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The area figures relate to districts, sub- Land use: ways in which man takes
The districts and the sub-districts were advantage of the land for activities such as: defined according to the official administrative construction, agriculture, forestation, industry, division of the State of Israel. According to etc. Land use relates to the situation today, this division, Israel has six districts, which are as opposed to land allocation relating to As of 1967, the area of East Jerusalem has The information on land use is national and been included in the Jerusalem District. In continuous for all the land in the country. 1982, the Golan sub-district was attached to Information can be produced according to various geographic categories, such as Local Authorities, Regional Councils and natural Israel and Jordan, which was signed on 26 October 1994, territories were exchanged in Land use can be divided into two main types: the Southern Arava and Bet She’an Basin in This chapter also presents data on the natural according to various functions: housing, region areas within each sub-district as wel services, culture and leisure, commercial, Natural regions are continuous areas, as industry and infrastructure, transportation and uniform as possible, both with regard to physical structure, climate and land, as wel Open area is cross-sectioned according to the following types: public open area, forests, SOURCES OF DATA: The information is district or, in some cases, an entire sub- based on processing and integration of a district or entire district (see the Map of Israel variety of administrative sources that were - Districts, Sub-districts and Natural Regions, received from ministries, non-government In the 1995 Census, the system of natural The database on which the information is increased from 45 (in the 1983 Census) to 50. After the 1995 Census of Population and Housing, the method of measuring areas was Israel’s climate has unique characteristics. Israel’s geographic location, between 290-330 The areas of districts and Sub-districts were north of the equator, makes it a subtropical revised according to boundary adjustments region, which is a transitional area between the temperate zone and the arid zone. Israel, therefore, is on a “climatic crossroads”: its southern and eastern areas are characterized by an arid climate, while the rest of its areas characterized by a Mediterranean climate. of the main characteristics of this kind of climatic formation is the high variability in quantities of precipitation from year to year Be’er Sheva, Negev Institute: 34048’E; 31015’N; and between different areas. The summer is hot with hardly any rain, and the winter is cool Be’er Sheva, West: 34043’E; 31016’N; 195 m. Mizpe Ramon: 34047’E; 30037’N; 837 m. The rainy season in Israel usually begins in
October and ends in May of the next year.
Precipitation data are presented for rain Sede Eliyyahu: 35031’E; 32026’N; -190 m. years, i.e., from August to July of the next Data on average precipitation have been standardized and adjusted to the normal The multi-annual averages of number of rain pollutants - see Chapter 27 - Environment. Presented are the number of rain days with quantities of more than 1 mm. Relative humidity - the ratio (in percentages)
of vapour in the air, and the amount the air can contain in a state of saturation at the Global radiation: short-wave radiation of the
Temperature data and relative humidity are horizontal plane from a spatial angle of 2 π temperature and relative humidity refer to the Duration of sunshine: the amount of time
period from 1981 to 2000, except Haifa (1988- 2000). The division into regions in the tables, has been adapted to the division into geoclimatic Data were obtained from the Meteorological The table presents data on global radiation at 4 stations out of 20 (the number of stations varies): Haifa (Technion), Bet Dagan, Jerusalem (Giv’at Ram) and Be’er Sheva (Negev Institute). These stations started , Technion: 35001’E; 32046’N; 230 m. Aviv, Sede Dov: 34047’E; 32006’N; 4 m. Dagan, meteorological station: 34048’E; HILL REGION Har Kena’an: 35030’E; 32058’N; 934 m. Gal’ed (Even Yizhaq) 35004’E; 32033’N; 180 m. Jerusalem, Center: 35013’E; 31046’N; 815 m. Jerusalem, Giv’at Ram: 35011’E; 31046’N; 765 The monthly multi-year average of sunshine the aquifer is bordered by the southern slopes of the Carmel and Tanninim Stream. In the south, it is bordered by the Be’er Sheva Valley. The main flow of water at this aquifer is from the Rosh HaAyin and Tanninim
Stream springs.
HaHof Aquifer: The aquifer spans from
Binyamina in the north to Nir Am in the south. In the east, the aquifer is bordered by the foothills of the mountains and the plain of the Quality of water at the beaches and streams, central mountain ridge and in the west, by the It has a good collection capacity, and it is filled with rainfall, from artificial recharging of flood water and from effluents at selected sites. Height of drilling: Height of drilling point in
The aquifers in Israel are: HaHof Aquifer, Yarqon-Tanninim Aquifer, Western Galilee Water level: Height of the water level in
Aquifer, Eastern Hill Aquifer, and Negev and Arava Aquifers. The water level of the aquifers changes according to, among others, The data were obtained from the Hydrological run-off entering it and pumping activities If there is no way of measuring the water The data presented in the table focus on the two main sources of utilizing ground water in addition, a hydrological model is used to The table presents specific data on a limited number of drillings (out of hundreds) in carried out in only a small percentage of accordance with the recommendations of the Hydrological Service. Water level values were published in relation to Mean Sea Level for the months of: April (Spring), and October (Fall), to indicate Water Level of the Sea of Galilee and the
Sea and Water Salinity in the Sea of
observation drillings, as in exploratory drills, its water level is therefore essential as it Water level values presented in the table are Salinity values presented in the table are the Information on the water level of the Sea of Galilee and the Dead Sea in these time series may provide an indication of short-term as Yarqon-Tanninim
extends from the ridges of the Judea and constitute a basis for understanding the Samaria hills to the east and reaches the Mediterranean coast in the west. In the north, changes resulting from human intervention in the ecosystem. In addition, the time series provide important information on natural Cl (mg/liter)
fluctuations of water. There is no Israeli standard yet for the quality of the Sea of All the water level values appear with a minus sign, since the height of Sea of Galilee and Data on the water level in the Sea of Galilee Hydrological Service. Data on the salinity of indicate the maximum water level for a given the Sea of Galilee were obtained from the Hydrological Service for the years 1960-1968 (November, December) indicate the minimal water level. The value presented in the table Limnological Laboratory (Nishri et al.) for the is the result of the first measurement of that The statistical parameters of salinity are As of 1969, all salinity tests have been carried calculated out of a series of observations. out at one sampling point in the center of the An observation is the weighted average of representative point of the average salinity of Water salinity: the parameter which
constitutes the main element in determining possible uses of water. Accepted practice is neighbour” imputation methods or other to determine the salinity by the concentration of chlorides in the water (Cl), measured by milligrams of chlorides per liter of water (mg/l). According to its salinity, the quality of water is measurement in one of the permanent depths from which an observation is calculated during the years 1969-1991, the CBS uses an imputation of a datum, which is the average of measurements at the same depth and in the same month for 3 consecutive years. In certain instances, the datum of the measurement was imputed on the same date. List of Localities, Their Population and Codes 31.12.2003


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