International law Essay Example | Topics and Well Written Essays - 1500 words

International law - Essay Example Despite existence of the political, global and territorial differences the whole world is considered as a global village and such concept mainly enhances the idea of universal brotherhood. At the same time in the context of trade, cultural intercourse, the idea of globalization plays a major part. In this context it needs mentioning that no matter how much the globalization aspect seems positive and flawless but at the same time it includes several lacunas. In this global society also the superior nations are finding an opportunity to show their aggression, to inflict oppressive approaches towards the other nations, their people and their economy. The rate of crime has also increased to a great extent and most of the criminal, after committing the criminal deeds flee to other nations to seek shelter. As administrative system of a particular nation does not have the power to exercise the hold over other jurisdictions, the fear of being caught is reduced to a great extent for those cri minals. At the same time economic aggression is also taking a brutal shape. According to modern international treaties in the post World War II situation it has not been possible for the nations to exaggerate the power of politics to express their imperialistic mentality. Thus, those nations have adopted the procedure of economic aggression through which a superior nation can enjoy economic hold over the other nation through trade relationship. Thus, the importance has also been realized by legal scholars that there must be some kind of restraints that prevent one nation to become havoc over the other. These are some of the typical situation; rather problems at the international level that generated the emergence of this new discipline of legal jurisdiction: International Law. Legal and scholars of jurisprudence have attempted to provide definition of the International Law in different

Watch the film on a speech by renown anti-racist activist The Essay

Watch the film on a speech by renown anti-racist activist The Pathology of White Privilege of Tim Wise - Essay Example The fair housing act was compiled in 1968 and until 1968, there were no highest number of race based housing discrimination complaints. One million Afro-Americans died to till date due to lack of heath care facilities. In the similar manner, law enforcement authorities are continuously maintains the white supremacy. Afro-Americans and Latin Americans are three times more likely suspected and checked for drugs; however, white Americans are found to have drugs four and half times more like when they are stopped. He argues that when white people see a Latin American young person driving a nice car, they would say him a drug dealer; however, if a white young person drives the similar car, people would say, â€Å"spoiled rich child†. The average white American family holds 4 times more wealth as compared to an average Black American family and 8 times more wealth as compared to average Lain American family residing in USA premises. He argues that in 1962, 1963, 90% of the White Americans argued that black Americans are receiving equal education opportunities and services but we know that the real situation at time. In 2005, 80% of the white Americans believe that black and Latin Americans are receiving equal educational rights. He argues that white Americans use the word underprivileged for the black and Latin Americans but who is then â€Å"overprivileged†. He uses the word â€Å"overprivileged† for the white Americans. He argues that if someone is down then someone must be up on him. That is the reason he is down and someone is making him down. He argues that why white American do crimes regarding racial discrimination and then escape into woods. White people give black Americans low wages as compared to white Americans. Free labor is demanded when black Americans are hired to work in fields. It is right to torture a Muslim for the act he has never done. White Americans

Psychological theories relating to Frankenstein (Mary Shelley's Case Study

Psychological theories relating to Frankenstein (Mary Shelley's Frankenstein) - Case Study Example Although Frankenstein has been noted for its treatment of the philosophical, mythological, scientific, and feminist questions, it is fundamental to realize that the novel also undertakes an in-depth study of the psychology of mind, human nature and, most significantly, alienation. The offers an important case of reference to an analysis into how human brain creates one’s mental world and the novelist portrays the images of her politico-cultural world and value system through the characters of the novel. Significantly, Mary Shelley has been greatly novel effective in unleashing the images of her mental world into the intellectual sphere of her novel in a subjective, complex and problematic way and establishes the relationship between the theories of the mind and the motivations of the characters. â€Å"Mary Shelley translates politics into psychology. She uses revolutionary symbolism†¦ Her characters reenact earlier political polemics on the level of personal psychology.à ¢â‚¬  (Sterrenburg, 144) Therefore, a reflective analysis of the novel Frankenstein by Mary Shelley corroborates that the motivations of the characters in the novel are directed by the mental world of the novelist. Psychological theories dealing with the working of human mind can be greatly useful in comprehending the construction of a literary work, especially the characterization of a novel. ... In order to comprehend the theories of mind in relation to the motivations of the characters in the novel, it is essential to realize the philosophical context of the work which is suggested by the theory of the ‘tabula rasa’ or ‘clean slate’. â€Å"This theory, held by the Empiricists, maintains that the mind, at the beginning of a person’s life, is empty; after birth, the senses receive impressions and are able to formulate ideas.† (Joshua, 25) The mental world of the novelist created by the socio-cultural and political images of her contemporary situation was crucial in the creation of the major characters in the novel. Significantly, the major characters of the novel, the young student of science and the monster created by him, offer a crucial example of how the mental world is linked to character-motivations. An investigation into the complex and multifaceted personalities of Frankenstein and the creature is essential in realizing the moti ves of these characters as the making of their mental world. Similarly, every significant question concerning science and society as discussed in the novel brings out this crucial link between the motivation of the character and their mental world. In a profound understanding of Mary Shelley’s creation account in the novel, it becomes lucid that the mental world of the creator has a great influence on the motivations of his creation. Thus, the mythic ambiguity of the central characters, Victor Frankenstein and the creature, points to the underlying moral ambiguity of the story. In Shelley’s creation account, neither the creator nor the creature in his rebellion has morally pure motivation. This characteristic feature of the novel corresponds to the link between the mind and the motivations

Polar ice and climate change Research Paper Example | Topics and Well Written Essays - 750 words

Polar ice and climate change - Research Paper Example This is especially so with the ever increasing rate of melting attributed to the environmental degradation. For years, scientists have had their eyes set on the world’s ice shields hoping to monitor changes with the advancements in technological systems. Global temperatures indicated a downward trend in the period from 1940 to 1970, but increased gradually in 1980s. This phenomenon can be attributed to the increase of the amount of sunlight that hits the snow and ice in these regions. As such, various reports have illustrated an accelerated rate of melting raising the sea levels at an alarming state. For instance, a survey done every September to ascertain the area covered by sea ice demonstrates an average decrease at a rate of 8.6% between the years of 1979 and 2007 (Thompson and Kuo, 2012).However, there was a significant loss of sea-ice placed at 24% in the 2007 alone. Various scientists have voiced concerns based on these and current findings that corroborate the eminent danger of melting ice caps and rising sea levels. Extrapolations of existing data suggest that thermal expansion and ice sheet changes will dominate the processes affecting the sea level (Ward, 2003). Similarly, areas that are marginally glaciated are most likely to be ice-free, which will eventually lead to the disappearance of the Polar Regions. ... This is because these gases increase temperature of the atmosphere near the earth and its troposphere; resulting in corresponding changes in climatic conditions. Fundamentally, the dangers associated with global warming are erratic changes in the weather, which are experienced in extremity, causing persistent natural disasters and extinction of species. In essence, the continual warming trend has been broken down to climatic change, which refers to the measurable effects of global warming. These measurable effects refer to shifts in major aspects of the climate that is, rainfall, temperature, snow, and wind patterns. With this differentiation, global warming is identified as a long-term reference of the effects of these shifts in climatic conditions. Notably also, ocean currents are included as an aspect that facilitates the continual warming trend. Currently, environmental degradation is an issue that requires immediate action because of the escalating rate at which it has been occu rring, making it hard for the ecosystem to convalesce. Pollution is considered as the major cause of ozone layer depletion owing to the release of chlorofluorocarbons that rise into the troposphere causing its depletion (Fahey and Hegglin, 2010). Industrial processes and automobiles are responsible for the release and as such, governments have been asked to tax the companies for the emissions. In addition, the destruction of tropical rainforests by logging industries has resulted in destruction of natural habitats of plants and animals, which increases the level of carbon dioxide in the atmosphere. The destruction of habitats interferes with photosynthetic organisms that are responsible for carbon-fixing cycle, which seeks to relieve the greenhouse effect. In

Why Marijuana Should Remain Illegal Essay Example for Free

Why Marijuana Should Remain Illegal Essay Specific Purpose:To teach my audience how to drive a stick shift car. Thesis Statement:By learning how to start a stick shift car, changing from first to fifth gear and reverse you would someday like to buy a stick shift car. Organizational Pattern:Chronological Introduction: Did you know that by knowing how to drive a Stick shift car you can save money on the initial price, maintenance, and fuel economy? How many of you guys could use an extra couple thousand. I am going to teach you how to drive a stick shift car and to do so you will need to know how to properly start the car, change the gears, and how to reverse the car. Body: 1. First, you will need to get in your car adjust your seat, so you can reach all three pedals. A. You will need to put your foot all the way down on the clutch. B. Then put your car in neutral so you can take your foot off the pedal 2. Second, you will need to put your foot on the clutch then put it in first gear with your foot on the clutch A. As you start to ease your foot off the pedal you need to start stepping on the gas your two feet must past each other at same time. B. Then you will completely take your foot off the clutch as you start to step on the gas you will no longer need your foot on the clutch. The process will repeat 3. Third, you will need to be at a full stop then you will need to put your car in neutral, A. Step on the clutch then push down on the knob till you feel a little nudge B. Then you will change the gear as you would do with your first gear C. You will need start to ease off clutch then step on gas pedal D. Finally you will need to come to a complete stop put your car in neutral and turn your car off. Step on the clutch then put your car in first gear and pull the hand break. Conclusion: Now that you all know how to start a stick shift car, change the gears and put it in reverse. Hope you guys can enjoy driving a stick shift car and also the benefits you get when you buy a stick shift car.

Financial audit Essay Example for Free

Financial audit Essay A deficiency in internal control exists when the design or operation of a control does not allow management or employees, in the normal course of performing their assigned functions, to prevent, or detect and correct, misstatements on a timely basis. A deficiency in design exists when (a) a control necessary to meet the control objective is missing, or (b) an existing control is not properly designed so that, even if the control operates as designed, the control objective would not be met. A deficiency in operation exists when a properly designed control does not operate as designed or when the person performing the control does not possess the necessary authority or competence to perform the control effectively. * Material weakness. A deficiency or a combination of deficiencies, in internal control, such that there is a reasonable possibility that a material misstatement of the entitys financial statements will not be prevented, or detected and corrected, on a timely basis. * Significant deficiency. A deficiency, or a combination of deficiencies, in internal control that is less severe than a material weakness yet important enough to merit attention by those charged with governance. AU-C Â §265 also claims that the auditor should communicate to management at an appropriate level of responsibility, on a timely basis. in writing, significant deficiencies and material weaknesses that the auditor has communicated or intends to communicate to those charged with governance, unless it would be inappropriate to communicate directly to management in the circumstances. * in writing or orally, other deficiencies in internal control identified during the audit that have not been communicated to management by other parties and that, in the auditors professional judgment, are of sufficient importance to merit managements attention. If other deficiencies in internal control are communicated orally, the auditor should document the communication.

Temporal Variation in Water Column Structure in Estuary

Temporal Variation in Water Column Structure in Estuary Panourgias Siderakos Temporal variation in water column structure, transmissometry, and fluorometry in a macrotidal estuary Abstract The temporal variation in water column structure, transmissometry and fluorometry was observed and monitored on the 10th of November 2016 in Southampton Water, over a half tidal cycle (approximately from 9 a.m. to 4 p.m.). That specific day a neap tide behaviour occurred. Variable measurements were performed on the Callista vessel and also with the CTD device. Additionally, nutrient and zooplankton measurements took place in order to acquire more data. The chlorophyll concentrations that were measured showed low values with an average value of 0.7 to 0.8 ÃŽÂ ¼g/l. The maximum values were observed during the transition from the high-tide time to the low-tide time (almost 1.1 ÃŽÂ ¼g/l). Temperature, light and salinity measurements performed a small change during the day, in relation to depth. The data that were collected and processed imply that the main factor that influences the temporal variation in water column structure is the tidal cycle of the specific area concerned. This cycle, and its currents, is responsible for the general behaviour of the water column (how much stratified or mixed is).          1. Introduction Estuaries are very diverse systems. This is due to the existence of very shallow waters, which in relation to other various factors, can potentially affect the temporal variation in water column structure, transmissometry and fluorometry. Perhaps, the most essential factor that must be taken into consideration in Southampton estuarine environment, on a daily basis, is the Spring Neap tidal cycle. Southampton Water forms the north-westerly extension of the Solent System on the south coast of England, and forms the estuary of three chalk-derived rivers: Test, Itchen and Hamble. The area has an unusual tidal pattern, where the interaction of the M4 and M6 tidal constituents (usually during a Spring tide) creates a double high water. This high water stand can last up to 3h, reducing the time for the ebb phase. This tidal asymmetry leads to 6h of moderate flood currents and 4h of rapid ebb velocities (1.5 m/sec). The flood phase has also a slack period (young flood stand), where the tidal currents become temporarily weaker. The foregoing factors generate stronger mixing during the ebb phase showing also an increase from a Neap to a Spring tide (Lauria et al., 1999). The present survey aims to identify and clarify at the same time the patterns influencing physical and biological parameters and the processes linking these patterns in a macrotidal estuary, more specifically the Southampton Water estuary. Furthermore, these patterns must also be examined if they differ, during other tidal states and at different times of year. 2. Materials and Methods 2.1. Survey area The survey area was Southampton Water. A shallow, partially mixed coastal plain estuary. It is located on the south coast of England. Its length is 10 km and has a width of 2 km with a dredged central shipping channel of 15m below mean tide. It is essentially marine in character, with little variation in salinity number (~30) in the mouth. Stratification occurs mostly at the head of the estuary. Water temperature within Southampton Water varies according to the season, with minimum winter temperatures below 7 ° C and maximum summer temperature above 17 ° C. (Williams et al., 2006) 2.2. Materials and Methods Sampling took place over an approximate 7 hour time period on the 10th of November 2016. The area was in a small radius of 0.5 nautical miles from the position 50 ° 52.259 ´ N and 001 ° 22.348 ´ E (data-buoy coordinates). During the day, a neap tide was occurring. The tide cycle involved two high-tides and one low-tide. First high tide took place at 07:57 local time (4.17 m) and the second one at 20:07 local time (4.08m). The low tide between them was at 12:37 (1.85m) (Southampton Tide Times internet site). Samples were collected using the research vessel Callista of the National Oceanographic Centre. The winds had a Northeast direction and varied from 10 to 20 knots speed. However, the sea state was around 3 (~0.5 m wave height) and the cloud coverage varied from 3 to 6 octal. The survey plan that had to be followed was a continuous measurement (every half hour) from approximately 09:00 to 16:00 (local time), averaged in every meter of depth for later processing. Vertical profiles of conductivity (salinity), temperature, density, transmissometry and fluorescence were obtained using a CTD. On the CTD, a transmissometer and a fluorometer were mounted, along with the Niskin bottles for water sampling. Although there is not going to be an analytical description of their abilities and their ranges of measurement, a list of the devices that were used both on Callista and on the CTD is shown below: CTD SeaBird SBE 19+V2 RDI Workhorse Mariner 600kHz ADCP Biospherical Instruments Inc. QCP2300 Irradiance Sensor C-Star 25cm Transmissometer FL-NTU(RT) Fluorometer The Aanderaa SOOGUARD system Enviro-T In-Line Fluorometer Oxygen Optode 4330/4330F Conductivity Sensor 4319 Temperature Sensor 4060 Samples of water were collected with the Niskin bottles at two depths every one hour. The first one at 1m below sea surface and the second one around 2m above sea bed. These samples were obtained for further chlorophyll, phosphate and silica analysis. Chlorophyll-a was measured with the method of acetone extraction. Silica and phosphate concentrations were measured in the chemistry lab at the National Oceanographic Center, from the samples that were collected by the groups on the RIB. Current speed and direction could not be measured because the sensor was out of order. Zooplankton measurements were made and samples were also collected. The first occurred at the beginning of the boat trip (from 09:37 to 09:43 local time) and the second one at the end of it (from 15:45 to 15:50 local time). Special zooplankton nets were used and the samples were kept in special chemical liquid (formaldehyde) for preserving, until it was processed. Essential data were also collected from the Xylem Analytics UK EMM700 Data Buoy in Southampton Water. The buoys coordinates are 50 ° 52.259 ´ N and 001 ° 22.348 ´ E and the data involved air temperature, water temperature, wind direction, wind speed, PH, Chlorophyll, O‚‚ etc. The collected data concerned the time periods between February 2016 to October 2016 and also the week from 7th to 11th of November 2016 (Boat Week). 3. Results 3.1. Tide In the morning, when the sampling begun, the tide height was decreasing until 12:37 (local time) to the height of 1.85m (ebb phase). After that, the tide height increased again until the end of the survey (flood phase) and headed to its second high tide for the day at 4.08m (20:07 local time). Despite the fact that there were no data obtained for the tide currents speed and their direction because of the non-functioning sensor, taking into consideration the Nautical Charts from the British Hydrographic Service for the specific area, we observe that tide currents have different directions during the day (tide cycle) and their velocity varies from 0.5 to 2 m/sec, approximately. In figure 1, the half-tide cycle of the day is demonstrated and also the Potential Energy Anomaly, derived from the different densities and energies at each depth, showing a value of average stratification for each station. 3.2. Temperature-Salinity The water column demonstrated a temperature variation between +11.1 and +11.5  °C (fig. 2(a)). In the meantime, salinity values were measured between 33.0 and 34.0 units (fig. 2(b)). Temperature decreased with depth while salinity increased. The small range variation of the vertical temperature and salinity profiles, imply that the water column was partially mixed throughout the whole sampling time period. A small water mass with high salinity is observed at the depth of 6.5 m at 13:00 (local time) which is obviously a more saline, sea-water mass below the fresher river-water masses. The temperature distribution seems more homogeneous with depth. The two figures show a relative resemblance, as more saline water goes deeper. As a result, during the day hours, when the sun light still exists, the deeper we go in the water column, the colder it gets. 3.3. Chlorophyll fluorescence Chlorophyll fluorescence measurements were very low during the survey, demonstrating values between 0.55 and 1.15 approximately (fig. 3 (a)). A water mass of higher chlorophyll fluorescence was observed near the water surface around 13:30 (local time). However, chlorophyll did not demonstrate any essential changes, being almost homogeneous in relation to depth, which implies a well-mixed water column as well. 3.4. Light Transmission Light transmission measurements also showed a very well mixed water column. The measured values had a small range and demonstrated from 2.7 % to 3.15% maximum (fig. 3 (b)). In this figure, the vertical profile of the percentage of light that is transmitted is shown. The light transmission plot also agrees with the chlorophyll fluorescence plot. A small area of 2 meters depth (from 5 to 7 meters depth) was observed between 10:00 and 11:00 with the highest values of transmission (3,15%), but this was, possibly, a random phenomenon. 4. Discussion 4.1. Temperature and Salinity According to the measurements that were made and the width of change, no significant pattern of temperature change was observed in relation to depth. Southampton Water temperatures vary from a winter minimum of 17 ° C (June-August) (Muxagata et al., 2004). Temperature homogeneity in relation to depth signifies that temperature is not playing any essential role in the estuary dynamics, nor the estuary water stratification. General speaking, temperature indeed enhances the growth of phytoplankton while in most temperate marine systems seasonal thermal stratification is the main factor that triggers the start of spring bloom. In the marine environment of Southampton, it seems that temperature is not the most important factor. (Iriarte et al., 2004). Salinity did not play any significant role either. The range of values that were measured was really small. However, the contour of salinity in relation to depth implies a more stratified water column than that of the temperature. As a result, salinity is more important than temperature in affecting the estuarine stratification. 4.2. Chlorophyll Chlorophyll concentrations did not demonstrate a big change either. The general measured values were very small (~0.5 to 1.1 ÃŽÂ ¼g/l), which phenomenon agrees with the general rate of chlorophyll growth in Southampton Water during autumn. This fact can also be observed in figure (4), where the buoy data from February 2016 to October 2016 are shown. It can be clearly stated that the largest chlorophyll growth occurs in August, simply related to temperature and weather conditions (low winds-low seas states). However, chlorophyll blooms which happen in spring and summer, coincide with the period of relatively low Spring tide, followed by a Neap tide. The higher degree of stability in the water column allows growth to occur without the greater flushing that is experienced at Spring tide. The reestablishment of high Spring tides caused chlorophyll levels to fall as the estuary was flushed (Wright et al., 1997). Moreover, phytoplankton populations can show changes from seasonal and inter-annual variations, but more extended variations occur during periods of low mixing on Neap tides (Lauria et al., 1999). The tide cycle in Spring and Neap tides is probably one of the most important factors in the phytoplankton growth. As long as the pattern in Southampton Water is concerned, the seasonal distribution of chlorophyll-a showed low winter values followed by a spring peak during the last week of April and intermediate concentrations during summer, dropping to pre-spring bloom levels by October (Purdie et al., 2004). 4.3. Light The measurements with the Secchi disk and the transmissometer in the water implied the fact. That light did not play a key-role in the general growth of phytoplankton in the Southampton Water. Furthermore, figure 5 shows the turbidity (%) of the water during the day. Although the changes are very small, it can be observed that after 12:00 (local time), when the ebb phase of the tide cycle approaches and the mean water depth decreases, the values slightly increase. This also draws a conclusion that the light influence on the water column is mainly affected by the tidal cycle. 4.4 Nutrients-Zooplankton Although not shown in figures in this report, nutrient concentrations in the Southampton Water were mainly affected by the tidal cycle. All the measurements that were made during this survey supported the fact mentioned above. Silica and phosphate measurements showed that their behaviors were affected mainly by the tide cycle. In addition, special measurements also revealed that during the ebb phase, zooplankton was moved, probably with the water masses that the tide currents moved. This fact also resulted in a significant decrease in zooplankton numbers. The most abundant species were copepods (while all the other species had an almost null value), whose numbers indicated a decrease of around 30% after the ebb phase (zooplankton measurement No 2). Words: 2156 References Iriarte, A., Purdie, D.A., 2004. Factors controlling the timing of major spring bloom events in an UK south coast estuary. Estuarine, Coastal and Shelf Science 61, 679-690. Lauria, M.L., Purdie, D.A., 1999. Contrasting phytoplankton distributions controlled by tidal turbulence in an estuary. Journal of Marine Systems 21, 189-197. Williams, J.A., Muxagata, E., 2006. The seasonal abundance and production of Oithona nana (Copepoda: Cyclopoida) in Southampton Water. Journal of Plankton Research 28, 1055-1065. Wright, P.N., Hydes, D.J., Waddington, I., Rawlinson, M., 1997. Real time chlorophyll and nutrient data from a new marine data buoy in Southampton Water, UK. Electronic Engineering in Oceanography, 73 78. Figure 1: The Neap Tidal Pattern during the sampling period (10:00-16:00 local time-GMT) and the Potential Energy Anomaly (a) (b) Figure 2 (a): Water temperature contour in relation to depth, during the sampling period (b): Water salinity contour in relation to depth, during the sampling period (b) Figure (3) (a): Plot of Chlorophyll fluorescence in relation to depth, during the day (b): Plot of Light Transmission in relation to depth, during the day Figure (4): Chlorophyll concentration and water temperature in relation to time (from February 2016 to October 2016) Figure 5: Turbidity in relation to depth, during the day   Ã‚