eChapters

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.