首页> 外文期刊>Annals of Agricultural Research >Change in climate water balance and agro-climatic situational analysis for crop planning in southern Odisha
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Change in climate water balance and agro-climatic situational analysis for crop planning in southern Odisha

机译:奥里萨邦南部的气候水平衡变化和农业气候形势分析,用于作物计划

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摘要

Tribal dominant undivided Koraput district of southern Odisha represents four Agro-climatic zones viz. Eastern Ghat High Land, North Eastern Ghat, South Eastern Ghat and Western Undulating zones. Based on altitude, soil type, rainfall, irrigation, topography and cropping pattern, each agro-climatic zone is sub-divided into different agro-ecological situations (AESs). As water balance is an important tool to develop plan for optimal utilization of scarce water, the parameters of climatic water balancefor three agro-climatic zones of southern Odisha were computed by employing Thornthwaite (1948) method using weather parameters like rainfall, temperature etc, for three decades 1971-1980, 1981-90 and 1991-2000 and 1971-2000 (i.e. for the normal year).Potential evapotranspiration was determined by Hargreaves method. From the decadal change of water balance it was found that in different block years the precipitation (P) almost remaining the same, the potential (PE) and actual evapotranspiration (AE) have increased from 1702.6 to 1774 mm and 937.7 to 960.6 mm, respectively. The water surplus (WS) has decreased from 493 to 449 mm and water deficit (WD) has increased from 765 to 814 mm. The normal water balance (1971-2000) shows that the average annualPE, P, AE, WD and WS is 1689.9 mm, 1397.7 mm, 946.1 mm, 743.8 mm and 470.4 mm, respectively. During October to May, there has been a constant spell of deficit. However, soil has been almost completely recharged during the month of June. Based on the criteria of Moisture Index (MI) on annual basis, the region is slightly moist. In rabi season it is extremely dry and in kharif it is wet. The length of crop growing season has been assessed and found as normal varying from 163 to 180 days with slight moisture stress and 178 to 210 days with moderate stress condition. Further, the season starts from mid May to November 1 to 23 and accordingly a remunerative alternate crop planning has been suggested.
机译:奥里萨邦南部部族的主要未分割科拉普特地区代表着四个农业气候区。东高止山脉高地,东北高止山脉,东南高止山脉和西部起伏地带。根据海拔,土壤类型,降雨,灌溉,地形和种植方式,将每个农业气候区细分为不同的农业生态状况(AES)。由于水平衡是制定稀缺水最佳利用计划的重要工具,因此,采用Thornthwaite(1948)方法,利用降雨,温度等天气参数,计算了奥里萨邦南部三个农业气候区的气候水平衡参数。 1971-1980年,1981-90年和1991-2000年以及1971-2000年(即正常年份)的三个十年。通过Hargreaves方法确定潜在的蒸散量。根据水平衡的年代际变化,发现在不同的区块年份中,降水量(P)几乎保持不变,势能(PE)和实际蒸散量(AE)分别从1702.6毫米增加到1774毫米,从实际蒸散量增加到937.7毫米到960.6毫米。剩余水(WS)从493毫米减少到449毫米,缺水(WD)从765毫米增加到814毫米。正常的水平衡(1971-2000年)显示年平均PE,P,AE,WD和WS分别为1689.9毫米,1397.7毫米,946.1毫米,743.8毫米和470.4毫米。在十月至五月期间,经常出现赤字。但是,在6月份,土壤几乎已完全充满。根据年度水分指数(MI)的标准,该地区略湿。在狂犬病季节,它非常干燥,而在卡里夫,它是湿的。已经评估了作物生长季节的长度,发现正常情况下,轻度水分胁迫为163至180天,中度胁迫条件为178至210天。此外,该季节从5月中旬至11月1日至23日开始,因此建议采用有酬替代作物计划。

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