eChapters

Weather phenomena are not localized, it moves and varies over space and time. The weather over a place or area is the result of far away weather events/conditions. Acquisition of global scale observation, therefore, becomes a pre-requisite for understanding the physics of the weather and also to represent the weather condition over an area at a particular time. Complex three-dimensional models of weather systems can be made by collecting weather data at multiple levels in the atmosphere. Upper-air data are important to know present weather over a place and crucial for weather forecasting.

Wind influences the plant life both physiologically and mechanically. Wind affects plant directly by increasing the transpiration and intake of CO₂. Thus raising the supply of CO₂ to the plants and thereby increase in photosynthesis. However, the increase in photosynthesis is again upto a certain wind speed beyond which its rate become constant. The warm and dry winds increase evaporative loss and cause moisture stress. Lodging is one of severe injury caused by strong winds which causes great yield loss depending upon the stage of crop. This injury is common in paddy, maize, wheat, sorghum and sugarcane. Strong winds damage fruit trees extensively by breaking leaves and twigs and causing fruit drops.

Surface-Enhanced Raman Spectroscopy (SERS) may detect and identify chemical and biological species ultrasensitively. Through localized surface plasmon resonance (LSPR) effects, metal nanostructures boost analyte Raman signals. This chapter covers current advances and essential principles in metal nanostructures for SERS chemical detection. It discusses SERS fundamentals and enhancing processes, such as metal nanostructure size, shape, and composition. Top-down and bottom-up processes including lithography, chemical synthesis, and self-assembly are used to create repeatable and controllable metal nanostructures. The complex interactions between light, metal nanostructures, and analyte molecules are best understood by combining theoretical modeling and experimental observations. 

7.1 Introduction
The preceding chapters have detailed the myriad ways in which meteorological data is collected, from direct in situ observations to various ground-based and space-borne remote sensing platforms. We have also explored the crucial aspects of data formatting, storage, and retrieval, recognizing the immense volume and diversity of atmospheric information. However, the journey from raw measurement to actionable insight is not complete without a critical intermediate step: data quality control (QC) and preprocessing. No observational system, regardless of its sophistication, is entirely free from errors, biases, or inconsistencies. Sensors can drift, communication links can suffer interference, environmental factors can contaminate readings, and automated systems can malfunction. Consequently, raw meteorological data often contains spurious values, missing records, or systematic biases that, if left unaddressed, can severely compromise the accuracy of weather forecasts, the reliability of climate analyses, and the validity of scientific research.
This chapter will delve into the essential processes of quality control, which involves rigorously identifying, flagging, and, where appropriate, correcting or removing erroneous data points. We will explore various automated and manual techniques employed to ensure the integrity and reliability of meteorological observations. Furthermore, we will examine preprocessing steps, which prepare the quality-controlled data for its intended use, including tasks such as unit conversions, interpolation to common grids, and handling of missing values. By understanding the meticulous procedures involved in data
quality control and preprocessing, we gain a profound appreciation for how raw atmospheric signals are transformed into the trustworthy information that underpins all of modern meteorology.

Meteorology is not merely the study of weather patterns; it is a critical science that intersects agriculture and allied sectors in numerous ways. In a world where food security is intimately tied to climatic variability, understanding the basic principles of meteorology is essential for both traditional farming practices and modern integrated food production systems. This chapter explores the foundational concepts of weather and climate, examines the atmospheric dynamics that directly impact agricultural systems, and contrasts historical meteorological practices with modern forecasting approaches. By delving into these topics, we can better appreciate how the environment influences agricultural productivity and how innovative meteorological tools can improve decision-making in the food production chain. Weather describes the state of the atmosphere at a specific time and place. It is the sum of short-term atmospheric conditions such as temperature, humidity, precipitation, wind, and visibility. In contrast, climate refers to the long-term average of weather patterns over a period of decades or more. Understanding this distinction is crucial for agriculture, as farmers and allied sector professionals must respond to immediate weather events (such as sudden frost or heavy rainfall) while also adapting to long-term climatic trends (like gradual temperature increases or shifting precipitation patterns).

Meteorological hazards are severe and extreme weather and climate events that occur in all parts of the world, although some regions are more vulnerable to certain hazards than others. Meteorological hazards include cyclones, droughts, floods, hurricanes, hailstorms, heat waves and tornadoes. The hazard is distinguished from an extreme event and a disaster. An extreme event is simply an unusual event; it does not necessarily cause harm. A disaster is an event that does cause harm in significant amounts. Meteorological hazards are often called as natural hazards. The natural hazards become natural disasters when people’s lives and livelihoods are destroyed.

Hydrological hazards are the result of either excess or a severe lack of water, i.e., flood or drought. Hydrometeorological hazard is a process or phenomenon of atmospheric, hydrological or oceanographic nature that may cause loss of life, injury or other health impacts, property damage, loss of livelihoods and services, social and economic disruption, or environmental damage. Human and material losses caused by natural disasters are a major obstacle to sustainable development. By issuing accurate forecasts and warnings in a form that is readily understood and by educating people about how to prepare against such hazards, before they become disasters, lives and property can be protected.

Abstract

Agroforestry is an integrated self-sustainable land use management system that is not only capable of producing food from marginal agricultural land but also capable of maintaining and improving the quality of environment. It plays a vital role in achieving integrated rural and urban development. But reliable data on number of trees and area under agroforestry is not available as methodology for estimation of even area under agroforestry is not yet standardized. In this paper, a methodology for estimation of number of trees under agroforestry using high resolution satellite data has been proposed and estimation of number of trees as well as area under agroforestry in Ludhiana district of Punjab State has been done using the proposed methodology. Land use/land cover map of the district has also been generated using ERDAS IMAGINE software. It has been observed from the accuracy assessment that the estimates of number of trees as well as area under agroforestry obtained using the proposed methodology under this study are very reliable. Therefore, the proposed methodology may be replicated for estimating number of trees as well as area under agroforestry in other parts of the country.

Keywords: Agroforestry; Estimation of number of trees, Area estimation; Remote Sensing; GIS

Methods of fertilizer application

Two major methods are used to apply fertilizers  
I) Application of fertilizers in solid form 
II) Application of fertilizers in liquid forms

10.1 Introduction

As one ofthe oldest and most widely used renewable energy sources, hydropower generates electricity by using the natural flow of flowing water. Streams and rivers have been used for producing mechanical energy for thousands of years. Hydroelectric power plants are located near or on water sources since they derive their power from flowing water. The amount of energy that can be released in moving water depends on the volume of the water flowing and the elevation change from one point to another, often called head. Generally, hydropower plants can produce more electricity when there is more water flow and a higher head. 

Microalgae have long been recognized as good potential sources for biofuel production due to their relatively high oil content and rapid biomass production (Schenk et al., 2008; Hu et al., 2008). These photosynthetic organisms thrive in a variety of aquatic habitats, including lakes, rivers, oceans, and even sewage, demonstrating their adaptability to diverse environmental conditions. They can tolerate a wide range of temperatures, salinities, and pH levels, as well as varying light intensities and aquatic or desert conditions. Additionally, microalgae can grow independently or in symbiosis with other organisms, making them highly versatile for various cultivation systems (Mutanda et al., 2011). Algae are generally grouped into three major categories: Rhodophyta (red algae), Phaeophyta (brown algae), and Chlorophyta (green algae), and are further classified by size into macroalgae and microalgae. Macroalgae are large, multicellular organisms visible to the naked eye, while microalgae consist of microscopic single cells that can be either prokaryotic, similar to cyanobacteria, or eukaryotic, similar to green algae (Fields et al., 2014; Maltsev & Maltseva, 2021). Microalgae are capable of producing a wide array of valuable bioproducts, including polysaccharides, lipids, pigments, proteins, vitamins, bioactive compounds, and antioxidants. They grow at a much faster rate compared to terrestrial crops and can be cultivated on non-agricultural land using non-potable saltwater or wastewater, reducing competition with food crops and ensuring sustainability (Lee et al., 2014). This has made microalgae an increasingly attractive alternative feedstock for biodiesel production, which relies heavily on the high lipid content of microalgae. The majority of these lipids are stored in the form of triacylglycerols, a type of oil that is ideal for biodiesel production. Beyond biodiesel, microalgae can also be utilized in various other energy production pathways. Some microalgal strains can produce hydrogen gas under specific growth conditions, while algal biomass can be combusted like wood or digested anaerobically to produce methane biogas, which can be used for heat and power generation. Additionally, algal biomass can be processed into crude bio-oil through pyrolysis, further expanding its applications as a renewable energy source (Mumtaz et al., 2019).

Nowadays, revolutionary changes in entire globe have led to the economic, cultural and scientific development in our society and have augmented considerable changes in our food habits and life-style. Continuously growing population had noticeably increased the pressure on land, water and energy resources. All these resources are scarce and going to be exhausted in coming decades at the present rate of consumption. Undoubtedly, production of food is more imperative than the production of energy or any other bioproducts. Moreover, with the world population rising to 9 Billion in 2050, with many inspiring to a western life style and diet, this challenge should be addressed urgently (Draismaa et al., 2013). The challenge to produce about 70% more food by 2050 for a growing and increasingly affluent world population has motivated several review papers addressing the different dimensions of the food system and food security (Verburg et al., 2013). Presently, human beings consume approximately 2.5 billion tons of dry weight of harvested crops which include approximately 2.3 billion tons of cereals (e.g., rice, wheat, and corn kernels) and grass from managed pastures (Smil, 2000).

Introduction 
Fossil Fuels like Coal, Coal product, Natural Gas, Petroleum, Crude Oil provide 80% of the world’s energy. However, burning them releases harmful pollutants, including carbon dioxide, nitrogen oxides and the sulfur oxides, contributing to global warming. To combat this, the World is shifting towards cleaner, renewable energy sources called biofuels. Biofuels are made from organic materials like plants and waste, offering several benefits: Renewable and Sustainable, Less greenhouse gas emissions, non-toxic [6]. Common biofuels include are: Biodiesel, Biogas, Bioethanol. These alternative fuels help reduce our reliance on fossil fuels, mitigating climate change and promoting a healthier environment. Biodiesel replaces fossil-based diesel/petrol made through Trans-esterifi cation process. The benefi ts include clean energy, renewable resources and the domestic production. Generations of biodiesel are: First Generation include Edible crops (Soybean, Corn, Sugarcane). Second Generation includes Non-edible biomass(Straw, Hay). Third Generation include Microalgae (70% yield). Fourth Generation include the genetically modifi ed algae and electro-biofuel. [2] Biodiesel production has changed over time. Initially, edible vegetable oils like soybean, corn, sunfl ower and palm oil were used. However this raised concerns: using valuable farmland for fuel instead of food, competing with food production, weather and soil quality affecting the crop yield , fertilizer use releasing harmful nitrous oxide greenhouse gas. To address these issues, focus shifted to non-edible oils and now Microalgae, offering; sustainable, climate-resilient production, no competition with the food crops, reduced greenhouse gas emission, higher oil yield. Microalgae -based biodiesel is the future providing a cleaner, more effi cient alternative.[4]

Introduction 
Fuels are essential to human existence and account for 70% of the world’s energy use. The demand for fossil fuels is rising daily due to the ongoing global population boom and has now reached a crisis point. The world’s current reserves cannot keep up with the projected 40% rise in demand between 2010 and 2040 [1]. According to Energy Information Administration (EIA) statistics, the world’s fossil fuel sources will run out in fewer than 50 years [2]. In addition, burning fossil fuels and living in an industrialised environment have released large amounts of carbon dioxide (CO2), carbon monoxide (CO), sulphur dioxide (SO2), nitrogen oxides (NOx), as well as a significant number of potentially toxic compounds into the atmosphere. This has severely degraded the natural resources that are currently available, including fossil fuels. The human and natural ecology have suffered significant damages as a result of the effects of global warming in recent years [3]. As a result, cutting CO2 emissions is crucial to preventing the negative effects of global warming. Therefore, there has been a greater focus on the improvement of CO2 capture and sequestration systems to significantly lower CO2 emissions from a variety of sources, including vehicle exhaust emissions and industrial flue gas [4] . Fuel production needs to be sustainable in terms of the environment and the economy, meaning it needs to be able to reduce CO2. It is critical to find inexpensive, sustainable, and clean energy options in order to handle the current circumstances. Currently, several traditional renewable energy sources, such as solar, biofuels, hydroelectric, geothermal, or wind are being used with varying degrees of success and detriment. Biofuels are sustainable and renewable energy sources that have emerged as a superior alternative to traditional fossil fuels in energy production. Biofuels have a lot of potential because they are abundant environmentally favourable renewable resources and their production is expanding globally, even though they are still more expensive than fossil fuels [5]. Researchers are actively investigating biomasses as a means of obtaining energy from renewable sources. It is commonly known that through a process called photosynthesis, plants can transform sun energy into chemical forms. Microalgae are fast-growing microorganisms that develop 100 times quicker than terrestrial plants. Their photosynthetic efficiency is also higher (10–50 times greater than terrestrial plants) among biomasses [6]. In less than a day, they can double their biomass. Unicellular microalgae, in contrast to plants, do not divide substantial amounts of biomass into supporting structures like stems or roots, which are costly to create energetically and frequently challenging for harvesting and processing to produce biofuel. Furthermore, they have the ability to adapt to harsh aquatic environments and economically absorb helpful substances. Moreover, 1 kg of microalgae biomass is produced by microalgae cells that fix 1.8 kg of CO2 and have a 50% carbon content [7]. Microalgae can be grown on terrain that is inappropriate for food production because of their high total yield and hence small land use footprint [8]. Microalgal species including Scenedemus sp., Chlorella sp., and Botryococcus sp.; are common, easier to grow than other species and may have higher lipid contents [9].

1.    Introduction    360
2.    Feedstocks for Biodiesel Production    361

    2.1.    Fats and oils, 362
    2.2.    Alcohols, 363
    2.3.    Catalysts and neutralizers, 367

1.    Introduction    468

2.    Biofuel Cell    470

    2.1.    Microbial-based Biofuel Cells, 471
        2.1.1.    Microbial bioreactors producing H2 for conventional fuel  cells, 475
        2.1.2.    Microbial fuel cells producing electrochemically active metabolites in  
                the anodic compartment, 476
        2.1.3.    Microbial fuel cells operating in the presence of artificial electron relays, 477
        2.1.4.    Microbial fuel cells producing electricity during wastewater treatment, 483
        2.1.5.    Microbial fuel cell producing  electricity from acetate or butyrate, 484

1.    Introduction    302
2.    Raw Materials for Alcohol Production    304

    2.1.    Sugary substrates, 306
    2.2.    Starchy residues (cereal grains), 309
    2.3.    Cellulosic materials (crop residues), 314

3.    Microorganisms for Alcohol Production    316

    3.1.    Comparision of ethanol production by bacteria and yeasts, 318

1.     Introduction    424

2.    Conventional Methods of Hydrogen Production    426

3.    Biological Methods of Hydrogen Production    429

    3.1.    Hydrogen production by biophotolysis of water, 430
        3.1.1. Photolysis by cyanobacteria (Blue green algae), 430
            3.1.1.1. Nitrogenase dependent hydrogen production, 434
            3.1.1.2.  Hydrogenase-dependent hydrogen production, 437
            3.1.1.3.  Factors affecting  hydrogen production by cyanobacteria, 440
            3.1.1.4.   Bioreactors for cyanobacterial hydrogen production, 443
            3.1.1.5. Future prospects for cyanobacterial hydrogen production, 446

1.    Introduction    392

2.    Landfill Gas    393

3.    Biogas    394

    3.1.    Benefits of biogas, 394
    3.2.    Potential of biogas, 395
    3.3.    Biogas production system, 396
        3.3.1.    Raw materials, 396
        3.3.2.    Biogas technology, 398
        3.3.3.    Process of anaerobic fermentation for methane generation, 400
        3.3.4.    Conditions for anaerobic fermentation, 404
        3.3.5.    Sludge-algae-methane system, 407
        3.3.6.    Biogas plant, 408

1.    Introduction    272
2.    Alcohols    273

    2.1.    Methanol, 274
    2.2.    Ethanol, 277
    2.3.        Butanol, 283

3.    Biodiesel    284
4.    P-series fuels

Abstract

Microorganisms inhabiting in the rhizosphere play a vital role in ecosystem functioning. Rhizosphere is an area around the root surface where pathogenic and beneficial microorganisms repose and influence the plant growth and health. These microbial groups of bioagents found in the rhizosphere include bacteria, fungi, nematodes, protozoa, algae and micro-arthropods. Because of their rich diversity, complexity of interactions and numerous metabolic pathways, microbes are an amazing resource for biological activity. These microorganisms require organic matter for their growth and activity in soil and provide valuable nutrients to the plants and hence maintaining the plant health. The most promising fields for the use of bioinoculants are agriculture, horticulture and forestry. There are many reports on the inoculation of bioagents in agriculture and horticulture crops but only a few reports are available in forestry. This article is an overview on various bioinoculants which are used during inoculation and a compilation of scattered reports of bioinoculants in forestry only.