eChapters

The coastal salt affected soils are low in productivity due to various soil fertility constraints that affect the crop growth and yield. The high salt content &/or high pH cause changes in solubility, availability and efficiency of plant nutrients, besides deteriorating the physical condition of soil. The soil biology (microbial population and enzymatic activities) also severely affected in these salt affected soils. The bio-resources are known to improve soil physical, chemical & biological properties of the soil. The maximization of rice production and considerable improvement in quality and composition of rice in coastal salt affected soil with the use of bio-resources have been reported by several research workers.

Introduction

The Intergovernmental Panel on Climate Change Fifth Assessment Report (IPCC, 2013) emphasized that warming of the climatic system is unequivocal and that anthropogenic warming will continue for centuries to come due to timescales associated with climate processes and feedbacks. While stresses caused by climate change are likely to negatively impact the agricultural and livestock sector and escalate existing small-scale farming challenges; agricultural and livestock productivity and sustainability have to improve to meet the needs of the growing human population (DEA, 2013; Zamykal and Everingham, 2009). Climate change is seen as a major threat to the survival of many species, ecosystems and the sustainability of poultry production systems in many parts of the world. Nevertheless, global demand for poultry products is expected to increase, as a result of the growing human population, and its growing af?uence. The extreme climatic conditions impose various stresses on poultry birds which adversely affect their growth, production and reproduction.

While climate change is a global phenomenon, its negative impacts are more severely felt by poor people in developing countries who rely mostly on the natural resource base for their livelihoods. Moreover, rural poor communities rely greatly for their survival on agriculture and poultry which belong to the most climate-sensitive economic sectors. Climate change is expected to intensify existing problems and create new combinations of risks and shift hazard zones. The incidences of draughts, snow-storms and blizzard like events have risen. The situation is made worst due to factors such as widespread poverty, inequitable land distribution, limited access to capital and technology inadequate infrastructure, long term weather forecasts and inadequate research and extension. Intensive poultry production has much less impact on global warming than organic or free-range production (Van der Sluis, 2007). Seo and Mendelsohn (2006) reported that small farms of poultry are better able to adapt to warming. However, organic egg production needs more energy than non-organic and increases most environmental burdens. The most disadvantageous, from environmental point of view, is litter-free breeding of birds which causes great amounts of liquid manure.

The world’s fisheries, encompassing both marine and freshwater environments, play a critical role in global food security, livelihoods, and economies. However, these vital resources are increasingly threatened by the far-reaching consequences of climate change. This chapter delves into the multifaceted impacts of climate change on the fisheries sector, exploring the complex interplay between rising temperatures, altered weather patterns, and ocean acidification, and how these changes affect fish populations, habitats, and the communities that depend on them.
We will examine the ways in which climate change is altering the fundamental
dynamics of aquatic ecosystems, leading to shifts in species distribution, disruptions in food webs, and increased vulnerability to extreme weather events. Special attention will be given to the differential impacts on various regions and fisheries, considering the unique challenges faced by small-scale fisheries and developing nations. Furthermore, the chapter will discuss the potential consequences for global fish production, economic stability, and food security, highlighting the urgent need for sustainable management practices and adaptive strategies to mitigate these adverse effects and ensure the longterm viability of the fisheries sector.
13.1 Climate Change Impacts on Marine Fisheries
Climate change is significantly altering marine ecosystems, leading to profound impacts on fisheries. These changes affect various aspects of fish biology and ecology, including fishery dynamics, migration patterns, and breeding seasons (Fig.13.1). Here’s a detailed breakdown:

INTRODUCTION

Any crop has its own optimal requirements or selective response to the environmental factors such as rainfall/ soil moisture supply, day/night air temperature, soil temperature, duration of sunshine and its intensity. The growth and development of a plant which ultimately governs the agricultural productivity of a region, is closely related with climatic factors. Weather phenomenon has a profound influence on crop growth stage. A moderate wind or a light rain, when the crop growth is near to harvest, may do more damage than even heavy rain and high wind in the vegetative phase. So land use planning by matching crop growth with weather parameters forms a basis for successful agriculture (Samra, 2003) in a particular region. In order to achieve sustainable agricultural productivity in the 21^st century, the climate and weather systems are being recognized as critical agenda and input.

Crop yields and agricultural sustainability are inextricably linked to weather patterns. While optimal weather conditions facilitate robust growth and abundant harvests, extreme weather events pose significant threats, disrupting food systems and impacting livelihoods globally. The chapter, “Effect of Extreme Weather Conditions on Crops,” delves into the multifaceted ways in which deviations from ideal climatic norms compromise agricultural productivity. The Earth’s climate is characterized by increasing variability and the rising frequency and intensity of extreme weather phenomena. These include, but are not limited to, prolonged droughts, severe floods, heat waves, cold snaps, hailstorms, and unseasonal strong winds .Such events can occur suddenly or develop gradually over extended periods, each presenting unique challenges to different crop types at various stages of their life cycle. For instance, a sudden hailstorm can physically destroy crops, while a long-term drought can stunt growth, reduce yield quality, or lead to

Toxic elements like Cadmium (Cd), Fluoride (F), heavy metals, radioactive metals are associated with mainly rock phosphates, other organic wastes like sewage sludge and pollutants. Their chemistry is similar to plant nutrients and replace them in their physiology leading to reduced uptake of nutrients, productivity and contaminated food chain.

Abstract

The experiment, conducted at research farm of Central Arid Zone Research Station, Bikaner during 2009 on sandy loam soil. The study revealed that in agri-horti system different irrigation levels significantly affected the growth parameters (plant height, stem girth and tree canopy) of fruit trees which was highest at 80% ETc irrigation level in intercropping of moth bean and cluster bean and it was significantly higher over no intercropping. Intercropping of sonamukhi gave 24.8% lower plant height of citrus over no intercropping. Highest fruit yield of citrus was recorded (40% fruiting) with intercropping of moth bean at 80% ETc irrigation level which was 51% higher over intercropping of sonamukhi.

Abstract

A field experiment was conducted at Mechanized Commercial Farm, College of Agriculture, Junagadh Agricultural University, Junagadh (Gujarat) during the Kharif-Rabi seasons of 2006, 2007 and 2008 to study the effect of tillage practices on yield of rainfed castor (Ricinus communis). The experiment was laid out in Randomized Block Design with four replications. The six treatments comprised viz., T_1- Conventional tillage (Cultivator + blade harrowing), T_2-Ploughing followed by cultivator and blade harrowing, T_3-Tillage through rotavator, T_4-Furrow opening through sub-soiling, T_5-Furrow opening through V-notch cultivator and T_6-Zero tillage (pre and post emergence herbicides + 2 hand weeding). Among the different treatments, the different growth and yield attributing parameters viz., plant height, number of spikes per plant, length of main spike, number of capsules per spike and test weight, seed and stalk yields, higher gross and net returns were recorded when field was prepared by ploughing followed by cultivator and blade harrowing. It also improved soil moisture content which was closely followed by tillage through rotavator (T₃) and furrow opening through sub-soiling (T₄).

The intricate dance between life and its atmospheric surroundings has shaped every living organism on Earth. From the microscopic bacteria thriving in extreme environments to the complex physiological systems of humans and large animals, weather and climate are not merely backdrops but active, pervasive forces dictating survival, distribution, behavior, and health. Weather, representing the short-term atmospheric conditions we experience daily— temperature, humidity, precipitation, wind, and sunlight—directly influences immediate comfort, activity levels, and susceptibility to acute events. Climate, on the other hand, embodies the long-term patterns and averages of these atmospheric variables over decades or centuries, acting as a fundamental determinant of ecosystems, biodiversity, and the sustained well-being of populations. This chapter delves into the multifaceted ways in which these atmospheric phenomena exert their influence. We will explore how thermal conditions drive physiological responses, from metabolic rate adjustments and thermoregulation to the very limits of endurance in extreme heat and cold. Beyond direct physiological impacts, we will examine the indirect effects, such as the role of climate in shaping

Introduction

The town Paithan is famous by it’s name Dakshin Kashi. Godavari river has pristine glory and great significance for Hindus.

Nath temple is situated on the bank of Godavari river. It is a holy place and that’s why it becomes a place of public gathering on Ekadashi, Aashadi Ekadashi, Poornima, Deepawali, Dasera etc. Every year during Chaitra lakhs of people gather.

But at the time of Sheshti, which occurs once in a year is a special event. Hence many fold increase of congregation compared to other melas. The particular small stretch of river near temple was highly polluted, due to mass bathing and other polluting activities. The warm weather shall alter the photosynthesis rates, biodegradation and affect BOD, DO, pH etc. Recent Nath Sheshti at Paithan during 20^th March to 22^nd March 2006, drew about one lakh of pilgrims and had a few special aspects of interests from an environmental point of view.

Considering all the above aspects, it was decided to assess the changes in quality of river Godavari during Nath Sheshti.

The Effective Climate Guidance (ECG) refers to information, tools, and frameworks designed to help individuals, organizations, and governments make informed and effective decisions and take appropriate actions to address climate change (Fig.7.1). It aims to provide practical, relevant, and actionable insights to navigate the risks and opportunities presented by a changing climate. Fig.7.1: Effective Climate Guidance (ECG)
7.1. Key Aspects of Effective Climate Guidance Include
• Materiality: Focusing on the most significant climate-related issues for the specific context (e.g., for a business, these would be the climate risks and opportunities that could impact its financial performance).
• Actionability: Providing clear steps or strategies that can be implemented.
• Decision-Usefulness: Ensuring the information is relevant and presented in a way that supports informed decision-making.
• Authority and Reliability: Based on credible scientific information and data.

14.1. Slope
It is a crucial topographic factor that affects water drainage, erosion and accessibility of agricultural machinery. Steep slopes increase the risk of soil erosion, and water run-off requiring erosion control measures such as contour ploughing or terracing. Slope also affects the availability of sunlight, as steeper slopes may cast shadows and influence microclimates within a field.
14.2. Altitude / Elevation
Elevation is the vertical distance of a point or location above a reference point, often mean sea level. It influences temperature, atmospheric pressure, and the types of crops that can be grown in an area. Higher altitudes generally experience cooler temperatures, which may limit the choice of crops that can thrive. Elevation affects the length of the growing season and influences the choice of appropriate crop varieties. In summary, elevation is an absolute measure of the vertical distance above a reference point (such as MSL), while it is a relative measure that describes the variation in elevation within a specific area or region. Elevation provides information about the height of a point, whereas it provides insights into the topographic features and slopes of a given agricultural landscape. Both elevation and relief are important considerations in agriculture as they influence factors such as water drainage, temperature gradients, and suitability for specific crops.
14.3. Aspect
Aspect refers to orientation of the slope (north, south, east or west). It affects the distribution of sun light; wind patterns and temperature gradients in a field. In the northern hemisphere, the north side of slope is often shaded while the southern side receives more solar radiation and heat, creating warmer microclimates and potentially influencing the choice of crops or planting strategies. Aspect can also impact the risk of frost or cold air drainage in certain regions. Whereas, in the southern hemisphere, the south side slopes get shaded and north facing slopes receive more solar radiation.
14.4. Relief
Relief refers to the variation in altitude between different points. It is a relative measure on changes in altitude across a particular landscape or agricultural area. The valley slopes are preferred sites for agriculture in mountain regions due to several reasons:
• The valley slopes offer relatively flatter terrain, making it easier for farming activities such as cultivation, irrigation and mechanization.
• The valleys tend to have better access to water resources such as rivers or streams which can be used for irrigation water.
• The valley slopes provide good sun exposure and protection from strong winds creating favourable microclimates for crop growth
• The natural drainage patterns of valleys help preventing water logging and ensure better water management.

Abstract

The present experiment was conducted to study the influence of weather parameters on the population dynamics of insect pests of rice during 2009-10 at ICAR-RC for NEH Region, Mizoram Centre, Kolasib, Mizoram. The result of the study indicated that, the mean populations of peak abundance of major insect pests rice crops during August were stem borer, flea beetle and gundhi bug. The Correlation studies showed that stem borer population a significant positively correlation was observed with maximum and minimum relative humidity. Nevertheless non significant negative correlation was obtained with maximum and minimum temperature. The finding of the present study indicated a positive non significant correlation with maximum relative humidity, maximum and minimum temperature where as negative insignificant correlation with rainfall and minimum relative humidity with flea beetle population. The highest minimum temperature showed a positive significant correlation with the Monolepta.

The ozone layer is a region in the Earth’s stratosphere where a certain amount of incoming solar radiation is absorbed. Over the last twenty years or so a series of man-made threats to it have been reported and each has been treated  with more gravity than the last. Now a-days such threats feature  regularly on the agendas of international conferences.

Ozone, Positive and Negative : Ozone, or trimolecular oxygen (O3) can be advantageous or exert harmful influence on human health, as well as that of other organisms. It is all depends on whether it is present in the troposphere or stratosphere (Fig. 8.1). In the stratosphere, ozone is a beneficial serving as a shield in screening out most of the damaging portions of ultraviolet radiation which have wavelengths between 290 and 320 nanometers. In the troposphere, ozone is a negative as it appears as a component of smog with a number of deleterious effects, as will be discussed below.

Abstract

As such in search of alternative to chemical insecticides against insect pest of rice resulted in identifying white muscardine fungus, Beauveria bassiana an entomopathogen out of several entomogenous fungi prevalent in rice ecosystem as the potential mycoinsecticides. The fungus has 78-87% virulence against rice hispa with  LC 50 value of 90.16. Under field situations it is required that the effectiveness of the bioagents are enhanced by combining them with compatible pesticides. A sublethal dose of a pesticide  would make the insect physiologically weak which makes it much more susceptible to the attack of the entomogenous organisms. In view of this, compatibility test was conducted with 14 different commonly applied insecticides at two different doses i.e., recommended and half of the recommended dose. In small scale field trial chloropyriphos at half of the recommended dose along with B. bassiana was the best treatment in controlling the pest along with increased yield of the crop consecutively for two years.

Abstract

The groundwater targeting in hard rock aquifer systems is complex, because of the heterogeneity of the aquifer systems. The ground water mobility and stability in such aquifer systems varies because of the lithology, folded structures, fracture density, geomorphology, slope etc., These occur in various permutations and combinations and control the overall water holding and conducting capacity in different parts of the aquifer systems. Hence, one needs to analyse all the data so as to understand and bring out precise spatial models on the groundwater probability in hard rock aquifer systems. In the present study, the authors have carried out GIS based appraisals to understand the relation between the lithology and groundwater movement in hard rock aquifer systems of parts of Central Tamil Nadu covering 1300 sq.km. In the said study, GIS images were generated on the maxima zones of various aquifer parameters such as water level, width of aquifer depletion, transmissivity, permeability, specific capacity, storage co-efficient, optimum yield and recovery rate. These were overlaid with the lithology GIS image. Such an analysis has shown that, in general, the fissile hornblende biotite gneiss appears to have some control over the groundwater systems.

Moisture deficit causing shortfalls in crop production is the characteristic feature of dryland agriculture. Other adverse factors viz., decline in soil fertility together with play of biotic stresses add to the complexities of dryland crop production. Added to the proven agronomic management to combat the problem of drought in dryland agriculture, there is the need to tailoring of suitable crop varieties which can yield reasonably well under conditions of moisture deficit (Varshney et al., 2021). In this context, the appropriate developmental rhythm along with the combination of the constellation of characters of the crop plant matching with the rainfall and the soil moisture availability patterns of the zone are the important considerations together with stability of yield (Hanson and Nelsen, 1980). This task being a complex one, the problem should be approached through multidisciplinary strategy that should buffer the genetic and breeding efforts.

El Nino is the name given to the occasional development of warm ocean surface waters along the coast of Ecuador and Peru. When this warming occurs the usual upwelling of cold, nutrient rich deep ocean water is significantly reduced. El Nino normally occurs around Christmas and lasts usually for a few weeks to a few months. Sometimes an extremely warm event can develop that lasts for much longer time periods. In the 1990s, strong El Ninos developed in 1991 and lasted until 1995, and from fall 1997 to spring 1998.

El Nino means ‘The Little One’ or ‘Christ Child’ in Spanish. It was originally recognized by fisherman of the coast of South America as the appearance of usually warm water in the Pacific Ocean, occurring near the beginning of the year i.e. around Christmas. That is why the name is used. El Nino, the periodic warming of Pacific Ocean waters that affects the weather worldwide. C. Fred and T. Andrus of the University of Georgia studied the ancient fish bones from refuse left about 6000 years ago by ancient peoples in Peru and found that ocean catfish lived in water that averaged 60 to 70 warmer than now and that there was little variation in temperature. He concluded that if El Nino was occurring at the modern rate, once every two to seven years, then the bones from the fish would have reflected the temperature variation.

11.1. Determination of Electrical Conductivity of Soil Solution

The conductivity or more precisely the specific conductance of a soil at a given soil-water ratio is the reciprocal of the specific resistance offered by the solution at 25ºC between the electrodes of 1 sq cm cross section kept 1 cm apart. Thus, the electrical conductivity of any solution depends on the amount of soluble salt present in it. Knowledge on the extent of salinity is important for management of saline soil including the choice of the crop suitable for that soil. Soluble salt content in saturation extract is more reliable index of salinity level than in soil: water ratio of 1: 2 or 1: 2.5 because it simulates the extent of salinity experienced by crop in field moisture condition.

Salinity class of soil is based on the electrical conductivity (EC) of saturation extract at 25ºC. However, EC of water extract from 1:2 soil-water suspension can be transformed into the EC of saturation extract following the formula (except for soil containing gypsum).