915 resultados para Storm beds


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毛乌素沙地是我国十二大沙漠之一,地处北方干旱半干旱区向亚湿润区过渡地带,长期以来,不合理的人类土地利用,结合当地脆弱的环境生态特征,引起了严重的现代荒漠化过程,是我国北方荒漠化研究的重点地区。本文着重从自然和人文学科密切合作的角度,对毛乌素沙地土地利用/土地覆被变化的内在作用机制进行了研究,得到以下主要结论: 1. 利用多年实地观测数据资料,考察了毛乌素沙地四种主要草地类型代表性植物群落地上生物量响应气候因子波动的变化规律,建立了植物地上生物量对气候因子的逐月回归模型,揭示出如下规律:①各种气候因子对不同类型草地以及同一类型不同生长阶段草地都产生不同的影响作用;②同一气候因子在植物不同生长阶段上,对生物量形成的重要性程度存在差异:③在植物生长期内,每个生长阶段的生物量都对后一时期的生物量产生显著影响,说明植物生长的连续性对于生物量的形成和积累是重要的;④在植物的凋枯期,各种气候因子基本上都不对生物量产生显著影响;⑤水分因子对毛乌素沙地几乎各种类型草地的生物量,都是重要的影响因子,毛乌素沙地降水状况在不同年份的显著波动对草地植物地上生物量的影响,不仅直接构成了土地覆被变化的重要组成部分,而且还影响到土地利用的方式、方法和后果。 2. 在考察毛乌素沙地草地地上生物量对气候因子变化的响应规律中,利用逐月动态回归建模方法改进了传统的累积气候因子回归建模方法。逐月回归模型与累积回归模型的比较显示,逐月动态回归模型的优势表现在三个方面:①可以提供累积回归模型无法揭示的作用规律;②模拟更加精确;③可以预测不同气候条件下群落地上生物量的变化范围。 3. 利用风速、降水和潜在蒸发等气象记录资料,建立了毛乌素沙地气候因子影响沙尘暴频率的作用模型,定量地考察了沙地各处气候因子对沙尘暴频率的影响作用。研究表明,气候因素是导致毛乌素沙地沙尘暴发生的主导原因,在沙地各处,气候因子可以解释沙尘暴频率分布格局总信息的比率分别为:乌审召83.6%,乌审旗77.5%,河南82.4%,鄂托克旗79.8%,新街73.1%,伊金霍洛旗82%。 4. 在定量考察气候因素对沙尘暴频率影响作用的基础上,对影响沙尘暴频率格局的自然和人为因素进行了定量分离,研究表明:人为影响因素对对沙尘暴发生起次要作用,解释沙尘暴频率分布格局信息的比率分别为:乌审召16.4%,乌审旗22.5%,河南17.6%,鄂托克旗20.2%,新街26.9%,伊金霍洛旗18%。 自然和人为因素影响作用的定量分离研究表明,毛乌素沙地人为因素的影响作用表现出空间上的差异性:①从方位上说,呈现自东向中、西部递减的梯度:②从地点上说,城镇附近人为影响作用远高于农村地区;③从土地利用方式上说,农垦种植业区域高于畜牧业区域。 5. 在实地观测基础上,建立了裸露沙面和植被覆盖沙面风蚀输沙率模型,定量考察了植被覆盖率与风蚀输沙率之间的关系。研究表明:当植被覆盖率达到60%以上,可以保护地表土壤使风蚀在大多数条件下不致发生;当覆盖率达到40%,可以使风蚀输沙大为减少;而当植被覆盖率低于10%,植被覆盖基本不能对地表土壤起到有效的防护作用。 6. 应用植被覆盖地表风蚀输沙率模型,考察了沙地不同风速条件下植被有效覆盖率。根据当地气象台站的多年气象记录,沙地最大风速在20m/s左右,这样的风速条件下,保证风蚀不致发生的植被有效覆盖率为65%左右;在沙地常见的大风风速14-16m/s下,植被有效覆盖率大致为50-55%;对于沙地一般的中等风速l0-12m/s.植被有效覆盖率为40%。植被覆盖对风蚀的影响作用也可以理解为,植被覆盖使沙粒起动风速发生了增大效应,研究表明:与裸露沙面沙粒起动风速4.5m/s对照,70%植被覆盖率使起动风速改变为15.4m/s;60%植被覆盖率使起动风速改变为12.1m/s;40%植被覆盖率使起动风速改变为8.Om/s;而在10%植被覆盖条件下,起动风速为5.Om/s,改变量很小,说明植被覆盖的保护作用极其有限。 7. 基于野外实地观测,比较了沙地五种常见植物种和二种人工防护材料防风效应上的差异。研究表明,防风效应由高到低的次序是,沙蒿>芨芨草>杨柴和牛心朴子>沙障>栅栏>旱柳;就乔、灌、草和人工材料而言,防风效应的次序是,灌木植被>草本植被>人工材料>乔木植被。植物和人工防护材料降低风速的比率与风速呈现二次函数关系,不同植物种或人工材料,降低风速比率都表现出不同的规律,在一般情况下,降低风速效应随着风速的增大而降低。 8. 通过不同植物种防风效应的比较研究,对毛乌素沙地植被生态建设的实践有一定的指导意义。毛乌素沙地的植被建设中对植被类型和植物种类的选择,应该遵循如下原则:①选取防风固沙效应好的植物种类;②应该考虑植物水分供给与需求的平衡状况,实行适地适树;③植物防护效应应该与当地风蚀气候在时间上较好地匹配,在春季等风蚀严重季节,植被覆盖应该具有较好的防风效应。 9. 在现实中,各种影响风蚀的因素是同时发挥作用的。将风蚀影响因素分解为风速、湿润度和植被覆盖率(以及植被类型)三个方面,在此基础上,建立了风蚀影响因素的综合作用的概念模型和沙丘活动性指数定量模型。湿润程度低、风速高、植被覆盖率低的地区,是风蚀最为严重的地区;在湿润程度高、风速低、植被覆盖率高的地区,是风蚀最弱的地区;在其他地区,风蚀状况根据三个方面因素的综合状况来决定。 10. 利用风蚀影响因子综合作用的沙丘活动性指数模型,从空间、时间、植被类型变化角度,考察了毛乌素沙地的风蚀变化状况。得到如下结论:①随着空间变化,风速、降水等气候因素也随之存在差异,导致沙丘活动性指数的变化规律是,西北部鄂托克旗沙丘活动性最高,乌审旗次之,其他几个站差别不太显著,这是由各地降水、气温、沙粒粒径等因素共同决定;②随着时间的变化,气候、植被生长等方面的状况随之发生改变,导致沙丘活动性发生变化,春季最高,冬季次之,夏秋季最低:③随着沙丘植被覆盖类型的变化,沙丘活动性也发生显著变化,在一般情况下,乔木覆盖沙丘活动性>草本植物覆盖沙丘>灌木覆盖沙丘。 11. 在实地调查土地利用现实状况及其社会、经济和政策影响因素的基础上,建立了我国北方干旱半干旱区土地利用决策机制的概念模型,分析了与土地利用密切相关的农牧民一政府一环境科学家这三个社会群体对土地利用的立场和影响作用力上的差异,分析了毛乌素沙地土地利用的现状及其影响因素,探讨了现实中不可持续土地利用行为发生的社会、经济和政策原因。 12. 在实地调查基础上,分别利用产出一费用分析法和过程影响因素分析法,建立了毛乌素沙地土地利用经济收益的定量模型。产出一分析研究表明,无论是农垦种植业,还是草地畜牧业,农牧民从这两种土地利用方式都只能获得较低下的经济收益。造成这种状况的原因,主要在于两个方面:一是低下且不断处于波动之中的农牧业产品物价,二是沉重的农牧业税收。 13. 将影响农牧业产出的因素,划分为四个方面:土地面积(牲畜头数)、环境状况、管理水平和利用强度,在此基础上建立了定量的影响作用模型。研究表明:环境状况指数每增加0.1,农牧业经济收益增加26%;管理水平因子每提高0.1,农牧业经济收益增加12.7%;农牧业经济收益最优的土地利用强度在0.4左右,在此之前,随着利用强度的增加,经济收益随之增大,而在此之后,随着利用强度的增大,经济收益逐渐降低,当土地利用强度达到0.9左右时,呈现负的经济收益。 14. 毛乌素沙地实施土地资源可持续利用,必须从技术的革新和社会经济政策等因素的调整两条途径同时入手,二者缺一不可。通过改进和应用节水灌溉、风能光能利用、生物增产技术,尽可能地提高各种资源的利用效率;通过应用免耕或浅耕技术,尽量减轻土地利用对资源和环境的破坏;通过栽培、速生技术,提高植被建设的成效和速度。而通过税收、物价政策的调整,尽可能地提高农牧民经济收益增长的速度,减轻土地利用压力;通过政府与人民之间对话和合作机制的建立,让广大农牧民参与到土地利用的决策和管理的过程中去;通过土地利用管理政策、措施的调整和完善,调动农牧民保护资源的积极性和自觉性;通过激励机制的建立,引导农牧民土地利用向着可持续的方向发展。 15. 实现毛乌素沙地土地资源可持续利用的有效途径,在于这样几个方面:①建立和完善政府及其管理部门与人民之间有效的对话和合作机制,让广大农牧民参与到土地利用决策和管理的过程中去:②实行产业结构调整,转变片面追求经济增长的做法,制订适应当地自然条件和生态特征的发展模式;③降低农牧业税收、稳定并提高农牧业产品的物价,增加农牧民经济收入,减轻土地利用压力;④进一步改进和完善土地利用管理政策和法规;⑤建立有效激励机制,引导农牧民土地利用向着可持续的方向发展:⑥努力改进节水灌溉技术、生物增产技术,提高土地利用的科技水平:⑦改进环境保护和植被建设决策的科学性,提高植被建设的成效。

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Comparison between past changes in pollen assemblages and stable isotope ratios (deuterium and carbon) analyzed in the same peat core from Tierra del Fuego at latitude 55°S permitted identification of the relative contribution of precipitation versus temperature responsible for the respective change. Major steps in the sequence of paleoenvironmental changes, such as at 12700, 9000, 5000, and 4000 years ago are apparently related only to increase in precipitation, reflecting the latitudinal location and intensity of the westerly storm tracks. On the other hand, high paleoenvironmental variability, which is characteristic for the late-glacial and the latest Holocene, is related to temperature variability, which affects the relative moisture content. Comparison with other paleoenvironmental records suggests that the late-glacial temperature variability is probably related to variability in the extent of Antarctic sea-ice, which in turn appears to be related to the intensity of Atlantic deep-water circulation. Temperature variability during the latest Holocene, on the other hand, is probably related to the dynamics of the El Niño/Southern Oscillation.

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EXTRACT (SEE PDF FOR FULL ABSTRACT): This report shows that the mean wintertime polar-front jet stream structure consists of three long waves. Prominent ridges in the jet stream flow occur near the longitudes of India, eastern Pacific/west coast of North America, and eastern Atlantic/British Isles; prominent troughs occur near the longitudes of the Middle East, western Pacific, and western Atlantic/east coast of North America. ... One of the climatological ridges occurs along the west coast of North America ... just off the central Oregon coast. The position of the jet stream at this location appears to be the main reason most Pacific storms pass to the north of California. Sustained rainfall in northern and central California occurs only when the storm track is displaced southward of this climatological position.

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Major controls on river salinity (total dissolved solids) in the western United States are climate, geology, and human activity. Climate, in general, influences soil-river salinity via salt-balance variations. When climate becomes wetter, river discharge increases and soil-river salinity decreases; when climate becomes drier river discharge decreases and soil-river salinity increases. This study characterizes the river salinity response to discharge using statistical-dynamic methods. An exploratory analysis of river salinity, using early 1900s water quality surveys in the western United States, shows much river salinity variability is in response to storm and annual discharge. Presumably this is because river discharge is largely supported by surface flow.

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EXTRACT (SEE PDF FOR FULL ABSTRACT): Since 1986, the U.S. Geological Survey and National Weather Service have operated a warning system for debris flows triggered by severe rainstorms in the San Francisco Bay region. The NWS tracks storm systems as they approach the region, forecasts precipitation, and observes rainfall with a network of radiotelemetered rain gauges (ALERT). The USGS also monitors ALERT data and compares the observed and forecast rainfall to thresholds for debris-flow initiation. Both groups jointly assess debris-flow hazards and issue public advisories when rainfall conditions reach or approach critical levels.

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EXTRACT (SEE PDF FOR FULL ABSTRACT): Torrey pine (Pinus torreyana Parry ex Carr.) has one of the most limited geographical ranges and population size in the Pinus genus; it is present only on Santa Rosa Island and on the coast between San Diego and Del Mar, where our research was conducted. A 168-year chronology (1827-1994) was developed using 28 increment cores extracted from 15 living and 2 dead stranding trees at Torrey Pines State Reserve, San Diego, California. ... The spatial correlation with western North America winter and spring precipitation, as well as with published tree-ring chronologies, indicates a connection with the American Southwest. Global correlation maps with winter sea level pressure and sea surface temperature are consistent with the hypothesis that San Diego precipitation is affected by a southerly displaced North Pacific storm track and by warmer water farther south, both leading to higher transport of lower latitude moisture.

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Mafia waters in the western Indian Ocean on the east coast of Africa is a natural attractive area for fishing. It has extensive coral beds which harbour good fish life and attracts sport fishery in the area. About 12 commercially important fishes listed are caught by sports fishermen. The data indicates that this area can become an attractive centre for sports fishery almost throughout the year with peak season from November to February. Long-term planning of the fishery is necessary. The conservation measures should be evolved and gan fishing, dynamiting or any other kind of distructive fishing should be prohibited. This area has natural potential to become a sports fishing centre in the future and a great attraction for tourists and anglers.

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Two species of mussels, the green mussel (Perna viridis) and the brown mussel (Perna indica) were cultured using the seed collected from the natural beds of the east and west coasts of India. The results of culture experiments are consolidated and the present status is reviewed. Although the culture experiments gave encouraging results, problems such as mooring of rafts in highly turbulent coastal waters, large scale seed requirements, control of predation, legal problems and marketing of end products require urgent attention before undertaking commercial operations. Some of the major problems of mussel culture are outlined for formulating effective management policies and their implementation for commercial mussel farming in India.

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Historical survey maps of Maryland oyster bars, crab bottoms, and clam beds, by county and watershed. PDF includes two index maps and forty-two survey maps scanned from microfilm.

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The continental shelf between the three and twelve fathom lines, off the Ceylon coast in the Gulf of Mannar is popularly known as the Pearl Banks. Though the area of this plateau is extensive the pearl oysters are concentrated on restricted areas known as "paars". The more productive of these are the Cheval Group of paars and the Moderagam Paar. The Peria Paar and Twynam's Paar though covering larger areas are not dependable as oyster beds. The True Vankalai, Peria Paar Karai and Muthuvarathu Paars are small in extent, but have yielded oysters on a commercial scale. Although the Ceylon Pearl Banks has been commercially fished for centuries, the first scientific investigation of its pearl oysters on an intensive scale was started by Herdman in 1902 (1902-06) and later continued by Hornell (1905-41), Shipley (1904-06), Pearson (1911-33), Jameson (1912-13), Southwell (1910-14) and Malpas (1922-39).

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Current design codes for floating offshore structures are based on measures of short-term reliability. That is, a design storm is selected via an extreme value analysis of the environmental conditions and the reliability of the vessel in that design storm is computed. Although this approach yields valuable information on the vessel motions, it does not produce a statistically rigorous assessment of the lifetime probability of failure. An alternative approach is to perform a long-term reliability analysis in which consideration is taken of all sea states potentially encountered by the vessel during the design life. Although permitted as a design approach in current design codes, the associated computational expense generally prevents its use in practice. A new efficient approach to long-term reliability analysis is presented here, the results of which are compared with a traditional short-term analysis for the surge motion of a representative moored FPSO in head seas. This serves to illustrate the failure probabilities actually embedded within current design code methods, and the way in which design methods might be adapted to achieve a specified target safety level.

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Carp seed traders in Bangladesh are considered as one of the poorest, most vulnerable and least studied sub-population. Millions of fingerlings are transported annually to various parts of the country using bus tops and/or truck-beds in open and hand agitated method by the traders and as a result they encounter mass seed mortality. They are the key players in augmenting aquaculture activities by distributing fish fry and fingerlings to the fish farmers. Assessment of the seed sources and the livelihood of the traders are important to identify their point of entry to the aquaculture sector and further improvement. Status of household asset, income profiles, and risks involved were examined using DFID's sustainable livelihood approach (SLA) framework. Tools used to collect data included group discussions (GD), semi-structured and structured household (HH) survey. Samples (n=637) were randomly drawn purposefully from 10% of the carp seed traders within 11 districts. Sampled HH were classified into six land classes.

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Live clams collected from their natural beds were depurated by starving them in water. Water from their natural environment, potable water from municipal water supply and sodium chloride solution made up to the strength of natural brackish water as well as all these chlorinated at 5 p.p.m. level were used. The acid insoluble ash could be brought down to insignificant level by depuration in natural water for a period of 16-18 h. Bacterial quality of the meat also could be improved by this method. Chlorination of the system at the end of depuration further improves the bacterial quality of the meat.

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Live clams (Villorita cyprinoides) collected from their natural beds were packed in different ways like dry pack, tray pack, in oxygenated water (wet pack) and depurated samples in wet pack. It was found that the packaging in l kg lots in 200 gauge polythene bags with oxygen at a temperature of 20°C could keep them live for 4 days. In tray pack without oxygen and water they can be kept alive for 3 days at 20°C. Temperature seems to be the critical factor in the transportation of live clams. At room temperature both dry and wet pack can be kept for 24 h only. Depuration technique does not appear to be useful in prolonging the storage life of clams in live condition as percentage mortality is more at 48 h both at 20°C and room temperature compared to the non-depurated samples.

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Live clams (Villorita cyprinoides) collected from their natural beds were packed in different ways like dry pack, tray pack, in oxygenated water (wet pack) and depurated samples in wet pack. It was found that the packaging in l kg lots in 200 gauge polythene bags with oxygen at a temperature of 20°C could keep them live for 4 days. In tray pack without oxygen and water they can be kept alive for 3 days at 20°C. Temperature seems to be the critical factor in the transportation of live clams. At room temperature both dry and wet pack can be kept for 24 h only. Depuration technique does not appear to be useful in prolonging the storage life of clams in live condition as percentage mortality is more at 48 h both at 20°C and room temperature compared to the non-depurated samples.