Unveiling rainfall and erosivity dynamics in Odisha’s varied agro-climatic zones for sustainable soil and water conservation planning

IF 2.8 4区 地球科学 Q3 METEOROLOGY & ATMOSPHERIC SCIENCES
Ch. Jyotiprava Dash, S. S. Shrimali, M. Madhu, Randhir Kumar, Partha Pratim Adhikary
{"title":"Unveiling rainfall and erosivity dynamics in Odisha’s varied agro-climatic zones for sustainable soil and water conservation planning","authors":"Ch. Jyotiprava Dash, S. S. Shrimali, M. Madhu, Randhir Kumar, Partha Pratim Adhikary","doi":"10.1007/s00704-024-05089-0","DOIUrl":null,"url":null,"abstract":"<p>Climate change leads to changes in climatic variables, with rainfall being one of them. Changes in rainfall influence rainfall erosivity and subsequently erosion rates. This study analysed rainfall data from 1901 to 2017 in Odisha, focusing on different agro-climatic zones to discern annual rainfall pattern, its spatial variation, and trend, particularly concerning the rainfall erosivity factor and its impact on soil erosion and agricultural productivity. Notably, the Eastern Ghats Highland region received the highest average annual rainfall of 1578.5 mm, while the Western Undulating Zone received the lowest (1308.4 mm). The rainfall distribution showed spatial variability largely influenced by topography, with areas experiencing orographic lifting receiving higher rainfall. The study observed significant trend in annual rainfall, noting a maximum decline of 1.2 mm yr<sup>−1</sup> in the North Western Plateau, Western Central Table Land, and Western Undulating Zone, whereas the East and South Eastern Plain, Mid Central Table Land, North Eastern Coastal Plain, North Eastern Ghats, and South Eastern Ghats exhibited a noteworthy increase in annual rainfall (0 to 3.9 mm yr<sup>−1</sup>). The decline in rainfall can result in the drying up of water bodies and reduced soil water availability to crop, thereby influencing agricultural production. On the other hand, areas with increased rainfall, may face extreme events which can aggravate soil erosion and thereby loss of soil fertility. Considering the scarcity of pluviographic data in countries like India, Modified Fournier Index (MFI) may be considered as one of the useful methods to capture rainfall’s aggressiveness towards soil erosion through rainfall erosivity (R-factor). Therefore, to evaluate potential soil erosion levels, the Modified Fournier Index method was employed, revealing varying degrees of soil erosiveness across different regions. The Eastern Ghats Highlands exhibited the highest erosion potential. The R-factor, aligned with these spatial patterns, with the Eastern Ghats Highland (12,965.4 MJ mm ha<sup>−1</sup> h<sup>−1</sup> yr<sup>−1</sup>) and South Eastern Ghats (12,242.3 MJ mm ha<sup>−1</sup> h<sup>−1</sup> yr<sup>−1</sup>) regions displaying the highest R-factor values. Furthermore, the research identified areas prone to soil erosion by overlaying R-factor, slope, and land use maps, highlighting vulnerable regions such as Eastern Ghats Highlands, North Eastern Ghats, South Eastern Ghats, and Western Undulating Zone. This comprehensive analysis allows for informed prioritization of conservation efforts and the implementation of appropriate measures like strip cropping of finger millet with groundnut, intercropping finger millet with hedgerows of <i>Gliricidia</i> and <i>Leucaena</i>, bio-engineering measures such as earthen or stone bunds with broom grass in arable land and growing of aromatic grasses like lemon and citronella grass, construction of staggered trenches in non-arable land to mitigate erosion in these susceptible areas.</p>","PeriodicalId":22945,"journal":{"name":"Theoretical and Applied Climatology","volume":"10 1","pages":""},"PeriodicalIF":2.8000,"publicationDate":"2024-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Theoretical and Applied Climatology","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1007/s00704-024-05089-0","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0

Abstract

Climate change leads to changes in climatic variables, with rainfall being one of them. Changes in rainfall influence rainfall erosivity and subsequently erosion rates. This study analysed rainfall data from 1901 to 2017 in Odisha, focusing on different agro-climatic zones to discern annual rainfall pattern, its spatial variation, and trend, particularly concerning the rainfall erosivity factor and its impact on soil erosion and agricultural productivity. Notably, the Eastern Ghats Highland region received the highest average annual rainfall of 1578.5 mm, while the Western Undulating Zone received the lowest (1308.4 mm). The rainfall distribution showed spatial variability largely influenced by topography, with areas experiencing orographic lifting receiving higher rainfall. The study observed significant trend in annual rainfall, noting a maximum decline of 1.2 mm yr−1 in the North Western Plateau, Western Central Table Land, and Western Undulating Zone, whereas the East and South Eastern Plain, Mid Central Table Land, North Eastern Coastal Plain, North Eastern Ghats, and South Eastern Ghats exhibited a noteworthy increase in annual rainfall (0 to 3.9 mm yr−1). The decline in rainfall can result in the drying up of water bodies and reduced soil water availability to crop, thereby influencing agricultural production. On the other hand, areas with increased rainfall, may face extreme events which can aggravate soil erosion and thereby loss of soil fertility. Considering the scarcity of pluviographic data in countries like India, Modified Fournier Index (MFI) may be considered as one of the useful methods to capture rainfall’s aggressiveness towards soil erosion through rainfall erosivity (R-factor). Therefore, to evaluate potential soil erosion levels, the Modified Fournier Index method was employed, revealing varying degrees of soil erosiveness across different regions. The Eastern Ghats Highlands exhibited the highest erosion potential. The R-factor, aligned with these spatial patterns, with the Eastern Ghats Highland (12,965.4 MJ mm ha−1 h−1 yr−1) and South Eastern Ghats (12,242.3 MJ mm ha−1 h−1 yr−1) regions displaying the highest R-factor values. Furthermore, the research identified areas prone to soil erosion by overlaying R-factor, slope, and land use maps, highlighting vulnerable regions such as Eastern Ghats Highlands, North Eastern Ghats, South Eastern Ghats, and Western Undulating Zone. This comprehensive analysis allows for informed prioritization of conservation efforts and the implementation of appropriate measures like strip cropping of finger millet with groundnut, intercropping finger millet with hedgerows of Gliricidia and Leucaena, bio-engineering measures such as earthen or stone bunds with broom grass in arable land and growing of aromatic grasses like lemon and citronella grass, construction of staggered trenches in non-arable land to mitigate erosion in these susceptible areas.

Abstract Image

揭示奥迪沙不同农业气候区的降雨和侵蚀动态,制定可持续的水土保持规划
气候变化导致气候变量发生变化,降雨量就是其中之一。降雨量的变化会影响降雨的侵蚀性,进而影响侵蚀率。本研究分析了奥迪沙邦 1901 年至 2017 年的降雨数据,重点关注不同农业气候区,以了解年降雨模式、空间变化和趋势,尤其是降雨侵蚀因子及其对土壤侵蚀和农业生产率的影响。值得注意的是,东高止山脉高原地区的年平均降雨量最高,达 1578.5 毫米,而西部起伏地带的降雨量最低(1308.4 毫米)。降雨分布的空间变化主要受地形影响,地形抬升地区的降雨量较高。研究观察到年降雨量的显著变化趋势,注意到西北高原、中西部台地和西部起伏带的年降雨量最大下降了 1.2 毫米,而东部和东南部平原、中部台地、东北部沿海平原、东北高原和东南高原的年降雨量则显著增加(0 至 3.9 毫米/年)。降雨量的减少会导致水体干涸和作物土壤水分供应减少,从而影响农业生产。另一方面,降雨量增加的地区可能会面临极端事件,从而加剧土壤侵蚀,导致土壤肥力下降。考虑到印度等国家缺乏雨水图数据,修正的富尼耶指数(MFI)可被视为通过降雨侵蚀率(R-因子)捕捉降雨对土壤侵蚀的侵蚀性的有效方法之一。因此,为了评估潜在的土壤侵蚀程度,我们采用了修正富尼耶指数法,结果显示不同地区的土壤侵蚀程度各不相同。东高止山脉高地的土壤侵蚀潜力最大。R 因子与这些空间模式一致,东高止山脉高地(12,965.4 兆焦耳毫米公顷-1 小时-年-1)和东南高止山脉(12,242.3 兆焦耳毫米公顷-1 小时-年-1)地区的 R 因子值最高。此外,研究还通过叠加 R 系数、坡度和土地利用地图,确定了易发生土壤侵蚀的地区,突出显示了东高止山脉高地、东北高止山脉、东南高止山脉和西部起伏带等脆弱地区。通过这种综合分析,可以对保护工作的轻重缓急做出明智的排序,并实施适当的措施,如将小米与落花生进行带状种植,将小米与格利西达树(Gliricidia)和鹅掌楸(Leucaena)树篱进行间作,采取生物工程措施,如在可耕地上用扫帚草筑起土堤或石堤,种植柠檬和香茅等芳香植物,在非耕地上修建交错的壕沟,以减轻这些易受侵蚀地区的水土流失。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Theoretical and Applied Climatology
Theoretical and Applied Climatology 地学-气象与大气科学
CiteScore
6.00
自引率
11.80%
发文量
376
审稿时长
4.3 months
期刊介绍: Theoretical and Applied Climatology covers the following topics: - climate modeling, climatic changes and climate forecasting, micro- to mesoclimate, applied meteorology as in agro- and forestmeteorology, biometeorology, building meteorology and atmospheric radiation problems as they relate to the biosphere - effects of anthropogenic and natural aerosols or gaseous trace constituents - hardware and software elements of meteorological measurements, including techniques of remote sensing
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信