Lessons Learnt from Long-Term Experiments on No-Till Systems in Semi-arid Regions

Author(s):  
Mahesh K. Gathala ◽  
Alison M. Laing
2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Ranjini Ray ◽  
Atreyee Bhattacharya ◽  
Gaurav Arora ◽  
Kushank Bajaj ◽  
Keyle Horton ◽  
...  

AbstractUsing information contained in the eighteenth to twentieth century British administrative documents, preserved in the National Archives of India (NAI), we present a 218-year (1729–1947 AD) record of socioeconomic disruptions and human impacts (famines) associated with ‘rain failures’ that affected the semi-arid regions (SARs) of southern India. By mapping the southern Indian famine record onto long-term spatiotemporal measures of regional rainfall variability, we demonstrate that the SARs of southern India repeatedly experienced famines when annual rainfall reduced by ~ one standard deviation (1 SD), or more, from long-term averages. In other words, ‘rain failures’ listed in the colonial documents as causes of extreme socioeconomic disruptions, food shortages and human distress (famines) in the southern Indian SARs were fluctuations in precipitation well within the normal range of regional rainfall variability and not extreme rainfall deficits (≥ 3 SD). Our study demonstrates that extreme climate events were not necessary conditions for extreme socioeconomic disruptions and human impacts rendered by the colonial era famines in peninsular India. Based on our findings, we suggest that climate change risk assessement should consider the potential impacts of more frequent low-level anomalies (e.g. 1 SD) in drought prone semi-arid regions.


2019 ◽  
pp. 132-152
Author(s):  
S. A. Yudin ◽  
V. P. Belobrov ◽  
V. K. Drediger ◽  
A. M. Grebenikov ◽  
A. J. Aydiev ◽  
...  

Author(s):  
Adriana Príncipe ◽  
Alice Nunes ◽  
Pedro Pinho ◽  
Lúcio do Rosário ◽  
Otília Correia ◽  
...  

2012 ◽  
Vol 7 (No. 1) ◽  
pp. 36-44 ◽  
Author(s):  
S. Kanzari ◽  
M. Hachicha ◽  
R. Bouhlila ◽  
J. Battle-Sales

Arid and semi-arid regions face the risk of soils and aquifers salinization. Rainy events are rare which is characteristic of these regions. They play a significant role in the leaching of salts from topsoil to deeper layers, which increases the risk of aquifers salinization. For this reason, a plot was selected in the semi-arid region of Bou Hajla (Central Tunisia). The simulation of water and salts dynamics was carried out by Hydrus-1D. Model calibration was realised on a flood irrigation experiment during 10 days and in a depth of 4 m. The hydrodynamic parameters were determined by inverse modelling. Model validation was performed successfully during 577 days. The simulation of water and salts dynamics has allowed the analysis of two scenarios: (i) the effect of a very rainy event (> 50mm/day) on the dynamics of salts. This type of event allows leaching of the accumulated salts in the topsoil which promotes their burial in the depth; (ii) the long-term evolution of the saline profile in 20 years showed the cyclical nature of salts leaching in the topsoil, the permanent accumulation of salts in the depth of around 2 m, and a continuous leaching in the deeper layers (around 4 m), which may increase groundwater contamination risk.


2021 ◽  
Vol 206 ◽  
pp. 104840
Author(s):  
Humberto Blanco-Canqui ◽  
Charles Shapiro ◽  
Paul Jasa ◽  
Javed Iqbal

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