client B, and vise versa. Although it is crucial to have fundamental knowledge of the legacy of oppression against African American people and to consider factors such as interdependence, collectivism, and emotional vitality as presumed long- standing black personality traits, I must also be able to draw connections between those factors and the individual experience- much like the womanist techniques mentioned in Carmen Braun Williams’ article African American Women, Afrocentrism and Feminism: Implications for Therapy. As a therapist, I am responsible for guiding and supporting the client in making the shift from object to subject; transferring ownership of self from one whose self is externally determined to one who is self- determining (Freire, 1990). And practice practice practice, with an open heart, ears, and mind. References Braun Williams, C. (1999). African American women, afrocentrism and feminism: Implications for therapy. Women Therapy, Vol. 22(4) 1999. Freire, P. (1990). Pedagogy of the oppressed. New York: Continuum. Sue, D. Sue, D. (2008). Counseling the culturally diverse: Theory and practice, Chapter 14.

Arthur Conan Doyle reveals Holmes Essay Example for Free

Arthur Conan Doyle reveals Holmes Essay Examine how Arthur Conan Doyle reveals Holmes character and his relationship with the police. Sherlock Holmes was created by Conan-Doyle in 1887. When Arthur Conan-Doyles character, Sherlock Holmes surfaced, London in the era of Queen Victoria was an intriguing place to live. At this time, Victorian people feared crime greatly due to the prostitution, drug abuse but mainly an infamous murderer, Jack the ripper. This brutal murderer was loose on the streets of London attacking vulnerable women savagely with a sharp, long-bladed weapon, this panicked many women due to the fact that the polices methods were seen as inefficient; therefore would rarely solve the cases by catching the ruthless villains. Many Victorians had little if no faith for the police in London, as they did not appear to be protecting the public. On the other hand, Holmes, who is an excellent detective, is well known for his use of logic and observational understanding to unravel complicated cases. He described himself as a consulting detective an expert who is brought in to cases that have proven too difficult for other investigators; we are told that he is often able to solve a problem without leaving his home. This is prodigious as Holmes was actually an amateur detective, not a member of the London police force. The purpose of this essay is therefore to show Holmes character and his relationship with the police. In some cases Holmes breaks the law, in others he does not. One example of when he doesnt is in Silver Blaze; Sherlock Holmes and Dr Watson pay a visit to their old friends the Baskervilles and find themselves in the middle of a mystery involving a missing horse and its dead trainer. Doyle reveals through his writing that Holmess character is very egotistical. This is shown many times throughout the story: I follow my own methods and tell as much or as little as I choose. Here, Holmes is being very demanding showing that he does not have much respect for other people; this is very shocking as Watson is not only a companion but most importantly a friend too. I think Doyle does this to ensure Holmes is referred to as a very dominant character in addition to being arrogant and making people feel small and unimportant. Doyle through his use of language creates Holmess character to have a greater intelligence over the police. Doyle uses sarcasm to show this: Inspector Gregory, to whom the case has been committed, is a very competent officer, were he but gifted with the imagination he might rise to great heights during his profession. This also shows that Holmes has no faith in the inspector in solving the case as Doyle uses the word might to show the sarcasm therefore implying that he has no hope for the police in cracking the mystery. This same egotistical behavior towards the police is also repeated later on when Holmes says See the value of imagination; it is the one quality which Gregory lacks. As this is repeated in his writing it reveals that Doyle is trying to emphasize Holmess views of the police as being incompetent. Furthermore, Holmes relationship with the police is very argumentative. Holmes is always mocking the police by acting witty. This is shown when Holmes says The inspector here has done all that he could possibly be suggested; but I wish to leave no stone unturned in trying to avenge poor Straker, and in recovering my horse. Doyle uses this sarcastic language to reveal Holmes true disrespectful manner and arrogance towards the police. In addition to that Holmes finds great pleasure in finding the clues way before the police are anywhere near. When the inspector says I cannot think how I came to overlook it, Holmes replies I only saw it because I was looking for it! Doyle, with the use of that language implies that Holmes was actually observing the murder scene, whereas the inspector did not think to do that. To Holmes, using his logic and observational understanding is general common sense, this is one of the reasons how Holmes makes the detectives feel incapable of their job in which they specialize in.

Solar Radiation Climate

Solar Radiation Climate Incoming solar radiation is a key component of the Earths Climatology. From maintaining the Earths climate, living forms are able to survive as Hulstrom (1989, p.1) points out solar radiation is a key principle for sustaining life and as a renewable source of energy it can prevent exploitation of the non-renewable sources e.g. oil. Depending on the landscape, solar radiation can create varies microclimates as explained by Chen, Saunders, Crow, Naiman, Brosofske, Mroz, Brookshire, and Franklin (1999, p.288) where a canopy of vegetation will absorb the short-wave radiation, increasing the sensitivity of the ground surface temperatures below. Chen, Hall and Liou (2006, p.1) state it is the spatial and temporal elements of incoming surface solar radiation that can determine many landscape scale processes. An area of interest where incoming radiation can create or trigger several processes and climates is mountainous terrain. Even though the total surface area of mountain systems around the world is a very small percentage of the total Earth surface, they can still create an input to the climate system experienced globally. The intensity of solar radiation reached at the surface plays a vital role in mountain climates. It is variations in elevation, slope, aspect, and shadowing that can affect the amount of radiation received at the surface (Dubayah, 1994, p.627, White, Mottershead Harrison, 1994, p. 207, and Chen et al., 2006, p. 1). This study will focus on incoming radiation and analyse the extent to which each of the factors above affect incoming radiation received upon uneven terrain. The focus will be on incoming radiation because, as Duguay points out (1993, p.339) any progress in the determination of surface radiation in mountainous terrain has to begin with incoming shortwave radiation. Another aspect that this study will approach is the extent to which vegetation canopy cover can intercept radiation before reaching the Earths surface. A study created by Mariscal, Orgaz, and Villaobos (2000, p.183) states the importance of measuring radiation received at the surface for purposes of photosynthesis and proposed 70% (p.184) of solar radiation can be intercepted by canopy cover. This study will be analysing the amount of radiation received beneath a forest canopy to aid the understanding between incoming radiation and vegetation cover. This study is designed to examine the intensity of incoming solar radiation received within Cwm Llysiog valley (51Ëš49N 3Ëš25W), located in the Brecon Beacons in South- East Wales. A Coniferous tree forest, located at the Southern end of the valley provides a canopy of vegetation to record radiation measurements beneath. The northern part of the valley is mostly grasslands and shrubs, providing a transect to measure radiation without vegetation inception. Across Britain in the 1970s Harding (1979,p.161) discovered there was very few actual observations of radiation reached on the surface across the uplands due to there be a lack of â€Å"robust automatic instruments, capable of withstanding the extremes of an upland environment†. A problem that was crossed in this study was the availability of automatic instruments for recording solar radiation, disallowing me to achieve the quantity of radiation data required. Literature Review Radiation Radiation is the main input to the black-box closed- system, planet Earth, received from the Sun, in the form of electromagnetic radiation waves ranging from 0.25-3.5 micrometres (Oke, 1987, p.8-9). These waves travel towards the Earth away from the source, at a speed of 299,800kilometers/second (Strobel, 2001). There is a large distance between the Sun and the Earth, resulting in only 0.002% of the total radiation secreted from the Sun is an input to the Earths system. The ozone is an important component for protecting the Earths atmosphere from captivating harmful amounts of solar radiation, by absorbing the majority of the radiation around wavelengths of 300mm. Each different wavelength is absorbed at different points of the Earths atmosphere. Shorter wavelength UV radiation and solar energetic particles are deposited mainly above the troposphere, where gases such as O2 (Oxygen) act as an absorber of the UV radiation (Lean Rind, 1998, p. 3072). Visible light is what can be seen b y the eye and is centred on wavelengths of about 0.5 µm (McIlveen, 1998, p.244). Acra et al. (1990), researched into how atmospheric interventions can cause this change in wavelength and how different colours can relate to the wavelength Blue skies are present when the degree of scattering is sufficiently high within the blue region of the spectrum (McVeigh, 1977, cited by Acra et al., 1990). The intensity of radiation reaching the Earth surface as a single value is 1353W/m5 and continues to be relatively constant (Rich, Hetrick Saving, 1995, p.3). Nunez (1980, p. 173) expresses the need for reliable knowledge of solar and terrestrial radiation at the Earths surface and looks into approaches that concentrate on the radiation fluxes over a unit of horizontal area, and some index of atmospheric turbidity to derive a climatic radiation model. It is analysed that in most of these cases the radiation fluxes at ground level are assumed to be non-related to the properties of the receiving surface. It would only be the reflected and outgoing terrestrial radiation that the surface would initiate changes (Nunez, 1980, p.173.). The surface properties aspect and gradient will be measured to analyse whether Nunez (1980) has the right idea. The receiving of energy emitted by the Sun, at the Earth surface is controlled by three sets of factors. Spatial and temporal variation in insolation at specific sites is predictable from basic geometric principles, and can cause variation in climatic conditions across local topography. Insolation is commonly expressed as the average irradiance and is a function of latitude, day of year, time of day, slope and aspect of the receiving surface, and horizon obstruction (Rich, Hetrick Saving, 1995, p.1). At different times throughout the day the Suns height appears to change, and is at its highest in around noon. At this point the sun rays have the least distance to travel through the atmosphere and UVB are at their highest. In the early morning and late afternoon the Suns rays pass through the atmosphere at an angle resulting in a reduction in intensity. The second is the scattering and absorption of incoming radiation within the atmosphere, through gases, aerosols and cloud particles. This results in three forms of incoming radiation received on inclined surfaces, including: direct (beam) radiation, which is the part of solar radiation that is not absorbed or scattered by the atmosphere and has a direct path from the sun to the surface (Allen, Trezza Tasumi, 2006, p.55). This study will be focusing on the factors influencing radiation once its nearer to the surface. Mathematical models have been used to estimate solar radiation. Alam, Saha, Chowdhury, Saifuzzaman and Rahman (2005) present a mathematical model to simulate the availability of solar radiation in Bangladesh using system dynamics methodology. describes the formulation of the mathematical model used for the study. It takes into account slope angles, atmospheric absorption and scattering by diffused radiation, and the amount of extraterrestrial radiation that would be received. One problem with these models is that the outcomes are only predictions of radiation intensity. Surface based measurements avoid estimations from modelling on radiation, but are more labour intensive. Holst, Rost and Mayer (2005) used both surface based measurements and empirical modelling, because it was recognised that modelling did not reach a standard of accuracy on its own. For this study field based measurements were carried out over the period of two days to measure the intensity of radiation received at the surface. Mountain Climates Observations made in mountains are very important for the understanding of solar radiation and solar constant. Data collection on mountains and their climates over many years has been seen to be quite problematic. The areas tend to be remote from major centres of human activity, have limited physical access, difficult to install and maintain weather stations, and can experience extreme climates. Recent studies have used satellite remote sensing and digital terrain data for analysing mountain climates (Duguay, 1994, Haefner, Seidel, Ehrler, 1997, Dubayah, 1994). Digital and satellite imagery has confirmed many climatic conditions that have emerged over thousands of years from the analysis of synoptic data, and has increased the understanding of cloud cover influencing radiation at the surface. Geographical controls that vary the intensity of solar radiation reaching the surface are Latitude and Altitude. Barry (1992, p.18) explains that latitude has a great influence on mountain climates with solar radiation and temperature decreasing with increasing latitudes. The Ozone becomes increasingly rich with altitude resulting in the mid and higher altitude regions reaching less radiation because the sun is lower in the sky and therefore the rays must travel a greater distance through the Ozone. This gives reason to why Holland and Steyn (1975, p.181) discovered aspect as being an important parameter in the mid- latitudes. Barry (1992, p. 77) also pronounces slope effects changes with latitude. Around latitudes of 40 ºN in the northern hemisphere, north facing slopes receive a greater duration of direct radiation throughout the day compared to south facing slopes (Barry, 1992, p.77). The Brecon Beacons is 51ËšN so the duration of direct radiation will be shorter on the north facing slope, but the differences between intensities on each slope will be compared for the duration of the day. Cloud cover is recognised as being a limiting parameter of incoming radiation (Arking Childs, 1984, Rieland Stuhlmann, 1992) and a main contributor to diffuse radiation. This research believes cloud cover plays a vital role in scattering and preventing direct solar radiation reaching the Earths surface. Rumney (1968, p. 89) exemplifies the fact that the amount of radiation and sunshine from one year to another would be the same were it not for variable amounts of cloud cover. Cloud cover is thought to cause â€Å"back scattering, and can reduce the solar power reaching the underlying surface by as much as 90%,† (McIlveen, 1998, p.244). Fritz (1951, cited by Garnier Ohmura, 1968, p.798) noted that cloudless skies are appropriate in climate studies to limit the atmospheric tranmissivity influence on incoming radiation. Spatial characteristics of mountainous terrain such as orientation, angle, vegetation cover and shadowing from neighbouring slopes have been the subject of many observational and analytical studies, Duguay (1993) by modelling downward fluxes (pp.341- 347), Churchill (1982) with aspect influence on hill slope process, Holland and Steyn (1975), vegetation response to angle and aspect, and Wendler and Ishikawa (1974) with the effects on slope and exposure on solar radiation. Figure 3 illustrates the three sources of illumination that can occur on slopes. Variability in slope angle can lead to strong local gradients in solar radiation (Ralph, 1994, p.627 Kumar, Skidmore, Knowles, 1997, 467). Holland and Steyn (1975, p.181) found that the differences in incident solar radiation in mountainous areas of different slopes and aspects were maximum in the mid-latitudes and the least in equatorial and polar regions. The mid-latitudes in the northern hemisphere are closer to the Sun in July (su mmer solstice) resulting in greater amount of radiation received on slopes north facing slopes receive more radiation in early hours (0600hrs) of the day and later hours in the evening (1800hrs) compared to the south facing slopes. The southern facing slopes, of an angle greater than 55 º receives a greater intensity of radiation at midday, where the north facing slopes are not illuminated, as displayed in figure 4. Barry (1992, p. 76) acknowledges the fact that â€Å"South- facing slopes at the equinoxes show a symmetrical diurnal pattern,† from the time the sun rises in the east, limiting the intensity shining on south facing slopes with increasing steepness in the early hours of the day. By comparing the north west and south east facing slopes through the duration of a day, I will be able to analyse whether the patterns found within research have correlated with my own findings. It shows the steep south facing slopes reach a greater amount of radiation compared to average south facing slopes, but it is clear the greatest difference between aspects is when the sun is either highest in June, or lowest in December in the sky (Ralph, 1994, p.633). Surface temperature is a useful parameter to estimate the amount of radiation received on varying slope aspects. Safanda (1999, p.367) expresses that the north facing slopes in the middle latitudes in the northern hemisphere are a few  ºC colder at similar elevations as on South-facing slope surfaces. Reason for this is that less solar radiation falls on a unit area of the slope surface (Safanda, 1999, p.367). By recording near surface temperatures for the two valley transects, it will allow me to correlate the differences between two aspects by comparing temperatures at the same elevation. Shadowing from neighbouring slopes or valleys is thought to be a â€Å"spatio-temporal function† because it depends on both topography and solar geometry (Ranzi Rosso, 1995, p.464). Shadowing, introduced by Ranzi and Rosso (1995, p. 468) for a catchment basin that has shadowing occurring across the surface from projected horizons within the catchment area, is ‘Self Shadowing. This should only occur in a valley with east and west facing slopes as the sun will rise in the east projecting a shadow onto the east facing slope if elevation is great enough. By knowing the different slope angles and orientations of the Cwm Llysiog valley, the effect of exposure and shadowing can be assessed. The McCall Glacier (Alaska) was studied (Wendler Ishikawa, 1974) for the effect of slope, exposure and mountain screening on solar radiation and discovered that the screening effect of mountains was much more important than the northerly exposure reducing radiation reaching the glacier. It is not only slope shadowing that could limit the intensity of radiation received at the surface in the Cwm Llysiog valley, vegetation cover will also reflect radiation. Cannell, Milne, Sheppard, and Unsworth (1987), and Bartelink (1998) explain with increasing canopy cover, radiation interception is increased resulting in a decrease of radiation at the surface (Jordan, 1969, p.663). Vegetation cover is thought to be the greatest limiting factor in the Vegetated valley and will be compared to the non- vegetated valley radiation readings to verify this prediction. 2. Aims and Objectives The aim of this study is to investigate how the variability in slope, aspect and shadowing comprise to create a changing affect on the gradients of incoming radiation in forested and non- forested valleys. This will be assessed by comparing north and south facing slopes within a South Wales valley with forested and non-forested slopes in the summer with cloudless skies. Below is each Hypothesis set before measurements were taken and research that backups the reasoning for the hypothesis. Hypothesis A: The vegetated slopes will decrease the intensity of solar radiation received at the surface compared to the non- vegetated slopes. This will reflect in the surface temperature, with an increase in solar radiation resulting in an increase in temperature. Safanda (1999, p.367) concluded that north facing slopes achieve a low temperature then south facing slopes. Bartelink (1998) is one of many that has proven vegetation cover will decrease the intensity of radiation received at the surface. Hypothesis B: The intensity of solar radiation will be greater on the south east facing slopes compared to the total solar radiation received on the north west facing slopes. The orientation of slope faces will be the most influential factor on incoming solar radiation. White et al. (1994, p.207) describes the azimuth (orientation of the surface) as being the most influential component in the intensity of solar radiation received at the surface. It is stated that a southerly facing aspect will receive a greater intensity of radiation at the surface compared to a northerly aspect, which might not receive any at all. On the other hand Whiteman, Allwine, Fritschen, Orgill, and Simpson (1988) compared radiation components from five stations situated in a single valley during September of 1984 and concluded that slope faces have distinctly different diurnal courses of radiation. Slopes facing north east, experience downward solar fluxes directly after the slope is illuminated during sunrise but the fluxes become weaker during the afternoon as a result sunset. In contrast the south west facing slopes, has weaker direct radiation in the morning but attains a strong peak in the early afternoon. This view is slightly different to Whites et al. theory on aspect. Hypothesis C: Slope angle will have a less influential impact on radiation intensity compared to slope aspect. It is thought with an increase in gradients the intensity of solar radiation will decrease and become less direct. White et al. (1994, p.208) explains that these two factors (aspect and gradient) combined have a greater effect on the amount of direct radiation on north facing slopes in the northern hemisphere. It is made clear, with increasing slope angles, there is a decrease in solar intensity directed at the north facing aspect. Dubayah (1994, p. 634) displays a time series of monthly incoming solar radiation for different slope terrains within the Rio Grande River Basin. The study shows steep south facing slopes receive around 140W/m2 more radiation than a steep north-facing slope in July. The differences displayed in these findings are thought to be due to slope gradient. Hypothesis D: Within the forested valley, the vegetation cover will cause a great deal of shadowing on the surface decreasing solar radiation received at the surface. The greatest shadowing in the non- vegetated valley will occur in the lower sites, near the valley floor where the surrounding horizons are at a higher elevation, decreasing the sky view factor. Ranzi and Rossos (1995, p.464) study in a drainage basin realised that shadowing occurs at low altitudes, as the â€Å"direct radiation is less important in relation to the other radiative fluxes, i.e. diffuse irradiance from the sky and direct and diffused irradiance reflected from nearby terrain†. This means any horizon at a higher elevation then the site being studied will reduce the intensity of solar radiation received at the particular site. White et al. (1989, p.419) agrees with Ranzi and Rosso views where changes in orientation or positioning on a slope, affects the view of surrounding topography, thus affecting receipt of reflected radiation. Jordan (1969, p. 663) explains The greater the vegetation cover the greater the greater the difference in radiation above and below the canopy. Null Hypothesis: There will be no correlation between radiation received at the surface on the vegetated and non- vegetated slopes. Factor such as slope orientation, slope angle and shadowing will not influence the amount of radiation reached at the surface. Elevation The relationship between direct radiation and surface elevation is complex and depends on the atmospheric conditions such as cloud cover. With an increase in surface elevation an increase in direct solar radiation will occur, because the solar path through the atmosphere is shortened. This only tends to occur under cloudless skies. Batlles, Bosch, Tovar-Pescador, Martinez-Durban, Ortega and Miralles (2008, p.341) studied atmospheric parameters to estimate radiation in areas of complex topography and came to the conclusion that only the global radiation changes with increase of 1000m in elevation. It was thought that in the current microclimate being studied, elevation variations are less significant than other topographic variables, such as shadowing affects. Measurements recorded in the field for this study only reached 40m up the slope, meaning the effect of elevation on radiation would be very little. Due to these findings elevation will not be included in this study as a control. Objectives The main objective is to examine any correlation between slope aspect, slope angle, shadowing and vegetation cover and to analyse the influence they might have on the intensity of incoming solar radiation reaching the surface. To assess these factors affecting incoming radiation on sloping terrain, this study will test the hypotheses determined by studying the previous research. The hypotheses will be tested by recording a set of incoming solar radiation readings along a transect across a valley over the period of a day. It was difficult to locate a valley with north and south facing slopes in Wales. The Cwm Llysiog presents north west and south east aspects. The increase in elevation will be measured to display differences in radiation at the base of the valley and the valley slopes. The gradient is also important to analyse the correlation between slopes and radiation. A set of temperature results at the nine sites along the transect will determine if there is a link between solar radiation intensity and near surface temperatures. Another main objective is to provide readings for all the above, on a slope covered by a forest canopy, creating a shadowing affect. Exposure readings for all sites will be recorded to assess the extent of shadowing from near surfaces and objects.

Oriental Art :: essays research papers fc

Oriental Art   Ã‚  Ã‚  Ã‚  Ã‚   Oriental Art is very unique and interesting. It is based on life all around them, nature. In Hsuan-ho hua pu classifies paintings in ten groups: „h Taoist and Buddhist (tao shih) „h Human affairs (jen wu) „h Places and other buildings (kung shih) „h Foreign tribes (fan tsu) „h Dragons and fishes (lung yu) „h Landscapes (shan shui) „h Animals (chu shou) „h Flowers and birds (hua niao) „h Ink Bamboos (mo chu) „h Vegetables and fruits (su kuo) This religious art, including portrayals of gods, stands at the head of the list and is followed by a group of paintings including portraits of legendary heroes. Group three and four also relate to men, while group five includes that fountainhead of moral virtue, the dragon. However the didactic value of the remaining categories is less apparent, and for this reason they occupy the lower half of the list. The category of Chinese painting called flowers and birds (hua niao) is to some extent cognate with European still-life painting in subject matter, yet spiritually the two have little or nothing in common. In China especially, this trait long outlived the primitive stage of human culture completely sophisticated form of picture- making. As a result, the tradition of Sung Chinese flower-and-bird painting made itself felt though out Asia. Among the Chinese themselves, flower-and-bird painting is a major form of pictorial expression, which for thousands of years has exercise their aesthetic imagination to extent comparable with, say, our European nude. Assembly of Birds can best be described in Rowland ¡Ã‚ ¦s words  ¡V a habitat group with a painted black cloth. For despite the beauty of its execution, it is as airless as a showcase in some provincial museum of natural history, in which someone has attempted to provide, for its palpably moribund occupants, a realistic setting of seashore, marsh, or tropical savannah. Paintings of bamboos are entered under the heading mo chu, or  ¡Ã‚ ¥ink bamboo ¡Ã‚ ¦. This term does not only mean bamboo painting done solely in monochrome ink; it also implies that brush and ink are used in recognizably calligraphic way, and not merely to build up forms by describing boundary lines. Paintings of bamboo done by means of outline (kou li) were not admitted as a separate category in Chinese painting; nor, theoretically at least, can be classified as mo chu. A piece of bamboo has objective existence as a percept before it has been painted, whereas a written character has none. Oriental Art :: essays research papers fc Oriental Art   Ã‚  Ã‚  Ã‚  Ã‚   Oriental Art is very unique and interesting. It is based on life all around them, nature. In Hsuan-ho hua pu classifies paintings in ten groups: „h Taoist and Buddhist (tao shih) „h Human affairs (jen wu) „h Places and other buildings (kung shih) „h Foreign tribes (fan tsu) „h Dragons and fishes (lung yu) „h Landscapes (shan shui) „h Animals (chu shou) „h Flowers and birds (hua niao) „h Ink Bamboos (mo chu) „h Vegetables and fruits (su kuo) This religious art, including portrayals of gods, stands at the head of the list and is followed by a group of paintings including portraits of legendary heroes. Group three and four also relate to men, while group five includes that fountainhead of moral virtue, the dragon. However the didactic value of the remaining categories is less apparent, and for this reason they occupy the lower half of the list. The category of Chinese painting called flowers and birds (hua niao) is to some extent cognate with European still-life painting in subject matter, yet spiritually the two have little or nothing in common. In China especially, this trait long outlived the primitive stage of human culture completely sophisticated form of picture- making. As a result, the tradition of Sung Chinese flower-and-bird painting made itself felt though out Asia. Among the Chinese themselves, flower-and-bird painting is a major form of pictorial expression, which for thousands of years has exercise their aesthetic imagination to extent comparable with, say, our European nude. Assembly of Birds can best be described in Rowland ¡Ã‚ ¦s words  ¡V a habitat group with a painted black cloth. For despite the beauty of its execution, it is as airless as a showcase in some provincial museum of natural history, in which someone has attempted to provide, for its palpably moribund occupants, a realistic setting of seashore, marsh, or tropical savannah. Paintings of bamboos are entered under the heading mo chu, or  ¡Ã‚ ¥ink bamboo ¡Ã‚ ¦. This term does not only mean bamboo painting done solely in monochrome ink; it also implies that brush and ink are used in recognizably calligraphic way, and not merely to build up forms by describing boundary lines. Paintings of bamboo done by means of outline (kou li) were not admitted as a separate category in Chinese painting; nor, theoretically at least, can be classified as mo chu. A piece of bamboo has objective existence as a percept before it has been painted, whereas a written character has none.

Purtian Men and Women in Edward Taylor and Anne Bradstreet Essay

Purtian Men and Women in Edward Taylor and Anne Bradstreet Crossing the Atlantic, Puritans faced not only the physical hardships of an uncultivated land, but also difficulties within the structure of their religion. In "The Puritan Dilemma," Edmund Morgan details the contradicting tenets of Puritanism. Puritans were to seek salvation even though they were â€Å"helpless to do anything but evil†; they were to rely entirely on Christ for salvation even though salvation was only possible if preordained by God (7). Additionally, in the Puritan paradigm, the relationship between Christ and the church was analogous to that of husband and wife. Husbands took pre-eminence over wives, just as Christ reigned supreme over His flock. This layered system of servants and masters caused men and women to experience Puritanism very differently. The poetry of Edward Taylor and Anne Bradstreet demonstrates that while Puritan men focused on pleasing their Heavenly Father, Puritan women sought the approval of earthly men. Studying female authorship in colonial America, William Scheick notes that Puritans supported this attitude of subordination with Biblical passages. In the Old Testament, Adam declares Eve the bone of his bones and the flesh of his flesh. Because â€Å"she was taken out of man,† Adam resolves on calling her â€Å"woman.† Similarly, in the New Testament, Paul describes Christians as â€Å"members of [the Lord’s] body, of his flesh, and of his bones.† Whereas the Genesis passage refers to earthly matrimony, Paul addresses the spiritual marriage between Christians and the Bridegroom Christ. Scheick observes how these passages imply â€Å"the silent subordination of the second sex to men, [and] the reverence wives owe to their husbands† (62).... ...ism in early New England. Works Cited Bradstreet, Anne. â€Å"The Prologue [To Her Book].† The Heath Anthology of American Literature. Ed. Paul Lautier. New York: Houghton Mifflin Company, 2004: 188-190. Hambrick-Stowe, Charles E., ed. Early New England Meditative Poetry. New York: Paulist Press, 1988. Morgan, Edmund S. The Puritan Dilemma: The Story of John Winthrop. Boston: Little, Brown and Company, 1958. Stanford, Ann. â€Å"Anne Bradstreet: Dogmatist and Rebel.† The New England Quarterly 39 (1966): 373-389. JSTOR. Colorado State University, Fort Collins, CO. 3 Oct. 2005 . Taylor, Edward. â€Å"Prologue.† The Heath Anthology of American Literature. Ed. Paul Lautier. New York: Houghton Mifflin Company, 2004: 239-240. ---, â€Å"Huswifery.† The Heath Anthology of American Literature. Ed. Paul Lautier. New York: Houghton Mifflin Company, 2004: 236-237.

No Fixed Address :: essays research papers

  Ã‚  Ã‚  Ã‚  Ã‚  No Fixed Address   Ã‚  Ã‚  Ã‚  Ã‚  In Aritha Van Herk’s â€Å"No Fixed Address†, one key symbol surfaces many times. The main character’s name is Arachne, which means spider, and sets the reader up to understand the central symbol in the novel—the spider web. The reader sees several other instances of webs showing up throughout the novel. Arachne’s dependence on the road and her random driving is another form of web in â€Å"No Fixed Address†. To tie in Arachne’s driving with webs, we see Thomas’s maps as webs of sorts. The most important web that Arachne is seen to weave is that perverbial web of lies—a person can never escape from that web. In the end, Arachne is indeed caught in her own web, and in the end, she is caught in it.   Ã‚  Ã‚  Ã‚  Ã‚  Arachne, in mythological terms, is the master weaver; the women who pitted herself against a god and lost, thus being turned into a spider. Arachne Mantea is much the same. She is constantly putting herself into categories that she doesn’t belong in. Much of her life, Arachne was certain that she was adopted. Her family seems to be poor, but Arachne could not fit herself into that social class. When she finally meets a family that is of a rich class, she realizes whole-heartedly that she doesn’t belong to that class either. Arachne seems to belong nowhere, almost as if she belongs to that race in the heavenlies—this is her first and most fatal lie. When Arachne ceases to belong to any particular group, she becomes capable of anything. Cheating, stealing, and killing are no longer beneath her. If she doesn’t belong where she is anyway, Arachne doesn’t need to remember her past; she doesn’t need to cope with the things that have happened to her. Thus, Arachne forms lies of denial concerning her past and present actions. She represses the memories of a painful youth, while believing that her whoring around will never catch up with her. She begins to live a lie, and one that eventually gets her. Other aspects of her life mirror the level of lie that she is living. The manner in which she drives shows us more than any other.   Ã‚  Ã‚  Ã‚  Ã‚  When Arachne is merely lying to herself, we see her driving in a relatively small area, and very predictably so. She drives a bus, and in doing so, Arachne has a defined route.

Funding the Rising Cost of U.S. Health Care Essay

Give your opinion of the rising cost of health care’s overall impact on the U.S. economy It is more expensive for individuals, families and employers to have health care coverage because of the rising cost. Spending on the use of new technologies, treatment, and high cost for medical services. There has also been a high cost on local, federal and state government which led to high cost on to medical and Medicaid. This spending of health care has affected the economy and now people have to choose between a need for health care of the need to have shelter, food, or not having sufficient funding. Health care spending is moving faster than the economy is growing. High health care rising cost is causing the government to re-examine eligibility for public health and rising taxes on the consumers is leading to reduce investments. The U.S. will not be able to compete in the economic global market. These rising cost in health care will affect business, house wholes, providers, employees, health status, income levels, age, and increase premiums. (Rising Health Care Costs ) http://www.ahip.org/Issues/Rising-Health-Care-Costs.aspx â€Å"Health plans are playing a vital role in reducing the cost of care and improving value†¦Ã¢â‚¬  – Karen Ignagni, President & CEO, America’s Health Insurance Plans Health Plan Innovations in Delivery System Reforms, American Journal of Managed Care Compared and contrasted at least two (2) areas of the economy that the new health care act impacts. Small business and middle class families are two areas that the new health care act will impact. It used to be the economic strength in the U.S. was the small business owner. Small business has been strength to the economic by bring diversified groups opportunities of people to the workforce. Small business bring products have that are innovative to the services market. Small business has been able to create new jobs for the economic. However since the housing bubble in 2007 and 2008 small businesses are struggling very hard from the bank credits. Small businesses are the back bone to job growth and innovation for the economy. Small business owners who offer health care insurance to their workers are facing a hit by heavy taxes and high premiums for the employer. Small business pays up to 18% more per worker for health insurance than larger firms. This is a tax disadvantage for small business. Which cause profits to be eaten  up by higher health insurance cost and workers working for lower wages makes the small business workers, product, and market at a disadvantage. Small business(less than 50 workers) is less likely to provided health insurance. Back in the 50s and 60s a middle class family of three could live off a one person income which was the father. Mothers were house wives and people could purchase a home, car, and have a small savings. Families could go on vacation and own a late model car. The burden for middle class families today is the high cost for health care insurance and premiums. There have been an increase in unemployment and employees are scaling back on wages. Credit card debt gone up and slow job creation. Increase in bankruptcy files, income inequality and out-sourcing of America business has been causing problems for the middle class families. This growth in health care spending has change priorities for middle class life style. With saving money, retirement benefit pension, and 401K plans shifting. Middle class person who have been working all their lives, now rick the chance of not having sufficient funds to maintain middle class life style. Will the middle class be able to retire and live a middle class style? Middle class families are not sure if there will be available income for retirement. (http://www.aarp.org/research/ppi/security/impact-of-rising-healthcare-cost-AARP) Debated the main pros and cons of using private insurance versus using the new affordable insurance.  Our population in this country has increase over the last 30 years and because of healthier life style and medical advances people are living longer. This can be a disadvantage to the patients who are using private insurance. This has put a strain on the private health insurance because most companies don’t cover previous medical conditions that cover injuries and short-term illness. Illness is something that happens on its own and worrying whether or not your condition is cover can add stress. After receiving a referral from the internal doctor the patient has to act as its own administrator who calls the insurance company to check, if the cost is cover before they can see a consultant for treatment. If you want more coverage you pay higher premiums. There also a disadvantage of having so  many private health insurance companies to pick from. Each representative only disc usses their company policies and not how their policy compares with others. Leaving the patient not knowing which one is the best offer for you. Private insurance advantages is you can choose where you want to be treated without a long wait. There are specialist teams that will deal with specifically types of conditions. There continuity cares that allows you to be seen by the same consultant until the end of your treatment. The new affordable insurance covers families, small business, and individuals with the cost assistance through the market place program. There are no limits on life time health care which this will cut down on large medical bills for long term illness. This will keep people out of debt. If you make a mistake on your application or if you are sick an insurance company can’t drop you. A person with pre-existing condition can’t be denied care or charge a higher premium. The new affordable insurance allows for parents to keep their children on their plan until the age 26 years old whether they live at home, married, or attend school. The affordable insurance has free preventive care for checkups, well woman visits, mange care to control chronic illness before they become costly to treat or complex. http://obmacarefacts.com/benefitsofobamacare.php) OBMA CARE FACTS dispelling the myths Analyzed the major impact this new health care system may have on different immigrant demographics; Predicted the cost associated with the changing the accommodation to facilities having to review organizational planning in order to actualize these changes