eChapters

Pesticides are used to control plant growth (herbicides), insects (insecticides), worms  (vermicides), bacteria (bacteriocides), fungi (fungicides), and other organisms. Almost without exception, pesticides are used to benefit humans by the control of unwanted species of plants (e.g. weeds in a lawn), disease-causing bacteria (e.g., Pneumococcus, the causative agent of pneumonia), disease-carrying insects (e.g. malarial or yellow fever mosquitoes) or in controlling destruction of agricultural products by disease-causing organisms (e.g., corn-borers, the virus of anthurium blight). Although they are by and large mostly beneficial, pesticides used both properly and improperly are also “resources out of place”, that is pollutants, that are subject to normal ecological processes.

It is a well known fact that natural disasters strikes countries, both developed and developing, causing enormous destruction and creating human sufferings and producing negative impacts on national economies. Due to diverse geo-climatic conditions prevalent in different parts of the globe, different types of natural disasters like floods, droughts, earthquakes, cyclones, landslides, volcanoes, etc. strikes according to the vulnerability of the area. India is considered as the world’s most disaster prone country. It has witnessed devastating natural disasters in recent past like droughts, floods, cyclones, earthquakes, landslides, etc. 

The phenomenon we call tsunami is a series of large waves of extremely long wavelength and period usually generated by a violent, impulsive undersea disturbance or activity near the coast or in the ocean. A tsunami is a very long-wavelength wave of water that is generated by sudden displacement of the seafloor or disruption of any body of standing water.  Tsunami are sometimes called “seismic sea waves”, although, as we will see, they can be generated by mechanisms other than earthquakes.  Tsunami have also been called “tidal waves”, but this term should not be used because they are not in any way related to the tides of the Earth.  Because tsunami occur suddenly, often without warning, they are extremely dangerous to coastal communities.

Continental drift is the theory that continents move slowly about the earth’s surface, changing their positions relative to one another and to the poles of the earth. It includes the idea that former continents may have broken apart and that the fragments have recombined in different patterns (Fig. 15.1). Some authorities have considered that this happened only once, beginning within the past 200 million years; others believe that it has long been a continuous process, so that all existing continents are mosaics. Those who accept the theory believe that the rates of motion have been only a few inches a year. Earlier, it was considered that the continents moved like ships through a slightly plastic ocean floor. Today some consider that the continents are frozen into the earth’s surface like rafts in ice, and that the motions are the result of growth of the sea floor along certain midocean ridges and reabsorption of the sea floor elsewhere beneath deep ocean trenches and young mountains. The continents are carried passively about embedded in moving plates of the surface. Some authorities  now  agree  that  there  is  a  deformable  layer,  called  the asthenosphere, at depths of from about 50 to 400 kilometers within the earth. It is white hot, and slightly viscous, and many believe that the surface can break into plates which slide over it.

HUMAN POPULATION GROWTH

The evolution of man took place about one million years ago in response to changes in the physical environment. We learnt gradually to adapt different modes of life to varying environments and migrated different parts of the world. Human activities have had their impact on the environment, which was depending on the number of people living in  the area and  their level  of economic development. Per capita consumption of food, energy and other resources in developed countries is larger and its impact on the environment is much greater than equal number of persons living in developing countries in Africa or Asia. Therefore, the distribution of population needs to be examined in detail.

Energy, food production and various other natural resources are the limiting factors on this earth. The result of this bitter truth has been published in a book titled ‘The Limits to Growth’ in 1972. If the enormously growing population and the industrial process is not checked, then the earth’s civilization may come to an end within next hundred years.

By considering the space travel, we can very well understand about the Ecosystem. When we go away from the biosphere, it will be appropriate to develop unlimited environment through the energy accumulated from the sunlight in space. For the space travel for some days to moon and back to earth, we need not establish the entire ecological system as greater quantity of O₂ and food stuffs can be stored and CO₂ and other unwanted materials can be fixed for establishing space colonies, we have to build a special space ship with important abiotic components which can be recycled for use again and again. The vital processes of production, consumption and decomposition can be established and balanced through biotic components. In other words we are creating a complete mini human ecological machine. Before we established this system, we should be quite familiar about the space problems and its implications.

3.1.Processes
                    
    Leaching                    
    Fragmentation/Comminution
    Catabolism                    
    Decomposition models
                
3.2. Patterns
                    
    Litter decomposition
    Root decomposition                    
    Limit values for decomposition            
    Decomposition pattern in ecosystems

1.1    General Circulation of the Atmosphere
    
1.2    World Climates
    
1.3    World Climate Classification by Köppen’s method
    
1.4    Climatic Classification over India
    
1.5    Asian Summer Monsoon and Rainfall Distribution
    
1.6    The Indian Monsoon
    Features of monsoon
    Monsoon circulation
    Onset of monsoon
    Withdrawal of monsoon
    Southwest monsoon rainfall
    Active phase of monsoon
    Break monsoon conditions
    Winter monsoon

1.7    Causes for Failure of Monsoon
    
    Prediction of onset of monsoon rainfall

1.8    Spatial Distribution of Weather Parameters over India
    Rainfall
    Temperature
    Humidity
    Sunshine and Radiation
    Wind speed

1.9    Famines in India
    
1.10    Historical Evidences of Droughts
    
1.11    Distribution of Drought Prone Regions over the Globe
    1.11.1    Occurance of drought in different countries
    
1.12    Distribution of Drought Prone Regions in India
    
1.13    Weather Phenomena Associated with Droughts
    
1.14    Effect of Droughts on Natural Resources
    1.14.1    Surface water resources
    1.14.2    Groundwater sources
    
1.15    Impact of Latest Droughts on Crop Production in India
    
1.16    Economic Impacts of Droughts in India
    
1.17    Economic Impacts of Droughts in other Nations
        
References

2.1    Definition of Droughts
    
2.2    Types of Droughts
    2.2.1    Meteorological Droughts
    2.2.2    Agricultural Droughts
    2.2.3    Hydrological Droughts
    2.2.4    Socio-economic Droughts
    
2.3    Criteria for Classification of Droughts
    Meteorological Droughts
    Agricultural Droughts
    Hydrological Droughts
    
2.4    Data requirements in Drought Analysis
    
2.5    Drought Indices
    2.5.1    Rainfall-based Indices
    2.5.2    Climate Derivate Based Indices
    2.5.3    Remote Sensing Based Indices
    2.5.4    Processes Based Indicators
    
2.6    Assessment of Drought Prone Regions in India
    
2.7    Indicators for Declaration of  Droughts in India
    2.7.1     Rainfall Deficiency
    2.7.2    Area Under Sowing
    2.7.3    Normalized Difference Vegetation Index
    
2.8    Drought Management Procedures in India
    
2.9    Drought Code adopted by Local Governments
    
2.10    Spatial Variability of Droughts and their Frequency of Occurrence in India
    
2.11    Drought Vulnerability Assessment
    
2.12    Vulnerability of Society to Drought
        
References

3.1    Factors Contributing to Climate Change
    3.1.1    Natural Causes to Climate Change
    3.1.2    Human Causes to Climate Change
    
3.2    Climatic Trends
    3.2.1    Global level
    3.2.2    National level
    
3.3    Climate Projections
    3.3.1    Global level Projections on Future Changes in Climate
    3.3.2    Climate Projections at the National level
    3.3.3    Climate Projections at the Regional level
    3.3.4    Projections of Extremes in Rainfall and Temperature
    
3.4    Consequences of Climate Change on Droughts and Agriculture
    3.4.1    Impact of Climate Change on Agriculture in some States of India
    
References

4.1    Approaches for Drought Monitoring
    
4.2    Weather Network System in Different Countries
    
4.3    Drought Monitoring using Climatological, Hydrological and Combination Approaches in Different Countries
    
4.4    International Cooperation in Drought Monitoring
    
4.5    Drought Monitoring Mechanism in India
    
4.6    Early Warning and Decision Support System
    4.6.1    Software for Drought Detection, Monitoring and Early Warning
    4.6.2    Decision Support System for Droughts Developed Outside India
    
4.7    GIS and Drought Monitoring
        
References

5.1    Global Food Production
    5.1.1    Area Under Cultivation
    5.1.2    World Food Production
    
5.2    Variability in Global and Indian Food Grain Production
    
5.3    Impact of Phenomenal Drought During 2009 on Food Grain Production in Different Countries
    
5.4    Impacts on Livestock and Fisheries
    5.4.1    Livestock
    5.4.2       Milk Production
    5.4.3    Fisheries
    
5.5    Estimation of Food Grain Production in India using Rainfall indices
    5.5.1    Trend in the annual food grain production
    5.5.2    De-trended production index
    5.5.3    Construction of rainfall indices (RI)
    5.5.4    Development of model for estimation of production index
    5.5.5    Verification of model performance
    5.5.6    Estimation of Kharif Price Production
    
5.6    Forecasting of Agricultural Output Using Space, Agrometeorology and Land based Observation (FASAL)
        
References

6.1    Hydrological Cycle
    
6.2    Global Surface Waters
    
6.3    Surface Water over India
    
6.4    Ground Water Potentials in India
    
6.5    Influence of Drought on Water Resources, its Fauna and Flora
    6.5.1    Effects on Fauna and Flora
    
6.6    Influence of Changing Climate on Droughts and Water Resources
    6.6.1    Global warming and droughts at global scale
    6.6.2    Global warming on water resources at global scale
    6.6.3    Global warming and droughts at national scale in India
    6.6.4    Global warming impacts on water resources at National scale
        
References

Good Practices for Drought Management
    7.1    Drought Planning and Preparedness
    7.1.1    Drought Planning in India
    7.2    Global Experiences in Drought Planning
    7.2.1    USA
    7.2.2    South Africa
    7.2.3    African Nations
    7.2.4    Namibia
    7.2.5    Ethiopia
    7.2.6    Botswana
Drought management plans in Europe
    7.2.7    Spain
    7.2.8    England and Wales
    7.2.9    Portugal
    7.2.10    Australia
    7.2.11    China
    7.2.12    Palestine
    7.2.13    Global Initiatives
    7.3    Drought Preparedness Action Plans in India
    7.3.1    Drought Preparedness Checklist
    7.4    Drought Preparedness Action Plans in Different Countries
    7.4.1    Arizona State in USA
    7.4.2    Texas State in USA
    7.4.3    Italy
    7.4.4    Mediterranean Region
    7.4.5    Pakistan
    7.4.6    Darfur in Sudan
    7.4.7    Bangladesh
    7.5    Indigenous Knowledge for Drought Management
    7.5.1    Astro Meteorological Methods
    7.5.2    Traditional Knowledge in Weather Prediction
     7.5.3    Traditional wisdom in Drought Risk Region (DRR)
        Rajasthan and Bundelkhand region in Uttar Pradesh
    7.5.4    Indigenous technologies for moisture conservation 
        in dry lands of semi-arid regions of India
    7.6    Traditional Wisdom for Drought Management in a few selected countries
    7.7    Role of Weather-based Agro-advisories
    7.7.1    Strategies for dissemination of advisories
    7.7.2    Role of ICAR and AICRPAM on Agromet Services
    7.7.3    Agromet Advisory services through mobile phone
    7.7.4    Status of Agromet Advisory Services in other Countries
    7.8    Value Addition to Agromet Information
    7.8.1    AICRP on Agrometeorology
    7.8.2    Thumb rules for weather-pest/diseases
    7.9    Contingency Crop Planning for Minimizing Risks
    7.9.1    Contingency Crop Planning for Rainfed Regions of India
    7.10    Drought Proofing Mechanisms
    7.10.1    Watershed Development for Drought Management
    7.10.2    Watershed Development in India
    7.10.3    The Success Stories of Watershed as a Drought Proofing Mechanism
    7.10.4    Watershed Policies and Recommendations
    7.10.5    Farm Ponds for Drought Management
    7.10.6    Success Stories of Farm Ponds
    7.11    Rainfed Technologies for the Drought Management in different agro climatic region
    7.12    Farmer’s Awareness on Climate Management
    7.12.1    India
    7.12.2    In other Countries
    7.13    Role of ICT in Climate Risk Management through AAS
    7.13.1    India
    7.13.2    Application of ICT in Providing Advisories in other Countries
    7.14    Integrated Drought Management Strategies through Farming Systems Approach
    7.14.1    Drought Adaptation Strategies in Rajasthan and in Maharashtra
    7.14.2    Improvement and Rural Livelihood
    7.15    Drought Mitigation Measures
    7.15.1    Drought Mitigation Plans
    7.15.2    Soil water Conservation and Recharging of Ground water Methods
    7.15.3    Traditional Water Harvesting and Conservation 
        Techniques
        References

Review of the state of art of Drought on impact assessment, monitoring and management with special reference to agricultural production has revealed that Drought is still a complex natural disaster and difficult to forewarn in spite of advancements in atmospheric sciences and computational procedures. It is realized only after it is set in and is not known when it is likely to withdraw. A long way one has to travel to predict its occurrence, spread and its continuation to the next season over a region. The existing net work of observational set up in developing countries in Africa, Asia and in South America need to be strengthened further for effective monitoring of significant weather events at regional and micro regional level. With the rapid expansion of communication system over the past two decades, establishment of Automatic Weather Stations (AWS) at as many locations as possible even in remote regions should be taken up on priority basis and funding may be provided by the respective governments or by the International Organizations where ever necessary. Nations with limited resources may also be convinced to strengthen their weather observational net work in view of the increased occurrences of climate extremes and changing climate. Drought vulnerability regions over the globe were delineated based on sparse historical weather data which do not match with real surface conditions. Now, with the availability of weather data from more number of stations both temporally and spatially, drought prone regions over the world may be re-delineated. This would help the planners to allocate funds rationally to the affected regions. Globally every year, some regions or others may be experiencing droughts and more so in drought prone regions.

The aim of this book is to further strengthen the knowledge of readers on management of disasters so that they are better prepared to cope with more frequently occurring natural and manmade disasters.

The process that helps us to face disasters effectively is commonly known as disaster preparedness.  When a disaster strikes, it affects us directly and immediately. While as the government, international agencies such as United Nations, Red Cross Society, non government organizations, like Ramakrishna Mission, OXFAM, CARE, resident welfare associations in urban areas and panchayats in rural areas assist us when faced with disasters the community, invariably remains the first responders. Hence, the individuals as a part of community should prepare adequately to prevent, face and respond to disasters effectively. History has  shown that where communities have prepared adequately to confront disasters, losses to life and property have been less and environment could be protected. People living in an area may be prone to more than one type of disaster. For example Kutch District of Gujarat is vulnerable to floods, drought, cyclones and to earthquakes. Such an area is called ‘multiple hazard’ zone.

The United Nations had declared the decade of 90s (1990-1999) as the International Decade for National Disaster Risk Reduction to enable developing countries to build up their capacity to cope up with disasters. The Government of India also set up a High Powered Committee (HPC), in August 1999, to review the preparedness and mitigation of natural and manmade disasters and recommend measures for strengthening the organisational structures and a comprehensive model plan for management of disasters at national, state and district level. The HPC after due deliberatons submitted the report in Feb. 2001. The HPC identified the disasters under the following types (categories) :

Introduction

Drought is temporary reduction in water or moisture availability significantly below the normal or expected amount for a specific period. This condition occurs either due to inadequacy of rainfall or lack of irrigation facilities, unexploitation or deficient availability for meeting the normal crop requirement in the context of the agro-climatic conditions prevailing in any particular area. This has been scientifically computed as Moisture Index (MI). Drought in this context can be defined as adverse MI or adverse water balance which may be attributable not only to a prolonged dry spell due to lack or sufficient rainfall but also due to such other factors as excessive evapo-transpiration losses, high temperature, low soil holding etc.

1. GEOLOGY

Geology : Earth Science

 Geo = Earth + Logos = Science

 Def : The science which investigates the history of the earth is known as geology.

 Following are the important branches of geology.

1.Coal Geology : it is related with natural gas, coal deposits and their formation.

2.Crystallography : includes the crystal and atomic structure of the mineral. 3. Drilling Technology : it is related with the cores, core logging and coorelation of the lithology.

4.Engineering Geology and Surveying : it is related with engineering aspects of the earth.

9. WEATHERING

The general process of production of rock waste partly by mechanical breaking and partly by chemical decomposition is known as weathering. The resulting products of weathering accumulate in the same place from which they are derived and there is no transport involved in the process.

Agents and types of weathering : The agencies which are involved in the process of weathering are atmosphere, water and organisms. The whole process of weathering may be conveniently divided into two types : mechanical or physical weathering and chemical weathering. Mechanical weathering involves those processes which bring about disintegration of rocks and minerals without any chemical activity. Chemical weathering involves various chemical processes which slowly decompose the rocks and minerals. In nature two processes are intimately associated and only under extreme conditions, they do occur as a separate entities. Mechanical weathering breaks down the rock creating more surface area and facilitates chemical weathering. Chemical weathering weakens the rock and makes it more susceptible to mechanical break down. Thus the two processes are always complementary to each other.