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IMPACT OF CLIMATE CHANGE ON JHARKHAND AGRICULTURE: MITIGATION AND ADOPTION

机译:气候变化对Jharkhand农业的影响:缓解和采用

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Jharkhand state, geographically located at 22 deg 28 min N -25 deg 30 min N latitude and 83 deg 22 min - 87 deg 40 min E Longitude with an altitude up to 1142 m above msl and having humid to sub-humid tropical monsoon type of climate, has a number of agro-climatic/physiographic constraints. Undulating terrain, shallow soil depth, low water retentive capacity and poor fertility of soils, fragmented holdings, high intensity (causing severe soil erosion) often erratically distributed (prolonged dry spells) rainfall and very meagre irrigation potential (10-12percent) are the most important constraints. Hence, agriculture is more difficult, tedious and challenging here than most other parts of the country. A considerable increase in average monthly maximum temperature and consistent increase in rainfall pattern with high variability, in recent decades, has further enhanced the agricultural problems in Jharkhand. Analysis of more than 40 years data of rainfall and temperature, recorded at Agrometeorological observatory located at Kanke (Ranchi) has revealed an increase in occurrence of extreme weather events with marked change in climate of Jharkhand state. The state is privileged to receive good amount of rainfall almost round the year.The annual average of rainfall has shown an increasing trend over the decades, the period 2001-08 being an exception because of the few drought years in this period.. It increased consistently from 1250.5 mm (1961-70) to 1623.5 mm (1991-2000). The quantitative increase in rainfall may be considered as a positive change in Jharkhand but it was associated with simultaneous increase in variability also (cv: 13percent in 1961-70 to 20percent in 1991-2000) which increased the level of uncertainty and possibility of intermittent prolonged dry spells. The increase in annual rainfall was mostly confined in the monsoon period. High intensity rainfall, often received in monsoon months, intensify the problem of soil erosion. Uncertainty on the dates of monsoon onset and its withdrawal also puts a great problem before the farmers. A considerable rise in temperature, over the decades, has been recorded in Jharkhand which might be one of the climatological reasons why the productivity has remained stand still over the decades though the total production has increased due to many other scientific efforts. From 1961 onwards the maximum temperature has been found in increasing trend. The increase in temperature, particularly the maximum temperature has been found to have considerable adverse effect on crop performances, more on the rabi season crops.
机译:jharkhand状态,地理位置为22°22°-25 deg 30 min n纬度和83°22 min-87 deg 40 min e经度,高度高达1142 m以上msl,潮湿地潮湿的热带季风类型气候,有许多农业气候/地理学约束。起伏的地形,浅层土壤深度,低水分保存能力和土壤肥力差,碎片持有,高强度(导致严重的土壤侵蚀)经常不规例地分布(延长干燥的法术)降雨和非常微薄的灌溉潜力(10-12percent)最多重要的限制。因此,农业在这里比大多数其他地区更困难,繁琐和挑战。近几十年来,平均每月最高温度和持续增加降雨量的降雨模式的持续增长,进一步提高了Jharkhand的农业问题。在位于Kanke(Ranchi)的农业气象天文台上记录了40多年的降雨和温度的数据,揭示了贾克手州气候变化的极端天气事件发生的增加。该州的特权是几乎围绕年度的降雨量。降雨年平均平均趋势越来越多的趋势,2001 - 08年期间是由于这一时期的几年少数几年的例外..它增加了始终如一从1250.5 mm(1961-70)到1623.5 mm(1991-2000)。降雨量的定量增加可能被认为是jharkhand的正变化,但它与可变异的同时增加有关(简介:1961-70在1991-2000的1961-70到20次)相关的增加,这增加了不确定程度和间歇性的可能性延长了间歇性的水平干法术。年降雨量的增加主要是在季风期间限制。高强度降雨,经常在季风月收到,加剧土壤侵蚀问题。对季风发病的日期的不确定性及其撤回也在农民面前产生了很大的问题。几十年来,温度较大的升高,在贾克大人中录得可能是虽然在许多其他科学努力所造的总产量增加的情况下,生产力保持仍然存在的气候原因之一。从1961年开始,在增加趋势时已发现最高温度。已经增加了温​​度的增加,特别是最高温度对作物表演具有相当大的不利影响,更多关于rabi季节作物。

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