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The paper discusses the definitions and distinctions between drought, famine, and aridity, emphasizing the importance of understanding these terms in the context of climate and social conditions. It outlines the four primary types of drought: meteorological, hydrological, agricultural, and socio-economic, detailing their characteristics and impacts. Furthermore, it describes the operating procedures for drought management in Pakistan, highlighting the roles of various governmental and local bodies in monitoring and responding to drought conditions, aiming to enhance resilience in agriculture and the broader economy.
Climate changing affected the life of people. Because of they have to managing their living via farming, gardening and husbandry. Sometimes in drought periods not only lose economical source but also lose theirs drink water and have to use from waters how carry by tanker from far way. Drought effected to be secret at parts of farming and gardens in Nain County. During years of 1999 to2003, the most intensive droughts happened in counties of Isfahan province. In this research, struggle to drought compared between damages of drought in Nain county with other counties in province. The aim of this research, at first is comparison between damages of drought in Nain County with other counties and discovers methods for lessening the effect of drought in Nain County. Method of research is use analysis, descriptive, and statistical that base matter are provided from agriculture organization and statistical year book of meteorological organization and also vulnerable data achieve from unpredictable disaster office. Nevertheless, we compare tiller lands, which were damaged during disaster period in all over of the province to Nain County with same effects and accounted damage quantity in these parts of agricultural, and gardens. For each parts of these research accounts to method of descriptive in Spss and Excel and in other part this Information is shown by Arc-G-IIS in the computer.
Environment Conservation Journal
Drought is one of the important natural disasters which lead to maximum severity to human among all others. The vulnerability increases with the resource poor nature of developing and under developing nations. Considering the extent of rainfed area in India, the vulnerability to drought is higher compared to other peer nations. It has implications on agriculture, livestock, fisheries, rural employment, human nutrition and health. However, the impact initiates with crop production and encompasses livestock in medium term which has severe economic implications for farmer. Therefore, it is desirable to present an extensive study on the impact of drought on major crops and livestock in India. Further, we have also emphasized on the remedial measures to be followed for crop production and livestock.
Advances in Atmospheric Sciences, 2017
In this study, we investigate the spatiotemporal characteristics of drought in India and its impact on agriculture during the summer season (April-September). In the analysis, we use Standardized Precipitation Evapotranspiration Index (SPEI) datasets between 1982 and 2012 at the six-monthly timescale. Based on the criterion SPEI < −1, we obtain a map of the number of occurrences of drought and find that the humid subtropical Upper Middle Gangetic Plain (UMGP) region is highly drought-prone, with an occurrence frequency of 40%-45%. This UMGP region contributes at least 18%-20% of India's annual cereal production. Not only the probability of drought, but the UMGP region has become increasingly drought-prone in recent decades. Moreover, cereal production in the UMGP region has experienced a gradual declining trend from 2000 onwards, which is consistent with the increase in drought-affected areas from 20%-25% to 50%-60%, before and after 2000, respectively. A higher correlation coefficient (−0.69) between the cereal production changes and drought-affected areas confirms that at least 50% of the agricultural (cereal) losses are associated with drought. While analyzing the individual impact of precipitation and surface temperature on SPEI at 6 month timescale [SPEI (6)] we find that, in the UMGP region, surface temperature plays the primary role in the lowering of the SPEI. The linkage is further confirmed by correlation analysis between SPEI (6) and surface temperature, which exhibits strong negative values in the UMGP region. Higher temperatures may have caused more evaporation and drying, which therefore increased the area affected by drought in recent decades.
Water International, 1985
Methodology to characterize meteorological drought and drought frequency curves have been developed for the drought prone Hazaribagh district, Jharkhand, India. The annual and monsoon seasonal rainfall data for a period of 80 years (1913 – 1992) were analyzed to determine excess and deficit from normal. The annual and seasonal rainfall follows log normal and normal distribution respectively. Meteorological drought is investigated by various methods and using proposed methodology. Based on seasonal rainfall of 80 years the proposed methodology classified 45 years (56.25%) as drought years out of which incipient, large, severe, disastrous and extreme drought years were 12 (15.55%), 21(27.77%), 8 (10%), 3 (3.75%) and 1(1.25%) respectively. Drought indices were also developed and year 1966 was classified as the extreme drought year of the area. Multiyear drought characteristic reveals that as drought duration increased from 2 to 6 years the mean severity increased with increasing variability, though the mean drought intensity also increased gradually, but with decreasing variability.
Atmosphere, 2022
Droughts have been identified as an environmental hazard by environmentalists, ecologists, hydrologists, meteorologists, geologists, and agricultural experts. Droughts are characterised by a decrease in precipitation over a lengthy period, such as a season or a year, and can occur in virtually all climatic zones, including both high and low rainfall locations. This study reviewed drought-related impacts on the environment and other components particularly, in South Africa. Several attempts have been made using innovative technology such as earth observation and climate information as recorded in studies. Findings show that the country is naturally water deficient, which adds to the climate fluctuation with the average annual rainfall in South Africa being far below the global average of 860 mm per year. Drought in South Africa’s Western Cape Province, for example, has resulted in employment losses in the province’s agriculture sector. According to the third quarterly labor force sur...
Weather and Climate Extremes, 2018
2016
Drought has been a threat to human existence throughout history. Today, as in the past, drought alters the course of civilizations. It is not merely a physical phenomenon, but the result of an interplay between a natural event (precipitation deficiencies due to natural climatic variability on varying timescales) and the demand placed on water supply by human-use systems. Extended periods of drought have resulted in significant economic, environmental, and social impacts, including food supply disruptions, famine, massive soil erosion, migrations of people, and wars. Human activities often exacerbate the impacts of drought (e.g., the Dust Bowl in the Great Plains, the Sahelian drought of the early 1970s). This trend appears to be accelerating because of the increasing demand being placed on local and regional water resources as a result of the earth's rapidly expanding population. Recent droughts in developing and developed countries and the concomitant impacts and personal hardships that resulted have underscored the vulnerability of all societies to this natural hazard. It is difficult to determine whether it is the frequency of drought that is increasing, or simply societal vulnerability to it.
Weather, Climate, and Society, 2019
In the prevailing climate change scenario, to cope with drought, it is necessary to understand the characteristics of meteorological droughts in water-scarce regions to formulate judicial plans for the utilization of water resources. The present investigation, therefore, endeavored to assess the intensity and frequency of droughts over the five semiarid river basins in Maharashtra during the past (1980-2013) and future (2015-50). The study was carried out with the application of standardized precipitation index (SPI) methodology. The agricultural and satellite [normalized difference vegetation index (NDVI)] data were analyzed to understand the effects of meteorological droughts. Although the study area experienced three severe rainfall droughts in 1985/86, 2002/03, and 2011/12, higher frequency of low-intensity droughts is observed, particularly after 2000. The estimation suggests occurrence of moderate, severe, and extreme droughts once in 6, 28, and 50 years, respectively. Among the selected basins, the Agrani, the Karha, and the Man are expected to experience intense droughts and hence require special attention in drought management. The study also highlights that El Niño events considerably retard the monsoon rainfall. However, the occurrence of the positive phase of the Indian Ocean dipole in the El Niño years reduces the intensity of droughts. As agricultural productivity and cropped areas heavily depend on the monsoon rainfall, the meteorological droughts result in agricultural droughts. Moreover, the future warming (by 1.028C) over the study area is very likely to exacerbate the meteorological droughts (estimated to occur in the 2030s) and increase the agricultural water demand, further adding to an already difficult water management challenge in the study basins.
The Handbook of Environmental Chemistry, 2018
Drought by itself cannot be considered a disaster. However, if its impacts on local people, economies and the environment are severe and their ability to cope with and recover from it is difficult, it should be considered as a disaster. Droughts and floods are a recognizable category of natural risk. Hydrological assessments of drought impacts require detailed characteristics. We propose a new conceptual framework for drought identification in landscape with agricultural use. We described hydrological drought characteristics with impacts at the agricultural landscape and food security and the issues related to drought water management. In the past, the Slovak Republic was not considered a country immediately threatened with drought. The situation had changed at the turn of the millennium, especially after the extreme weather conditions in 2014 and also in 2015, when, for example, the historical minima were recorded.
2013
The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use. While the advice and information in this book are believed to be true and accurate at the date of publication, neither the authors nor the editors nor the publisher can accept any legal responsibility for any errors or omissions that may be made. The publisher makes no warranty, express or implied, with respect to the material contained herein.
International Journal of Research Studies in Agricultural Sciences
Stress is a change of the normal growth, development and productivity of crop plants and that is outside the normal range of homeostatic control. Among stresses, abiotic stress is caused due to moisture, temperature, mineral (deficiency/toxicity), salinity, soil acidity/soil P H. Drought is the primary cause of crop yield loss among abiotic factors around the world. It is a major problem in world, leading to food shortages and is a challenge for smallholder farmers to produce enough crop grain when rainfall is low and erratic. Climate change is the main cause of biotic and abiotic stresses, which have adverse effects the world's crop production and productivity. Crop production is determined by the existence of sufficient rain fall, especially in areas where crop production is totally relied on rain fall, there is always risk of crop failure or yield loss due to moisture stress. In severe cases, the stress could lead to total crop loss. This day, increasing crop yield is required to meet the needs of increasing population growth, however yield reduction is observed in areas where drought is predominantly devastated crop production. Short duration drought stress mostly reduces grain yield while prolonged drought stress leads to complete death of plant. Drought stress occurs at different stages of growth and adversely affect yield and yield related traits, which lead to reduction in yield. The effect of drought stress is mainly depending on the developmental stage of the plant, degree and duration of the stress, genotypic capacity of species and environmental interactions. Crop plants have adaptation strategies to survive under drought stress by the development of various morphological, physiological and biochemical mechanisms. However, a plant may exhibit more than one strategy to cope with drought stress. Drought resistance is the mechanism(s) causing minimum loss of yield in a drought condition. Drought escape, dehydration avoidance, reduced transpiration or physiological factors are some drought resistance mechanisms. Drought resistant genotypes maintain high photosynthesis under moisture stress condition by restricting transpiration water loss. Finally, the global food security is threatened by climate change and the most challenging in the 21 st century to supply sufficient food for the increasing world population. The use of well adapted and high-yielding varieties with resistance to drought stress is important to reach maximum yield potential as long as possible through minimizing the risk of climate change. Climate-smart agriculture is the only way to reduce the negative impact of climate variations on crop adaptation, before it might affect global crop production drastically.
Advances in Meteorology, 2016
Water, 2020
Water is the most important resource for sustainable agriculture in arid and semi-arid regions, where agriculture is the mainstay for rural societies. By relating the water usage to renewable water resources, we define three stages from sustainable to unsustainable water resources: (1) sustainable, where water use is matched by renewable water capacity, ensuring sustainable water resources; (2) transitional, where water use occasionally exceeds renewable water capacity; and (3) unsustainable, with lack of water resources for agriculture, society, and the environment. Using available drought indicators (standardized precipitation index (SPI) and streamflow drought index (SDI)) and two new indices for agricultural drought (overall agricultural drought index (OADI) and agricultural drought index (ADI)), we evaluated these stages using the example of Fars province in southern Iran in the period 1977-2016. A hyper-arid climate prevailed for an average of 32% of the province's spatio-temporal coverage during the study period. The area increased significantly from 30.6% in the first decade (1977-1986) to 44.4% in the last (2006-2015). The spatiotemporal distribution of meteorological drought showed no significant negative trends in annual precipitation during 1977-2016, but the occurrence of hydrological droughts increased significantly in the period 1997-2016. The expansion of irrigated area, with more than 60% of rainfed agriculture replaced by irrigated agriculture (especially between 1997 and 2006), exerted substantial pressure on surface water and groundwater resources. Together, climate change, reduced river flow, and significant declines in groundwater level in major aquifers led to unsustainable use of water resources, a considerable reduction in irrigated area, and unsustainability in agricultural production in the period 2006-2015. Analysis of causes and effects of meteorological, hydrological, and agricultural drought in the area identified three clear stages: before 1997 being sustainable, 1997-2006 being transitional, and after 2006 being unsustainable.
Drought Frontiers in Rice, 2009
International journal of research studies in agricultural sciences, 2022
A In the development of agricultural crops, biotic and abiotic stresses result in considerable yield losses. One of the main obstacles to agricultural production and global food security is abiotic stress. Stress is a word that refers to several biotic and abiotic environmental factors that prevent crop plants from reaching their full genetic potential. Drought is one of the fundamental issues in the current climatic environment and is one of the most severe abiotic stresses in many areas of the world. Plants experience moisture stress when their evapotranspiration requirements are not met. Drought has a negative impact on plant development and other metabolic processes, making it one of the most significant abiotic stresses and factors restricting the successful production of plant products globally. Drought is caused by a lack of water as a result of erratic rainfall or inadequate irrigation, but it can also be hampered by other elements such as soil salinity, physical characteristics, and excessive air or soil temperatures. Insufficient water supply throughout a crop's life cycle, including precipitation and the capability of the soil to store moisture, limits the crop's potential to produce the highest possible genetic grain yield. The most significant stressor that has a significant impact on crop development and productivity is without a doubt drought. For better management, it is crucial to comprehend the physiological, biochemical, and ecological actions connected to these stresses. It is possible to generalize morphological, physiological, and biochemical responses to a broad range of plant responses to this stress. Due to physical damage, physiological disruptions, and biochemical alterations, inadequate water supplies and abnormal temperatures have a severe impact on crop growth and yields. Drought stress reduces the size of the leaves, stem extension, and root proliferation within the soil; it also disturbs plant water relations and reduces water-use efficiency, which in turn reduces the plant's ability to yield; as a result, breeding for drought resistance is a good approach. This approach combines conventional and molecular methods to develop a drought-tolerant variety. Breeding more drought-tolerant cultivars may be more successful when selection is based on a thorough testing strategy. Practical implications for treatments and management result from a greater understanding of how plants react to this stress. High demand for drought-tolerant types would seem to be a difficult issue for plant breeders, but difficulties are aggravated by the difficulty of crop yield on a genetic and physiological basis. Food security is seriously threatened by drought, which is the main reason for agricultural loss worldwide. Plant biotechnology is currently one of the most promising areas for creating crops that can generate large amounts of food in moisture environments.
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