eChapters

Abstract

Climate change is a matter of great concern considering aquatic resources and the productivity. The likely impact of Climate Change is noted in the domain both in marine as well as estuarine capture fisheries, fresh water capture fisheries and freshwater aquaculture. Climate change is having a linkage with spread of fish diseases as increasing water temperature will shift the balance in favor of either the host or pathogen changing the frequency and distribution of diseases. There are a no of adaptation and mitigation measures in aquaculture in order to increase the productivity and properly maintain the survivability of many aquaculture species.

Parasitoids are important natural enemies that regulate insect-pest populations and reduce dependence on chemical pesticides. They lay eggs in or on host insects, and their developing offspring eventually kill the hosts. Rising temperatures, altered rainfall, elevated carbon dioxide and extreme weather can affect parasitoid survival, development, reproduction, host-searching ability, distribution and seasonal activity. Climate change may also disturb synchronization between parasitoids and their hosts, thereby reducing the effectiveness of natural biological control. This chapter examines how changing climatic conditions influence parasitoid diversity, abundance and pest-suppression services. It also highlights management approaches for conserving and strengthening parasitoid populations in agricultural ecosystems.

The specter of climate change looms large over our planet, its influence permeating every aspect of the Earth’s systems. Among the most concerning manifestations of this global shift is the increasing frequency and severity of extreme weather events, and atmospheric droughts are emerging as a particularly insidious threat. The present chapter shines a spotlight on this critical intersection, meticulously dissecting how the profound alterations in our climate are fundamentally reshaping the dynamics of atmospheric moisture Going beyond traditional notions of drought rooted in soil dryness, this chapter will illuminate the concept of atmospheric drought – a state where the air itself becomes exceptionally parched, characterized by low relative humidity and a voracious atmospheric demand for moisture. We will unravel the intricate ways in which climate change acts as a catalyst for these conditions. Rising global temperatures amplify evaporation rates, while shifts in large-scale atmospheric circulation patterns can steer moisture-laden air away from v

Black pepper (Piper nigrum L.), famous as “Black Gold” and also known the “King of Spices” is the most important agricultural commodities of commerce and trade in India. It is the most important, most popular and most widely used spice in the World. Of the total spices traded internationally, black pepper accounts for 34 per cent. South West India is the traditional home of this important spice, particularly the Malabar Coast. Black pepper is also grown in tropical zones such as the Asia Pacific Region, mainly India, Indonesia, Malaysia, Sri Lanka, Thailand, China, Vietnam and Cambodia. Outside the Asia Pacific region, the crop is distributed in Brazil, Mexico, Guatemala, etc., totaling about 26 countries. It is grown successfully between 20°N and 20°S latitude and from mean sea level to 1500 meters above sea level. World’s black pepper production varies in the range of 2.7 to 3.35 tonnes annually.

Small cardamom (Elettaria cardamomum Maton), popularly known as the “Queen of spices”, occupies an important position among the foreign exchange earning commodities. Cardamom is cultivated on a commercial scale in Sri Lanka, Guatemala, Tanzania and Papua New Guinea. Guatemala is the largest producer of cardamom in the World. In India, it is confined to the States of Kerala, Karnataka and Tamil Nadu, accounting for an area of 41588 ha, 25021 ha and 4561 ha, respectively (Spices Board, 2009). Among these States, Kerala accounts for the major portion of production (58.4 %), followed by Karnataka (35.2 %) and Tamil Nadu (6.4 %). In Kerala, Cardamom is mainly grown in the erstwhile Travancore area in the present Idukki district and it is known as the Cardamom Hill Reserve (CHR), which was specially reserved, denotified and removed from the control of forest development by the orders of the Travancore Government. By a Royal Proclamation in Medam 997(ME) 334 square miles (86,506 ha) area in Devikulam, Udumbanchola and Peermedu taluks of the present Idukki District was declared as CHR for the promotion of cardamom cultivation (Miniraj and Nybe, 2007). Cardamom is a native of the moist evergreen rain forests of the Western Ghats of South India and is grown extensively in the hilly regions at elevations of 700 to 1300 metres as an under crop in forest lands. Cardamom thrives well within certain thermal regimes. It is believed that diurnal symmetries in temperature trends, if any, have close links with the changes in cloudiness, humidity, atmospheric circulation pattern, winds and soil moisture (Kumar et al., 2002).

Cashew (Anacardium occidentale L.) is a very important horticultural crop which fetches considerable foreign exchange to India. The crop is a native of Brazil and was introduced in India by the Portuguese during 16^th Century. It is grown in India, Brazil, Vietnam, Tanzania, Mozambique, Indonesia, Sri Lanka and other tropical Asian and African countries. The crop is grown within the latitudinal belt of 27°N and 28°S of the equator experiencing a tropical temperature for its growth and development (Rao and Gopakumar, 1994). The trend in productivity has a phenomenal bearing to the distance from the equator. The world production of cashew is estimated to be around 20.8 lakh tonnes. The global productivity level of cashew is 690 kg/ha. Since 2000, the world raw cashewnut production registered an increase of 40 per cent. India’s share in the world raw cashewnut production accounts to about 25 per cent. In recent times, India is facing tight competition from Vietnam and Indonesia in international cashew trade. Since its introduction in the Country, cashew has well adapted to the Indian climatic conditions and is grown in the East and West Coasts of India. Now, India is the largest producer, processor, consumer and exporter of cashew in the world (Bhat, 2009 a). In India, cashew is grown mainly in Maharashtra, Goa, Karnataka and Kerala along the West Coast and Tamil Nadu, Andhra Pradesh, Orissa and West Bengal along the East Coast.

The Coconut palm, also known as the Cocos Nucifera L., is one of the most fascinating and beautiful palms in the world. Epigraphical, literary and sculptural evidence provide proof that coconut has served humanity for more than three millennia. The palm is looked upon with reverence and affection and is referred to by such eulogistic epithets as “Kalpavriksha”, tree of heaven, the tree of abundance, nature’s super market, king of palms and the tree of life. The coconut is believed to have originated in Southeast Asia (Indonesia, Malaysia, Philippines) or Micronesia (Harries, 1977; Purseglove, 1968 and 1972). Coconut has been cultivated in India since ages and plays an important role in social, economic and cultural activities of the people. The palm is amenable to both plantation and homestead management and it can be either a major crop or a minor one in a homestead garden of mixed crops. While responding favourably to scientific management, the palm also tolerates negligent farming to a certain extent. Thus, it can adapt to the divergent farming situations and management practices that are prevalent in different agro-climatic regions. The coconut palm is usually found near the sea on sandy beaches where it can tolerate salt spray and brackish soils. It is also grown under different soil types such as loamy, laterite, coastal sandy, alluvial, clayey and reclaimed soils of the marshy low lands. The ideal soil conditions for better growth and performance of the palm are proper drainage, good water-holding capacity, and presence of water table within three metres and absence of rock or any hard substratum within two meters of the surface. The coconut palm can also grow well inland, within altitudinal limit of 600 m to 1752 m in the Tropics. It requires an equatorial climate with high humidity. A year-round warm and humid climate favours the growth of coconut. The ideal mean annual temperature, which can be tolerated by coconut palm, is around 27ºC with 5–7ºC diurnal variation. The palm does not withstand prolonged spells of extreme weather/climate variations under rainfed conditions. A well-distributed rainfall of 1300–2300 mm per annum is preferred. It is known as a coastal tree since it is grown along the Coasts and Islands and does not tolerate high temperature range, that is the difference between the maximum and minimum temperatures.

Climate change refers to long-term shifts in temperatures and weather patterns. These shifts may be natural, such as through variations in the solar cycle. But since the 1800s, human activities have been the main driver of climate change, primarily due to burning fossil fuels like coal, oil and gas. (https://www.un.org/ en/climatechange/what-is-climate-change) While it is possible to achieve enhanced food production to meet the demands of growing populations, the prevailing negative environmental trends, if continued, might cause crises in many parts of the world (Molden, 2007). The effects of climate change on agriculture can take place through changes in average temperatures, rainfall, and climate extremes (e.g., heat waves); changes in pests and diseases; changes in atmospheric carbon dioxide and ground-level ozone concentrations; changes in the nutritional quality of some foods; and changes in sea level. (Anonymous, 2014A)

Abstract

Tripura is expected to be highly prone to the consequences to climate change because of its geo-ecological fragility, strategic location, its trans-boundary river basins and its inherent socio-economic instabilities.  Environmental security and sustainability of the state is and will be greatly challenged by the impacts of climate change in coming years.
Climate and weather can substantially influence the development and distribution of insects.

Entomopathogens are microorganisms that infect and kill insects, mites and other arthropods and are widely employed in biological control and integrated pest management. They include bacteria, fungi, viruses and entomopathogenic nematodes. Their effectiveness depends greatly on temperature, humidity, solar radiation, rainfall and interactions among the host, pathogen and environment. Climate change can alter pest populations as well as pathogen survival, infectivity, multiplication and field persistence. These effects may enhance some microbial-control agents while reducing the effectiveness of others. This chapter introduces major groups of entomopathogens and examines their performance under present and projected climatic conditions, emphasizing their importance in environmentally responsible pest management.

Introduction

The Intergovernmental Panel on Climate Change (IPCC) assessment reports (IPCC, 2007) suggests that consequently occurring climate extremes are likely to increase the frequency and intensity in the future. In the Indian context, events such as landfall of rare of rarest most intense pre-monsoon Tropical cyclone Fani (2019), back to back landfall of very intense tropical cyclones such as Phalini (2013) and Hudbud (2014), Cyclone Komen (2015), Extreme rainfall events of Kerala (2018 and 2019), Heavy rainfall events of over Northeastern states of India (2019), Cloud burst events of Uttarakhand (2013), Rainfall over Himachal Pradesh (2019), Mumbai Rain fall (2015) and extreme heat wave conditions of 1998, 2015 and many similar type of extreme events are not usual. However, at present there is no unanimity among scientists to exclusively and directly link such extreme weather events to climate change, however based on number of studies and observation data sets it is agreed that the impact of climate change is evident (beyond the natural variability) in many part of the globe including India. In 2019 monsoon season at least 1351 deaths happened to ?oods, heavy rainfall and landslides compared to 1550 for year 2018. In this manuscript, recent research findings related to extreme weather events in the context India are discussed in the following section-2, need for high resolution and long term data sets are emphasized in section-3, followed by recommendations as part of future preparedness, that will not only enable us to address these issues in a robust scientific manner but also provide us strong resilient society to face these extreme weather events in an optimized and effective manner to minimize the loss of lives, properties and socio-economic conditions of citizens.

INTRODUCTION

The latest Assessment Report (AR-5) of Intergovernmental Panel on Climate Change (IPCC) has concluded that warming of the climate system is unequivocal, and since the 1950s, many of the observed changes are unprecedented over decades to millennia. The report further pointed about the warming of atmosphere and ocean; shrinking of glaciers, sea level rise and more frequent and intense extreme weather events. The most critical information pertains to the increase of the concentrations of greenhouse gases. The report figures that human influence, primarily the burning of fossil fuels, has been the “extremely likely” dominant cause of global warming over the past several decades. Based on the scientific evidences, it is reported “warming by the end of the 21st century will lead to high to very high risk of severe, widespread, and irreversible impacts globally” (Edenhofer et al. 2015).

This chapter introduces the close relationship between climate change and forest ecosystems and examines how changing temperature, rainfall, drought, extreme weather, fires, pests, and diseases affect forest health and productivity. It discusses the importance of forests in carbon sequestration, biodiversity conservation, climate regulation, and ecosystem services. The chapter also examines climate-change mitigation through sustainable forest management, afforestation, reforestation, and initiatives such as REDD+. Particular attention is given to the Indian scenario, conservation policies, government initiatives, and challenges associated with forest degradation and climate change

1. Introduction

The world’s temperature has already warmed up to almost 1.2ºC since the preindustrial levels and this warming impact is visible in the form of extreme weather events, sea level rise and diminishing Arctic sea ice. Heat waves and drought in Europe and China, forest fires in the U.S., dust storms and extreme rainfall in India (including the Kerala floods 2018) and high precipitation in Japan and other island nations are all examples of the disasters which have occurred within a single year of 2018. With a further 0.5ºC warming, these effects would be even more pronounced than the scientists’ previous predictions. A 1.5ºC warmer world will see higher temperatures, increase in frequency and intensity of precipitation, higher sea levels, and floods, droughts and heat waves (Venkatesh, 2018). The climate change induced economic damage has been increasing in the past few decades and is likely to continue growing because of population growth, urban development and changing land use pattern (IPCC, 2012). Kerala encountered the most disastrous floods in its history since 1924, between June 1^st and August 19^th of 2018. As the torrential rainfall and associated storm thrashed the state, the entire state got buried under water with only few areas remaining above water. The combined precipitation received by the state during this period was 42 per cent in excess of the typical normal. The exceptional spell of rainfall inflicted heavy damage on the life and properties of thousands of people in the state.

Since 2012, the United Nations Framework Convention on Climate Change (UNFCCC) has considered gender and climate change as a stand-alone agenda item under the Conference of the Parties. This is because it has been already understood that climate change has a greater impact on those sections of the population which are more reliant on natural resources for their livelihood. People who have the least capacity to respond to natural hazards are also affected

more. Majority of women, who are considered among the poorest of the poor are at a greater disadvantage because their income is mostly derived from informal natural resources dependent livelihoods. Globally, more than 400 million women engage in farm work in more than 90 countries. Agriculture being a climate sensitive sector, climate change takes a huge toll on this area. Women are usually engaged in subsistence agriculture and labor-intensive works which worsens their susceptibility to climatic change (Lambrou and Piana, 2006). Hence, during extreme weather events, women experience greater impacts and vulnerability than men and become economically insecure following disasters.

People worldwide are getting affected by the changing climate and associated natural disasters. These climate changes affect both genders differently. Changing climate is not often thought of as an issue related to gender, yet it is increasingly evident that women are more affected by its impacts. Women of all ages are more vulnerable due to persistent cultural norms and low socioeconomic status. Women’s domestic roles often make them inconsistent users of nature-based resources such as firewood, water, and forest products. When these resources become scarcer, they experience an increased work burden. This is proved by many researchers that women in developing countries share the primary responsibility of providing basic needs like food (to feed) and water for their families; this is the cause behind their dependency on natural resources.

4.1 Climate Change

Climate change refers to long-term shifts in temperatures and weather patterns. These shifts may be natural, such as through variations in the solar cycle. But since the 1800s, human activities have been the main driver of climate change, primarily due to burning fossil fuels like coal, oil and gas. Burning fossil fuels generates greenhouse gas emissions that act like a blanket wrapped around the Earth, trapping the sun’s heat and raising temperatures. Burning of crop residues also adds to climate changes

Examples of greenhouse gas emissions that are causing climate change include carbon dioxide and methane. These come from using gasoline for driving a car or coal for heating a building. Clearing land and forests can also release carbon dioxide. Landfills for garbage are a major source of methane emissions. Energy, industry, transport, buildings, agriculture and land use are among the main emitters.

Key Facts
    
·    The United Nations Framework Convention on Climate Change (UNFCCC) defines ‘climate change’ as a ‘Change of climate which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over the comparable time periods’.
    
·    The main green house gases (GHGs) that have caused the global climate change or global warming are carbon dioxide (CO₂), methane (CH₄) and nitrous oxide (N₂O).
    
·    CO₂ is the principal anthropogenic GHG that affects the earth’s radiative balance. It is the reference gas against which other GHGs are measured and therefore has a Global Warming Potential (GWP) of 1. CH₄ and N₂O have a GWP of 21 and 310 respectively.
    
·    CO₂ is responsible for most of the enhanced green house effect of more than 50%, CH₄ for about 10-15% and N₂O for about 8%.
    
·    The global atmospheric concentrations of CO₂, CH₄ and N₂O have increased since 1750. While CO₂ increased from a pre-industrial value of 280 ppm to 379 ppm in 2005, CH₄ increased from 715 ppb to 1774 ppb and N₂O increased from 270 ppb to 319 ppb during the same period.

Summary

The main greenhouse gases (GHGs) that have caused the global climate change or global warming are carbon dioxide (CO₂), methane (CH₄) and nitrous oxide (N₂O). CO₂ is the principal anthropogenic GHG that affects the earth’s radiative balance. It is the reference gas against which other GHGs are measured and therefore has a Global Warming Potential (GWP) of 1. CH₄ and N₂O have a GWP of 21 and 310, respectively. CO₂ is responsible for most of the enhanced greenhouse effect of more than 50%, CH₄ for about 10-15% and N₂O for about 8%. The global atmospheric concentrations of CO₂, CH₄ and N₂O have increased since 1750. While CO₂ increased from a pre-industrial value of 280 ppm to 379 ppm in 2005, CH₄ increased from 715 ppb to 1774 ppb and N₂O increased from 270 ppb to 319 ppb during the same period. Rich countries and large developing countries account for most of global CO₂ emissions (China 23.5%, USA 18.27%, India 5.83%, Russia 5.72%, Japan 4.04% and European Union 13.98%). A new climate agreement called ‘Warsaw International mechanisms (November 2013) on loss and damage’ agreed to help the poor countries to cope with loss and damage from heatwaves, droughts, floods, typhoons, desertification and rising sea levels. The Warsaw agreement also includes a set of decisions to help developing countries to reduce GHG emissions from deforestation and degradation of forests which is backed by pledges of US$280 million financing by the United States, Norway and the United Kingdom. Projections for global average temperature rise is in the range of 1.1-6.4°C; a doubling of CO₂ (from pre-industrial 280 ppm) and average sea level rise is in the range of 0.18-0.59 m (Meehel et al. 2007) and 0.5–2.4 m (Brown et al. 2013). Hot extremes, heat waves and heavy precipitation events will continue to become more frequent. Projected data show that there is an increasing global trend in the rise of average temperature in all countries, regions or sub-zones; a decreasing trend in average precipitation in most sub-tropical areas and an increasing trend of precipitation in most of the tropical and high latitudes.

Key Facts
    
•    The United Nations Framework Convention on Climate Change (UNFCCC) defines ‘climate change’ as a ‘Change of climate which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over comparable time periods’.
    
•    The main green house gases (GHG) that have caused the global climate change or global warming are carbon dioxide (CO₂), methane (CH₄) and nitrous oxide (NO₂).
    
•    CO₂ is the principal anthropogenic greenhouse gas that affects the Earths radiative balance. It is the reference gas against which other GHGs are measured and therefore has a Global Warming Potential (GWP) of 1. CH₄ and N₂O have a GWP of 21 and 310 respectively.
    
•    CO₂ is responsible for most of the enhanced green house effect of more than 50%, CH4 about 10 to 15% and NO2 about 4%.
    
•    The global atmospheric concentrations of carbon-dioxide, methane and nitrous oxide have increased since 1750, CO₂ increased from a pre-industrial value of 280 ppm to 379 ppm in 2005, CH₄ increased from 715 ppb to 1774 ppb and NO₂ increased from 270 ppb to 319 ppb in 2005.

Introduction

Climate resilience is the capacity of a system, community, or person to foresee, prepare for, react to, and recover from the consequences of climate change while simultaneously preserving critical functions and minimising long-term harm. This ability is described as the ability to adapt to climate change. In order to handle the issues that are brought about by a changing climate, which include increasing temperatures, severe weather events, rising sea levels, and altering weather patterns, it is necessary to take a proactive approach.

Introduction

Global warming is a phenomenon of climate change characterized by a general increase in average temperatures of the Earth, which modifies the weather balances and ecosystems for a long time. In fact, the averages temperature of the planet has increased by 0.8° Celsius (33.4°F) compared to the end of the 19th century. Each of the last three decades has been warmer than all previous decades since the beginning of the statistical surveys in 1850. At the pace of current CO₂ emissions, scientists expect an increase of between 1.5° and 5.3°C (34.7° to 41.5°F) in average temperature by 2100 (Solarimpulse foundation, 2018). Most of the several dozens of predictive models indicate that average temperature can increase by 1.7-5.3°C, as a result of doubling CO₂ concentration within next 60-100 years. 2.3°C is a value most often mentioned what means an increase by 0.3°C a decade.

Climate change has emerged as the most pressing global challenge of the 21st century and which is one of the largest and most complex problems, the developed community has ever faced. The impacts of higher temperatures, variable precipitation, and extreme weather events have already begun to impact the economic performance of countries and the lives and livelihoods of millions of poor people. India is among the countries most vulnerable to climate change. It has one of the highest densities of economic activity in the world, and very large numbers of poor people who rely on the natural resource base for their livelihoods, with a high dependence on rainfall. By 2020, pressure on India’s water, air, soil, and forests is expected to become the highest in the world.

During the last few decades, the global agricultural production has risen and technology enhancement is still contributing to yield growth. However, population growth, water crisis, deforestation and climate change threatens the global food security.

Climate and weather strongly influence annual fluctuations in agricultural insect-pest populations. As ectothermic organisms, insects respond rapidly to variations in temperature, humidity, rainfall and wind. Climate change can modify their development, survival, reproduction, adaptation and geographical distribution. It may increase the number of generations, improve overwintering survival, alter host synchronization, encourage invasive species and reduce the effectiveness of natural enemies and existing control methods. Indirect effects also occur through changes in host-plant growth, resistance and nutritional quality. This chapter examines the responses of important agricultural insect pests to changing climatic conditions and discusses their implications for crop productivity and sustainable pest management.

Forests support diverse insect communities that contribute to pollination, decomposition, nutrient cycling and other ecological processes. Certain insects, however, become destructive pests when environmental changes weaken natural regulation and favour population outbreaks. Increasing temperature, altered precipitation, drought and land-use change can affect insect development, reproduction, survival and geographical range. Climate change may also disrupt synchronization between forest trees and associated insects, intensify native-pest outbreaks and facilitate the establishment of invasive species. Such changes can reduce tree growth, increase mortality and transform forest landscapes. This chapter examines climate-related forest-pest dynamics, ecological consequences and mitigation strategies for strengthening forest health and resilience.

Climate change affects horticultural crops through rising temperatures, irregular rainfall, extreme weather, altered carbon dioxide levels and changes in seasonal patterns. These conditions influence plant growth, flowering, fruit development, nutritional quality and geographical suitability. They also alter the development, survival, reproduction and distribution of horticultural insect pests. Warmer conditions may accelerate insect life cycles, increase the number of generations and intensify crop infestations. Changes in rainfall can either suppress pest activity or create favourable conditions for outbreaks. This chapter examines interactions among climate, horticultural crops and insect pests and highlights the need for proactive monitoring and climate-adaptive pest-management strategies to safeguard horticultural production.

Insect pollinators are essential for the reproduction of most flowering plants and contribute substantially to global crop production and food security. Bees, butterflies, moths, flies, beetles and other insects transfer pollen and support fruit and seed formation. Climate change can influence their physiology, development, activity, foraging, migration, distribution and seasonal emergence. It may also create mismatches between flowering periods and pollinator activity, reducing pollination efficiency. Drought, extreme heat, habitat loss and changes in floral resources further threaten pollinator diversity and abundance. This chapter examines the direct and indirect effects of climate change on insect pollinators and discusses conservation and management measures

Abstract

Climate change or elements of variability is a matter of great concern production positive, negative or natural impact on pest dynamics because of the specific nature of interactions of host, the pest and the environment. New pest such as Rice Whorl maggot, Flea beetal in rice/soybean and bark eating beetle in citrus are emerging with the change in climate pattern. Pest outbreaks in epemic form such as Rice hispa and rice ear cutting caterpillar are also noted. Location specific IPM packages with an emphasis on biological control are the need of the hour considering the threat of environmental pollution. The ecosystem diversification along with the study on natural enemies, spiders and coccinellids may be brought under purview.

Climate change is increasing the likelihood that invasive insects will establish, spread and cause economic damage in new geographical regions. Invasive species commonly possess high reproductive capacity, broad host ranges, environmental tolerance, ecological adaptability and competitive advantages. Rising temperatures and changing humidity and rainfall patterns can create favourable habitats beyond their traditional ranges. Extreme weather and global trade may further support their movement and establishment. Once introduced, invasive insects can compete with native species, disrupt ecosystems and cause serious crop losses. This chapter examines the relationship between climate change and invasive insect pests and emphasizes early detection, quarantine, surveillance, forecasting and coordinated management.

Introduction

Water and food security are the key challenges under climate change as both are highly vulnerable to continuously changing climatic patterns. Climate change has resulted in increases in globally averaged mean annual air temperature and variations in regional precipitation and these changes are expected to continue and intensify in the future. The projected changes in climate patterns over India include increase in surface temperature, variations in rainfall, increasing occurrence of extreme weather events like floods and droughts, rise in sea levels and impact on the Himalayan glaciers. Sectors of the Indian economy are most likely to be impacted by such changes in climate are those dependent on natural resources, namely agriculture, water and forestry. The likely impacts such as reduction in food production, water scarcity, loss of forest biomass Climate change is expected to bring more intense and more frequent extreme weather events including droughts and floods in India. The global atmospheric concentration of carbon di-oxide CO₂ for increased from preindustrial value of about 280 ppm to about 410 ppm at the present (2021). The global increase in CO₂ concentration is primarily due to fossil fuel use and land use change. Atmospheric methane was 1803 ppb in 2011, this is 150% greater than before 1750. Atmospheric nitrous oxide (N₂O) was 324 ppb in 2011, this is 150% greater than before 1750 (Table 1). These increase in GHGs have resulted in warming of the climate system by 0.74°C between 1906 and 2005.

The climate system is the highly complex system consisting of five major components; the atmosphere, the hydrosphere, the cryosphere, the land surface and the biosphere, and the interactions among them. The climate system evolves in time under the influence of its own internal dynamics and because of external forcings such as volcanic eruptions, solar variations and human-induced forcings such as the changing composition of the atmosphere and land-use.

The term ‘climate variability’ is often used to denote deviations of climatic statistics over a given period of time (e.g., a month, season or year) from the long-term statistics relating to the corresponding calendar period. In this sense, climate variability is measured by those deviations, which are usually termed anomalies.

‘Climate change’ refers to a statistically significant variation in either the mean state of the climate or in its variability, persisting for an extended period (typically decades or longer). Climate change may be due to natural internal processes or external forcings, or due to persistent anthropogenic changes in the composition of the atmosphere or in land use. The United Nation’s Framework Convention on Climate Change (UNFCCC) defines ‘climate change’ as ‘a change of climate behaviour which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over comparable time periods’. The UNFCCC thus makes a distinction between ‘climate change’ attributable to human activities altering the atmospheric composition, and ‘climate variability’ attributable to natural causes. Climate change is a long-term shift in weather conditions measured by changes in temperature, precipitation, wind, snow cover, and other indicators.

A key difference between climate variability and change is in persistence of ‘anomalous’ conditions. In other words, events that are used to be rare occur more frequently, or vice versa. Occasionally, an event or sequence of events occurs that has never been recorded before, such as the exceptional tsunami in the Indian Ocean in 2004 or hurricane season in the Atlantic in 2005. Yet even that could be a part of natural climate variability. If such a season does not recur within the next 30 years, by looking back it could be called as an exceptional year, but not a ‘climate change’. Only a persistent series of unusual events taken in the context of regional climate parameters can suggest that a potential change in climate has occurred.

Introduction

Any notable long-term alteration to the anticipated patterns of the average weather in an area (or the entire Earth) over an extended period of time is referred to as climate change. It concerns anomalous fluctuations in the climate and how these fluctuations affect other regions of the planet. Tens, hundreds, or even millions of years may pass before these changes occur. However, as a result of increased anthropogenic activity including industrialization, urbanization, deforestation, agriculture, and altered land use patterns, greenhouse gas emissions grow and accelerate the rate of climate change. Increases in temperature, variations in precipitation, and an increase in atmospheric CO₂ concentrations are all part of climate change scenarios.

Climate change is exerting profound effects on global agriculture, posing significant challenges to food security, agricultural productivity, and rural livelihoods. This article explores the intricate relationship between climate change and agriculture, examining how changes in temperature, precipitation patterns, and extreme weather events impact crop yields, livestock, and farming practices. It delves into the economic, social, and environmental repercussions of these changes, highlighting vulnerable regions and populations. The article also discusses adaptation and mitigation strategies, emphasizing the roles of technology, policy, and sustainable agricultural practices in building resilience. By understanding the multifaceted impact of climate change on agriculture, we can develop comprehensive approaches to ensure food security and sustainable development in an increasingly unpredictable climate.

Introduction

Climate change has been realised during 1840s when indisputable evidence of former ice ages was obtained. The climate has altered sufficiently in many parts of the world even within the last few decades which will affect the possibilities for agriculture and settlement. Reliable weather records have been kept only during the last hundred years or so, but proxy indicators of past conditions from tree rings, pollen in bog and lake sediments, ice core records of physical and chemical parameters, and ocean foraminifera in sediments provide a wealth of paleoclimatic data. The standard interval adopted by the World Meteorological Organization for climatic statistics is thirty years:1901–30, 1931–60, for example. However, for historical records and proxy indicators of climate, longer, arbitrary time intervals may be necessary to calculate average values. Tree rings and ice cores can give seasonal/annual records, while peat bog and ocean sediments may provide records with only 100- to 1,000-year time resolution. Hence, short-term changes and the true rates of change may, or may not, be identifiable.

The present climatic state is usually described in terms of an average value (arithmetic mean, or the median value in a frequency distribution), a measure of variation about the mean (the standard deviation, or interquartile range), the extreme values, and often the shape of the frequency distribution. A change in climate can occur in several different ways, for example, there may be a shift in the mean level, or a gradual trend in the mean values. The variability may be periodic, quasi-periodic or non-periodic, or alternatively it may show a progressive trend . First, it is important to determine whether such changes are real or whether they are an artefact of changes in instrumentation, observational practices, station location, or the surroundings of the instrumental site, or due to errors in the transcribed data. Even when changes are real, it may be difficult to ascribe them to unique causes because of the complexity of the climate system. Natural variability operates over a wide range of time scales, and superimposed on these natural variations in climate are the effects of human activities.

Global warming and climate change are becoming major challenges in the front of global community to deal with. Climate change is no more a myth but it is reality. The IPCC, 5^th assessment report clearly stated that “evidence of climate- change impacts is strongest and most comprehensive for natural systems”. Natural and human systems of almost all continents in the world have been affected by climate change in recent decades (IPCC, 2014). Agriculture is essential for sustainability of human life on earth but change in climate is threatening its sustainability. In recent decades all aspects of food security has been potentially affected by climate change, including food access, utilization, and price stability. It has been projected that in absence of adaptation measure, increases in local temperature by 2°C or more above late-20^th-century levels will negatively impact production of the major crops in tropical and temperate regions.

Agriculture is one of the major economic activities responsible for food security and livelihood for millions of people. Success, production and productivity of agricultural crops are highly dependent on climate, soil and water. Thus climate change will have adverse effect on agricultural crops. High atmospheric temperature, unpredicted erratic rainfall, rapid soil degradation and evolution of new insect and pests due to climate change will offer new challenge to sustain agriculture. Many part of the world and India is already experiencing impact of climate change on agricultural crops (like early maturity, geographical shift and occurrence of new pests) and these impacts are predicted to increase rapidly in future. The increasing concern about adverse impact of climate change on food security has led to extensive research and documentation of impact of climate change on field crops like rice, wheat and maize. While the clear and holistic idea about impact of climate change on horticultural crops like vegetables and fruits are not well documented especially in developing countries like India.

Stored-product insects damage grains, cereals, pulses and other commodities, causing quantitative losses and deterioration in food quality and nutritional value. Climate change influences temperature and humidity within storage environments, directly affecting insect development, reproduction, survival and population growth. Warmer conditions may shorten life cycles, increase the number of generations and expand the distribution of important storage pests. Poor storage structures and inadequate pest management further increase these risks, particularly in developing countries. This chapter examines the influence of changing climatic conditions on stored-product pests and emphasizes improved storage design, monitoring, sanitation and climate-adaptive management practices for protecting stored food and maintaining food security.

Abstract

Climate change is a change in the distribution of weather over periods of time that range. The effect of climate change is now visible every where including animal farm industry. Projected temperature rise around 2-5oC by 2100 due to climate change is likely estrus, start estrus and decline in reproduction efficiency of livestock species Climate change may have a significant effect on livestock and other animals through is impact on diseases Zoonotic diseases which can be transmitted between vertebrate animals and humans are a matter of great concerns. There is an urgent need for adoption of integrated approaches towards mitigation of advance effects of climate change in animal production. There are nutritional strategies to reduce enteric methane production. Surveillance and monitoring with various adaption strategies are to be brought under purvision to reduce adverse impact of climatic variability in livestock 

Abstract

Climate models predict a global average increase of air temperatures in the range of 14^°C by 2100 (IPCC 2014) - a pace exceeding that of past climatic modifications. Change in temperature is expected to influence species occurrence and distribution with up to 37% of all extant species “committed to extinction” due to climate change. These predictions, however, do not include species interactions and evolutionary change which will significantly alter the fate of species. It is therefore important to improve our understanding of host-parasite interactions and subsequent evolution in response to environmental changes in general and temperature changes in particular. Globally livestock production systems are estimated to account for around 18% of emissions. The need of hour is to draw on recent advances in climatology and epidemiology of various parasitic diseases to consider how environmental changes linked with urbanization and climate change can alter the biology of hosts, pathogens and vectors. Climate change is leading to unusual flare-up of diseases, outbreak recurrences, range expansions, or invasion into novel territories and ecosystems, concomitantly with vector or host range shifts. Higher temperatures increase the invertebrate metabolic rate, egg production amount, and feeding frequency, reducing the duration of the development periods and impacting on the number of generations per year and population abundance effecting livestock and human health and socio-economic transformation

Introduction
 
Climate change is a result from emission of greenhouse gases (e.g. CO₂, CH₄, N₂O, etc.) that will cause atmospheric warming (IPCC, 2007). Climate change may be due to natural internal processes or external forcing such as modulations of the solar cycles, volcanic eruptions, and persistent anthropogenic changes in the composition of the atmosphere or in land use. Human induced changes in atmosphere composition are a major concern. Burning of fossil fuels, like oil, coal, and natural gas is adding CO₂ to the atmosphere.

Mites are economically important pests of agricultural and horticultural crops whose development and population dynamics are strongly influenced by environmental conditions. Rising temperatures, drought, reduced humidity and altered rainfall can accelerate mite reproduction, shorten generation time and increase infestation severity. Climate change may expand the geographical range of damaging species, alter host suitability and disturb interactions with predatory mites and other natural enemies. Increased pesticide use following outbreaks may further disrupt biological control and encourage resistance. This chapter examines climate-related changes in mite biology, distribution and pest status and presents adaptive management strategies involving surveillance, resistant cultivars, biological control and integrated pest-management practices.

6.1 Introduction

The sensitivities of plants and of crop yield to a changing climate, is a major challenge for the agricultural research community to relate these findings to the broader societal concern with food security. This chapter reviews the direct effects of climate on both crop growth and yield and on plant pests and pathogens and the interactions that may occur between crops, pests, and pathogens under changed climate. The better understanding of the roles of pests and pathogens in crop production systems that might   make to enhanced food security is discussed. Evidence for the measured climate change on crops and their associated pests and pathogens is starting to be documented. Globally atmospheric CO₂ has increased, and in northern latitudes mean temperature at many locations has increased by about 1.0–1.4 ^°C with accompanying changes in pest and pathogen incidence and to farming practices. Many pests and pathogens exhibit considerable capacity for generating, recombining, and selecting fit combinations of variants in key pathogenicity, fitness, and aggressiveness traits that there is little doubt that any new opportunities resulting from climate change will be exploited by them.

Plant-parasitic nematodes are important soil-borne pests that reduce crop productivity by feeding on roots and interfering with water and nutrient absorption. Temperature, soil moisture, rainfall, carbon dioxide and host-plant conditions influence their development, reproduction, survival and geographical distribution. Climate change may allow certain nematode species to expand into new regions, complete additional generations and cause greater crop damage. Drought, flooding and altered soil conditions may also modify interactions among nematodes, plants, microorganisms and natural enemies. This chapter examines the likely effects of climate change on important plant-parasitic nematodes and discusses monitoring, forecasting and adaptive management approaches for climate-resilient crop protection.

Introduction

In India, almost 85 % of our population resides in rural areas and the same proportion is dependent on agriculture for sustenance and animal husbandry for additional income. Distribution of livestock is more equitable compared to that of land and about 85 percent of livestock are owned by the landless, marginal and small landholding families. This sector provides employment for the farmers through livestock farming as well as in processing, value addition and marketing of livestock products.

Rapid population, economic growth, increased demand for livestock products such as meat and dairy products, in?uences the present livestock production systemtowards intensive production. There is increased con?ict over scarce resources such as land, water, food grains etc. Losing livestock assets for rural communities might lead to abject poverty with serious effect ontheir livelihoods. The climate change impact will worsen the vulnerability of livestock systems and those farmers depending on livestock, particularly the poor.

Predatory arthropods provide valuable ecosystem services by suppressing agricultural pests and maintaining ecological balance. Important predators include ladybird beetles, lacewings, predatory bugs, spiders, mites and other groups that consume harmful insects at different developmental stages. Their small body size and ectothermic nature make them sensitive to changing temperature and moisture regimes. Global warming can affect their metabolism, development, body size, fecundity, longevity, dispersal and geographical distribution. Climate change may also disrupt temporal and spatial relationships between predators and their prey. This chapter examines the effects of climatic changes on predatory arthropods and their continuing role in natural and applied biological control.

Coffee is grown at higher elevation across the Western Ghats between 750 and 1200 m amsl. It requires a certain degree of shade for its better performance. The annual rainfall over the coffee growing tracts varies between 1400 and 2600mm, having uni/bi-model rainfall with prolonged dryspell from November to May. It is more so over North of the Western Ghats. The mean annual maximum temperature varies between 24 and 30⁰C while the minimum between 15 and 18⁰C. The difference between maximum and minimum temperatures (temperature range) varies between 5 and 16⁰C across the coffee tract. The ‘Monsooned Malabar Coffee’ is a specialty coffee produced from the erstwhile ‘Malabar Region’. It undergoes certain changes in physical and biochemical characters when the coffee beans are processed during the summer monsoon (June to September). It is processed at Mangalore, located in Coastal Karnataka. The processing location experiences heavy rainfall of more than 1000 mm in July, followed by 950 mm in June and 600 mm in August. Out of 3264 mm of annual rainfall, 2852 mm is received during the monsoon period. It accounts more than 80 per cent of annual rainfall. The maximum temperature during the monsooning varies between 28 and 30°C while night temperature revolves between 22 and 24°C. Being located in the tropics along the West Coast, the crop processing environment in terms of surface air temperature is relatively uniform and moderate with a characteristic feature of heavy clouds and continuous rainfall during the monsoon period.

Rice is one of the major staple food of the world’s population. About 114 countries grow rice and more than 50 have an annual production of 100,000 tonnes or more. Asian farmers produce about 90 per cent of the total, with two countries, China and India, growing more than half of the total crop. For most rice producing countries where annual production exceeds one million tonne, rice is the staple food. In Bangaldesh, Cambodia, Indonesia, Lao PDR, Myanmer, Thailand and Vietnam, rice provides 50–80 per cent of the total calories consumed.

Soil supports diverse arthropod communities, including insects, mites, springtails, spiders, millipedes and centipedes. These organisms contribute to decomposition, nutrient cycling, soil formation, microbial regulation and food-web stability. Their activities improve soil fertility, structure and overall ecosystem functioning. However, soil arthropods are highly responsive to temperature, moisture, vegetation and other environmental factors. Global warming, altered rainfall, drought and changes in soil properties can modify their diversity, abundance, distribution and ecological interactions. Despite their importance, climate-change effects on soil arthropods remain comparatively understudied. This chapter examines their ecological roles, relationships with soil properties and responses to changing climatic conditions in agricultural ecosystems.

Introduction

The problem of dealing with climate change, a critical global issue, has come to define our era. Human activities are rapidly altering Earth’s climate, with far- reaching repercussions for many industries, including agriculture. The necessity for environmentally responsible food production is pressing as the global population rises. One possible way to lessen the effects of global warming on food production is to adopt the sustainable agriculture practice of striking a balance between environmental protection, social justice, and economic viability. The impacts of climate change on farming may be seen all across the world right now. Global food security is threatened by climate change, which is causing higher temperatures, changing precipitation patterns, and increasing extreme weather events. Greenhouse gas emissions, deforestation, and unsustainable farming practices all have a hand in accelerating global warming. Therefore, it is crucial to tackle the double problem of lowering agriculture’s environmental imprint while also adapting it to climate change. Sustainable agriculture works toward a compromise by encouraging robust and flexible agricultural practices. It aims to ensure the sustainability of food production in the future while reducing environmental effects by incorporating climate change adaptation and mitigation techniques into agricultural practices. Agricultural systems can be made more resistant to climate change by the use of sustainable farming practices such as agroforestry, crop diversification, soil conservation, and water management. Sustainable farming practices help communities adapt to climate change, boost local economies, and secure food supplies for future generations.

2.1 Introduction

Weather has always been a popular topic but in the recent past it has received wide attention and debate as the public concern has increased about unforeseen changes in our climate. Over the 20^th century the average temperature of the earth has increased by 0.4 -0.8^oC. This increase is expected to continue and by 2100 the average global temperature is likely to be 1.4 - 5.8 ^oC warmer. One of the anticipated effects of climate change is the possible increase in both frequency and intensity of extreme weather events, such as heat waves, cold waves, hurricanes, floods and drought spells. The warming of the earth may fuel interactions between the ocean and atmosphere that will amplify the frequency and intensity extreme weather events. The possible changes in the frequency, distribution and intensity of extreme climate events have a significant influence at local, regional and global scales due to their multi-sectoral impacts on the overall economy.

Climate change significantly impacts agriculture, altering growing conditions, crop yields, and the livelihoods of farmers. Rising temperatures and shifting precipitation patterns can lead to more frequent and intense droughts, floods, and storms, which disrupt planting and harvesting schedules and reduce crop productivity. Changes in temperature and precipitation can also exacerbate pest and disease pressures, making it harder for farmers to protect their crops. Additionally, the increased frequency of extreme weather events can damage infrastructure and soil health, further challenging agricultural systems. These effects pose serious threats to food security, necessitating the development of climate-resilient farming practices and crop varieties, as well as policies that support sustainable agricultural development and climate adaptation.

The climate change is not “gender neutral”. Women and girls experience the greatest impacts of climate change, which amplifies existing gender inequalities and poses unique threats to their livelihoods, health, and safety.

Climate change effect on women

1. Reduced Agricultural Productivity: Climate change leads to crop failures, reduced yields, and changed growing seasons, affecting women’s income and food security.

2. Increased Water Scarcity: Changes in precipitation patterns and increased evaporation lead to water scarcity, forcing women to travel farther for water, reducing their time for other activities.

3. Soil Erosion and Degradation: Flooding and erosion caused by climate change degrade soil quality, reducing fertility and affecting crop growth, further threatening women’s livelihoods.