The density and distribution of climatological stations to be established in a land network within a given area depend on the meteorological elements to be observed, the topography and land use in the area, and the requirements for information about the specific climatic elements concerned. This module highlights all these aspects.
The document discusses various aspects of weather forecasting by the National Weather Service and U.S. Navy. It describes the different types of forecasts produced, including area forecasts by major Navy units, flight forecasts for successive flight stages, and local forecasts by ships and stations. It also outlines the roles of organizations like the National Oceanic and Atmospheric Administration, National Weather Service, and Navy Meteorology and Oceanography Command in coordinating weather data collection and forecasting activities.
Weather forecasting is the prediction of the state of the atmosphere for a given location using the application of science and technology. This includes temperature, rain, cloudiness, wind speed, and humidity. Weather warnings are a special kind of short-range forecast carried out for the protection of human life. This module explains the details of weather forecasting.
Meteorology is the scientific study of the atmosphere and weather processes. The field has a long history dating back millennia, though significant progress occurred in the 18th century with observing networks. Meteorologists work in various sectors to forecast weather and study atmospheric phenomena across micro, meso, and synoptic scales. Key instruments invented over time include the rain gauge, thermometer, barometer, hygrometer, and aneroid barometer, enabling the detailed study and prediction of weather and climate.
Earth's early atmosphere contained hydrogen and helium. After the Moon formed, volcanic activity produced CO, CO2, and water vapor. Once cyanobacteria evolved and performed photosynthesis, they consumed CO2 and produced oxygen. Currently, Earth's atmosphere is 78% nitrogen, 21% oxygen, and 1% trace gases. Burning fossil fuels adds excess CO2 and pollutants, warming the climate. CFCs have also depleted the ozone layer.
Meteorology is a discipline concerned with observational earth sciences and theoretical physics. It has the task of providing an accurate knowledge of the state of the atmosphere. Before the advent of weather satellites the weathermen had been severely handicapped by having only a very limited knowledge of the state of the atmosphere at any given time. Meteorological satellites have to a large extent has enabled to overcome this deficiency.
The document discusses weather forecasting. It describes the process of forecasting as involving observation, collection and transmission of weather data, plotting and analysis of this data, and then analysis of weather maps and other tools to formulate a forecast. Key tools used in forecasting include weather maps, satellite and radar images, and numerical weather prediction models. The accuracy of forecasts depends on knowledge of weather conditions over a wide area.
The document provides information about weather maps and weather concepts. It discusses key elements of weather maps including isobars, pressure cells, wind direction and speed. It explains that high pressure cells bring clear skies while low pressure cells bring cloud and rain. It also summarizes different types of rainfall including convectional, orographic and frontal rainfall. Seasons are determined by the positioning of pressure systems with lows over northern Australia in summer and highs in winter.
Meteorology is the scientific study of the atmosphere and weather forecasting. The word was coined from Aristotle's book Meteorologica in ancient Greece, which described earth sciences including weather. Significant progress occurred in the 18th century with observing networks and breakthroughs in the 20th century after computer development. Key early inventions included Galileo's thermometer, Torricelli's barometer, and weather instruments to measure variables like wind, humidity and rainfall. Modern meteorology has benefited from technology allowing rapid data sharing and atmospheric probing with balloons, satellites and radars.
The document discusses various aspects of weather forecasting by the National Weather Service and U.S. Navy. It describes the different types of forecasts produced, including area forecasts by major Navy units, flight forecasts for successive flight stages, and local forecasts by ships and stations. It also outlines the roles of organizations like the National Oceanic and Atmospheric Administration, National Weather Service, and Navy Meteorology and Oceanography Command in coordinating weather data collection and forecasting activities.
Weather forecasting is the prediction of the state of the atmosphere for a given location using the application of science and technology. This includes temperature, rain, cloudiness, wind speed, and humidity. Weather warnings are a special kind of short-range forecast carried out for the protection of human life. This module explains the details of weather forecasting.
Meteorology is the scientific study of the atmosphere and weather processes. The field has a long history dating back millennia, though significant progress occurred in the 18th century with observing networks. Meteorologists work in various sectors to forecast weather and study atmospheric phenomena across micro, meso, and synoptic scales. Key instruments invented over time include the rain gauge, thermometer, barometer, hygrometer, and aneroid barometer, enabling the detailed study and prediction of weather and climate.
Earth's early atmosphere contained hydrogen and helium. After the Moon formed, volcanic activity produced CO, CO2, and water vapor. Once cyanobacteria evolved and performed photosynthesis, they consumed CO2 and produced oxygen. Currently, Earth's atmosphere is 78% nitrogen, 21% oxygen, and 1% trace gases. Burning fossil fuels adds excess CO2 and pollutants, warming the climate. CFCs have also depleted the ozone layer.
Meteorology is a discipline concerned with observational earth sciences and theoretical physics. It has the task of providing an accurate knowledge of the state of the atmosphere. Before the advent of weather satellites the weathermen had been severely handicapped by having only a very limited knowledge of the state of the atmosphere at any given time. Meteorological satellites have to a large extent has enabled to overcome this deficiency.
The document discusses weather forecasting. It describes the process of forecasting as involving observation, collection and transmission of weather data, plotting and analysis of this data, and then analysis of weather maps and other tools to formulate a forecast. Key tools used in forecasting include weather maps, satellite and radar images, and numerical weather prediction models. The accuracy of forecasts depends on knowledge of weather conditions over a wide area.
The document provides information about weather maps and weather concepts. It discusses key elements of weather maps including isobars, pressure cells, wind direction and speed. It explains that high pressure cells bring clear skies while low pressure cells bring cloud and rain. It also summarizes different types of rainfall including convectional, orographic and frontal rainfall. Seasons are determined by the positioning of pressure systems with lows over northern Australia in summer and highs in winter.
Meteorology is the scientific study of the atmosphere and weather forecasting. The word was coined from Aristotle's book Meteorologica in ancient Greece, which described earth sciences including weather. Significant progress occurred in the 18th century with observing networks and breakthroughs in the 20th century after computer development. Key early inventions included Galileo's thermometer, Torricelli's barometer, and weather instruments to measure variables like wind, humidity and rainfall. Modern meteorology has benefited from technology allowing rapid data sharing and atmospheric probing with balloons, satellites and radars.
This document discusses weather forecasting and understanding weather maps. It explains that weather maps show isobars which indicate wind patterns around high and low pressure systems. Closer isobars mean stronger winds. It describes features of high and low pressure systems including wind direction. Cold fronts are shown where cold air pushes warm air upwards, potentially causing rain. Mechanisms that can trigger rain include fronts, low pressure systems, hills and turbulence. Clouds alone do not guarantee rain as clouds need sufficient moisture and lifting of air to produce meaningful rainfall.
This document discusses basic concepts about weather and climate. It defines weather as the current atmospheric conditions in a place, while climate refers to typical weather patterns over a longer period of 30 years. It describes various elements that affect weather and climate, such as temperature, precipitation, atmospheric pressure, winds, and ocean currents. It provides examples of how these elements are measured and influenced by factors like latitude, altitude, and distance from the sea.
The document discusses weather maps and how they are used to predict weather conditions. It provides information on several key topics:
- The atmosphere helps regulate Earth's temperature and creates weather through the movement of air masses. Weather maps show current conditions.
- Weather is influenced by properties like temperature, humidity and pressure. Maps depict systems like cold fronts, warm fronts and stationary fronts to understand weather changes.
- High and low pressure areas circulate clockwise and counterclockwise respectively, affecting wind patterns and whether conditions will be clear or stormy. Weather maps are interpreted to forecast upcoming weather.
1. The document discusses key concepts about Earth's atmosphere including how solar radiation drives global climate and local weather patterns.
2. It explains different climate types based on factors like latitude, proximity to bodies of water, and elevation. Humid climates receive more precipitation than potential evapotranspiration while arid climates experience the opposite.
3. Atmospheric circulation patterns like global wind belts and ocean currents play an important role in moderating Earth's climate by transporting heat energy from the tropics to poles and distributing it around the globe over long time periods.
1. The document discusses weather elements such as temperature, precipitation, wind speed, and cloud cover. It also describes how these elements are measured using instruments like a thermometer, rain gauge, and anemometer.
2. Common types of clouds are described as cirrus, cumulonimbus, cumulus, and stratus. The Stevenson screen, used to shelter instruments, is also characterized.
3. The difference between weather and climate is explained as weather referring to short term atmospheric conditions while climate describes average conditions over a long period.
The document discusses atmospheric stability and its relationship to moisture and weather. It defines stable, unstable, and conditionally unstable atmospheres based on environmental lapse rates. Stability impacts cloud formation and precipitation - unstable air leads to tall clouds and heavy rain while stable air suppresses vertical air movement and yields light precipitation. Daily changes in temperature and moisture content can increase or decrease atmospheric stability.
Weather forecasting is important for agriculture as it allows farmers to plan for and adjust to upcoming weather conditions. There are different types of forecasts including nowcasting (up to 1 day), short range (1-3 days), medium range (3-10 days), and long range (>10 days). Accurate forecasts can help minimize losses from adverse weather and optimize input use through timely adjustments. Forecasting methods include synoptic analysis of surface and upper air charts, statistical analysis of historical weather data, and numerical weather prediction using physics-based models. The reliability of forecasts depends on factors like weather data collection and dissemination systems, forecaster experience, and forecasting technology.
This document discusses condensation and the formation of fog and clouds. It begins by defining condensation as the process where a gas transforms into a liquid due to changes in pressure and temperature. It then discusses the necessary and sufficient conditions for condensation to occur, including cooling air to below its dew point until saturated and the presence of condensation nuclei. The document proceeds to describe different types of fog like radiation fog, advection fog, and freezing fog that form through various cooling mechanisms. It also covers cloud condensation nuclei and the classification system used to identify different types of clouds.
Fronts are boundaries between two air masses of differing characteristics. There are four main types of fronts: cold fronts, warm fronts, occluded fronts, and stationary fronts. Cold fronts are steep boundaries where cold air overrides warm air, bringing precipitation. Warm fronts are more gradual, with light, continuous precipitation as warm air rises over cold air. Occluded fronts occur when a cold front catches up to a warm front. Stationary fronts have little or no movement as the air masses are parallel.
Structure and Composition of the Atmospherebeaudry2011
The atmosphere is composed of gases, water droplets, and particles surrounding Earth. It has four main layers - the troposphere, stratosphere, mesosphere, and thermosphere - each decreasing or increasing in temperature with altitude. The troposphere is where weather occurs, extending 8-16km high. Above is the stratosphere where temperatures increase with little weather, then the mesosphere where temperatures decrease again up to 80km. The thermosphere is the outermost layer with increasing temperatures from 80km high. The atmosphere composition consists primarily of nitrogen, oxygen, argon, and trace gases. Water vapor is the most abundant variable gas.
This document discusses remote sensing and meteorology. It defines remote sensing as obtaining information about physical objects through non-contact sensors. Meteorology is the study of atmospheric phenomena like weather. Meteorological satellites and weather radars are important tools for monitoring weather. Satellites provide global coverage of cloud patterns and weather systems from space. They capture visible, infrared, and water vapor images to study cloud formations, temperatures, and moisture in the atmosphere. Radar emits microwaves that bounce off water droplets in clouds to measure precipitation and cloud locations. Satellite weather monitoring improves forecasts, especially over oceans with sparse weather station data.
Cyclones and western disturbances By Lohit Sainilohitsaini
Cyclones are intense low pressure weather systems characterized by strong circulating winds. They are classified as either extra-tropical or tropical cyclones. Tropical cyclones form over warm tropical waters and include hurricanes and typhoons. They develop through several stages from a tropical disturbance to a mature storm. Formation requires warm ocean waters, moisture, coriolis force, and low wind shear. Western disturbances originate in the Mediterranean and bring winter precipitation to South Asia when moisture is shed over the Himalayas. They are important for rabi crop growth but can also cause flooding.
Weather forecasting involves collecting data from weather stations, analyzing trends, and predicting future conditions for a given location. Data on temperature, pressure, wind, humidity and more is recorded, transmitted to analysis centers, and plotted on maps and charts. Forecasters use tools like radiosondes, radar, and weather satellites to monitor cloud and storm activity. Forecasts are categorized as short range up to 48 hours, medium range from 3 days to 3 weeks, or long range from 2 weeks to a season. Short range forecasts rely on current conditions while medium and long range try to predict average trends.
This document provides an introduction to climatology, including definitions of key terms and branches of the field. It discusses how climatology studies the atmosphere and spatial patterns of climate. Climatology is related to both meteorology, which deals with day-to-day weather, and geography, which studies spatial climate distributions. The document also outlines the major layers of the atmosphere and characteristics of atmospheric gases like carbon dioxide and ozone.
The document discusses air masses and fronts. It defines air masses as large bodies of air with uniform properties that form over land or water surfaces. There are four main types of air masses classified by their region of formation: maritime/continental and polar/tropical. Fronts are boundaries between unlike air masses. There are three main types of fronts: cold fronts, where cold air overtakes warm air; warm fronts, where warm air overtakes cold air; and occluded fronts, where a warm air mass is overtaken by two cooler air masses.
This document provides an overview of weather and climate concepts. It discusses how weather is caused by differences in temperature and air pressure between locations. It also describes common weather phenomena and how weather is forecasted using various instruments and models. The document outlines different climate zones and variables that influence climate. It explains phenomena like El Niño and hurricanes and how climate change is impacting environments and societies.
1. The document discusses the impacts of global climate change on human health. It summarizes the findings of the IPCC working groups on observed and projected impacts of climate change through different pathways.
2. Key observed impacts include rising sea levels, changes in precipitation patterns, and effects on ecosystems. Projected health impacts include increased deaths from heat waves, changing disease vectors, and threats to food security.
3. The document outlines the natural and human causes of climate change and examines the IPCC emissions scenarios for projecting future impacts. Understanding climate change drivers and impacts is important for developing response strategies to protect human health.
Climate data can provide a great deal of information about the atmospheric environment that impacts almost all aspects of human endeavour. This module explains the importance of climate data, its storage, security, applications and other aspects, in a nutshell.
This document discusses weather forecasting and understanding weather maps. It explains that weather maps show isobars which indicate wind patterns around high and low pressure systems. Closer isobars mean stronger winds. It describes features of high and low pressure systems including wind direction. Cold fronts are shown where cold air pushes warm air upwards, potentially causing rain. Mechanisms that can trigger rain include fronts, low pressure systems, hills and turbulence. Clouds alone do not guarantee rain as clouds need sufficient moisture and lifting of air to produce meaningful rainfall.
This document discusses basic concepts about weather and climate. It defines weather as the current atmospheric conditions in a place, while climate refers to typical weather patterns over a longer period of 30 years. It describes various elements that affect weather and climate, such as temperature, precipitation, atmospheric pressure, winds, and ocean currents. It provides examples of how these elements are measured and influenced by factors like latitude, altitude, and distance from the sea.
The document discusses weather maps and how they are used to predict weather conditions. It provides information on several key topics:
- The atmosphere helps regulate Earth's temperature and creates weather through the movement of air masses. Weather maps show current conditions.
- Weather is influenced by properties like temperature, humidity and pressure. Maps depict systems like cold fronts, warm fronts and stationary fronts to understand weather changes.
- High and low pressure areas circulate clockwise and counterclockwise respectively, affecting wind patterns and whether conditions will be clear or stormy. Weather maps are interpreted to forecast upcoming weather.
1. The document discusses key concepts about Earth's atmosphere including how solar radiation drives global climate and local weather patterns.
2. It explains different climate types based on factors like latitude, proximity to bodies of water, and elevation. Humid climates receive more precipitation than potential evapotranspiration while arid climates experience the opposite.
3. Atmospheric circulation patterns like global wind belts and ocean currents play an important role in moderating Earth's climate by transporting heat energy from the tropics to poles and distributing it around the globe over long time periods.
1. The document discusses weather elements such as temperature, precipitation, wind speed, and cloud cover. It also describes how these elements are measured using instruments like a thermometer, rain gauge, and anemometer.
2. Common types of clouds are described as cirrus, cumulonimbus, cumulus, and stratus. The Stevenson screen, used to shelter instruments, is also characterized.
3. The difference between weather and climate is explained as weather referring to short term atmospheric conditions while climate describes average conditions over a long period.
The document discusses atmospheric stability and its relationship to moisture and weather. It defines stable, unstable, and conditionally unstable atmospheres based on environmental lapse rates. Stability impacts cloud formation and precipitation - unstable air leads to tall clouds and heavy rain while stable air suppresses vertical air movement and yields light precipitation. Daily changes in temperature and moisture content can increase or decrease atmospheric stability.
Weather forecasting is important for agriculture as it allows farmers to plan for and adjust to upcoming weather conditions. There are different types of forecasts including nowcasting (up to 1 day), short range (1-3 days), medium range (3-10 days), and long range (>10 days). Accurate forecasts can help minimize losses from adverse weather and optimize input use through timely adjustments. Forecasting methods include synoptic analysis of surface and upper air charts, statistical analysis of historical weather data, and numerical weather prediction using physics-based models. The reliability of forecasts depends on factors like weather data collection and dissemination systems, forecaster experience, and forecasting technology.
This document discusses condensation and the formation of fog and clouds. It begins by defining condensation as the process where a gas transforms into a liquid due to changes in pressure and temperature. It then discusses the necessary and sufficient conditions for condensation to occur, including cooling air to below its dew point until saturated and the presence of condensation nuclei. The document proceeds to describe different types of fog like radiation fog, advection fog, and freezing fog that form through various cooling mechanisms. It also covers cloud condensation nuclei and the classification system used to identify different types of clouds.
Fronts are boundaries between two air masses of differing characteristics. There are four main types of fronts: cold fronts, warm fronts, occluded fronts, and stationary fronts. Cold fronts are steep boundaries where cold air overrides warm air, bringing precipitation. Warm fronts are more gradual, with light, continuous precipitation as warm air rises over cold air. Occluded fronts occur when a cold front catches up to a warm front. Stationary fronts have little or no movement as the air masses are parallel.
Structure and Composition of the Atmospherebeaudry2011
The atmosphere is composed of gases, water droplets, and particles surrounding Earth. It has four main layers - the troposphere, stratosphere, mesosphere, and thermosphere - each decreasing or increasing in temperature with altitude. The troposphere is where weather occurs, extending 8-16km high. Above is the stratosphere where temperatures increase with little weather, then the mesosphere where temperatures decrease again up to 80km. The thermosphere is the outermost layer with increasing temperatures from 80km high. The atmosphere composition consists primarily of nitrogen, oxygen, argon, and trace gases. Water vapor is the most abundant variable gas.
This document discusses remote sensing and meteorology. It defines remote sensing as obtaining information about physical objects through non-contact sensors. Meteorology is the study of atmospheric phenomena like weather. Meteorological satellites and weather radars are important tools for monitoring weather. Satellites provide global coverage of cloud patterns and weather systems from space. They capture visible, infrared, and water vapor images to study cloud formations, temperatures, and moisture in the atmosphere. Radar emits microwaves that bounce off water droplets in clouds to measure precipitation and cloud locations. Satellite weather monitoring improves forecasts, especially over oceans with sparse weather station data.
Cyclones and western disturbances By Lohit Sainilohitsaini
Cyclones are intense low pressure weather systems characterized by strong circulating winds. They are classified as either extra-tropical or tropical cyclones. Tropical cyclones form over warm tropical waters and include hurricanes and typhoons. They develop through several stages from a tropical disturbance to a mature storm. Formation requires warm ocean waters, moisture, coriolis force, and low wind shear. Western disturbances originate in the Mediterranean and bring winter precipitation to South Asia when moisture is shed over the Himalayas. They are important for rabi crop growth but can also cause flooding.
Weather forecasting involves collecting data from weather stations, analyzing trends, and predicting future conditions for a given location. Data on temperature, pressure, wind, humidity and more is recorded, transmitted to analysis centers, and plotted on maps and charts. Forecasters use tools like radiosondes, radar, and weather satellites to monitor cloud and storm activity. Forecasts are categorized as short range up to 48 hours, medium range from 3 days to 3 weeks, or long range from 2 weeks to a season. Short range forecasts rely on current conditions while medium and long range try to predict average trends.
This document provides an introduction to climatology, including definitions of key terms and branches of the field. It discusses how climatology studies the atmosphere and spatial patterns of climate. Climatology is related to both meteorology, which deals with day-to-day weather, and geography, which studies spatial climate distributions. The document also outlines the major layers of the atmosphere and characteristics of atmospheric gases like carbon dioxide and ozone.
The document discusses air masses and fronts. It defines air masses as large bodies of air with uniform properties that form over land or water surfaces. There are four main types of air masses classified by their region of formation: maritime/continental and polar/tropical. Fronts are boundaries between unlike air masses. There are three main types of fronts: cold fronts, where cold air overtakes warm air; warm fronts, where warm air overtakes cold air; and occluded fronts, where a warm air mass is overtaken by two cooler air masses.
This document provides an overview of weather and climate concepts. It discusses how weather is caused by differences in temperature and air pressure between locations. It also describes common weather phenomena and how weather is forecasted using various instruments and models. The document outlines different climate zones and variables that influence climate. It explains phenomena like El Niño and hurricanes and how climate change is impacting environments and societies.
1. The document discusses the impacts of global climate change on human health. It summarizes the findings of the IPCC working groups on observed and projected impacts of climate change through different pathways.
2. Key observed impacts include rising sea levels, changes in precipitation patterns, and effects on ecosystems. Projected health impacts include increased deaths from heat waves, changing disease vectors, and threats to food security.
3. The document outlines the natural and human causes of climate change and examines the IPCC emissions scenarios for projecting future impacts. Understanding climate change drivers and impacts is important for developing response strategies to protect human health.
Climate data can provide a great deal of information about the atmospheric environment that impacts almost all aspects of human endeavour. This module explains the importance of climate data, its storage, security, applications and other aspects, in a nutshell.
Drought refers to a prolonged period of abnormally low rainfall, leading to a shortage of water. A drought can last for several months or years. Sometimes, droughts are declared for a full district for a few years.
It can have a substantial impact on the ecosystem and agriculture of the affected region and harm to the local life and economy. This module highlights the basics of climatic drought.
Adaptation to global change must include prudent management of groundwater as a renewable, but slow-feedback resource in most cases. Groundwater storage is already over-tapped in many regions, yet available subsurface storage may be a key to meeting the combined demands of agriculture, industry, municipal and domestic water supply, and ecosystems during times of shortage.
The Earth’s climate is changing. Temperatures are rising, snow and rainfall patterns are shifting, and more extreme climate events—like heavy rainstorms and record-high temperatures, are already taking place. One important way to track and communicate the causes and effects of climate change is
through the use of indicators. An indicator represents the state or trend of certain environmental or societal conditions over a given area and a specified period of time. This lesson highlights all those indicators for a better understanding of climate change.
Meteorological observations are made for a variety of reasons. They are used for the real-time preparation of weather charts and maps, for weather forecasts and severe weather warnings, for the study of climate, and for local weather-dependent operations. This module highlights all related details.
To aid in understanding many complex interactions, scientists often build mathematical models that represent simple climate systems. This module highlights the fundamentals of climate models.
Map is a drawn or printed representation of the physical features of the Earth.
It is the best tool to show, understand and analyse the features of an area. Cartography is the art and science of making maps. This module highlights many information on maps, types and their uses.
This document discusses research methodology and provides an overview of key concepts in conducting research. It describes research as a systematic, rigorous, and empirical process of inquiry aimed at discovering and interpreting new facts or reaching new conclusions. The document outlines various types of research based on their application, objectives, and inquiry mode, and discusses important characteristics of research such as being controlled, valid, and verifiable. It also presents various frameworks for classifying research purposes and types.
The climate of a region is ultimately determined by the radiation energy of the sun, and its distribution and temporal fluctuations. The long-term state of the atmosphere is a function of a variety of interacting elements. They are: Solar radiation, Air masses, Pressure systems (and cyclone belts),Ocean Currents, and topography.
The term precipitation is also used to refer all forms of falling moisture viz., rainfall, snowfall, sleet, hail etc. Rainfall occurs in the form of a pattern. Atmospheric Precipitation is a wonderful process for the whole globe to use. This module explains it in general.
Ozone exists in two layers of the atmosphere - the troposphere and stratosphere. Stratospheric ozone protects life on Earth by absorbing harmful UV radiation from the sun. Chlorofluorocarbons and other ozone depleting substances released chemicals that destroyed stratospheric ozone, causing thinning of the ozone layer. Thinning of the ozone layer allows more UV radiation to reach the Earth's surface, increasing health risks like skin cancer as well as risks to plants, animals, and ecosystems. International agreements like the Montreal Protocol aimed to phase out ozone depleting substances and allow recovery of the ozone layer.
The document discusses immuno-oncology and the relationship between cancer and the immune system. It provides an overview of topics that will be covered in an upcoming webinar, including advances in immuno-oncology for different cancer types and combination immunotherapy approaches. The document then reviews key topics in more depth, including how immuno-oncology focuses on improving the body's immune response against cancer and recent immunotherapy approvals. It also discusses how cancer can evade the immune system and strategies for cancer immunotherapy, such as manipulating co-stimulatory signals, enhancing antigen presenting cells, and using cytokines, monoclonal antibodies, and cancer vaccines.
This document discusses the procedures and tools used in weather forecasting. It describes how weather data is collected from over 9,500 observation stations and 7,400 ships worldwide and transmitted to analysis centers. Forecasts are made using synoptic charts, computer modeling, and satellite imagery from geosynchronous and low-Earth orbiting satellites. Forecasts can be short-range up to 48 hours, medium-range from 3 days to 3 weeks, or long-range from 2 weeks to a season. The goal of weather forecasting is to continue advancing techniques to better predict high-impact weather events.
Wx forcasting and Reporting for mariners.pdfCaptMadanKumar
The World Meteorological Organization (WMO) is a specialized UN agency responsible for international cooperation around weather, climate, hydrology and related geophysical sciences. It was established in 1950 and has 191 member states. The WMO facilitates the global exchange of weather and climate data, contributes to policy around these issues, and promotes international cooperation between national meteorological services.
Atmospheric Dispersion in Nuclear Power Plant SitingHussain Majid
This document discusses atmospheric dispersion modeling for nuclear power plant siting. Meteorological data collection is important for modeling radioactive releases from plants during normal operation and accidents. Stability classes are determined from factors like temperature lapse rate, wind fluctuations, insolation, and cloud cover to characterize turbulence levels affecting dispersion. Both simple and complex terrain features must be considered when collecting and interpreting meteorological data used in dispersion calculations.
The document discusses different types of stations and networks used for climate observation in the US. It describes 4 major networks operated by NOAA: 1) local climatological data stations that define climate for 275 cities and towns, 2) the co-op network that establishes baseline climate using 5,200 temperature and 7,400 precipitation stations, 3) the hourly precipitation data network of 3,000 stations for hydrologic records, and 4) the historical climate network of 1,215 stations for documenting climate variations.
The document discusses different types of stations and networks used for climate observation in the US. It describes 4 major networks operated by NOAA: 1) local climatological data stations that define climate for 275 cities and towns, 2) the co-op network that establishes baseline climate using 5,200 temperature and 7,400 precipitation stations, 3) the hourly precipitation data network of 3,000 stations for hydrologic records, and 4) the historical climate network of 1,215 stations for documenting climate variations. It also outlines standard procedures and equipment for measuring temperature, humidity, wind, and radiation parameters.
This document discusses using geostationary satellites to predict aviation weather hazards like downbursts and fog. It describes how satellite measurements can be used to calculate indices like the Microburst Wind Potential Index (MWPI) to forecast downburst wind speeds up to 3 hours in advance. Case studies of downbursts in Southern California in 2014 and fog in Salt Lake City in 2015 are presented, showing how satellite data matched observations. The conclusions emphasize that MWPI has conditional skill in forecasting thunderstorm winds and that fog can be detected using infrared channel brightness temperature differences from GOES satellites.
CEPSI 2014 Full paper JKT Alstom WIND TURBINE OPERATION IN TYPHOON CONDITIONSJosef Tadich
- Typhoons are a challenging design condition for wind turbines in the Asia-Pacific region. They can produce extreme 10-minute wind speeds over 45 m/s.
- Typhoons are characterized as tropical cyclones that develop over warm water and rotate counter-clockwise in the northern hemisphere. The most destructive winds occur at the eyewall.
- Extreme wind speeds for turbine design are estimated using statistical analysis of long-term wind data and exceedance rates, with a typical standard being the 50-year return period wind speed.
Weather balloons are high-altitude meteorological balloons particularly used for carrying scientific payloads into the upper atmosphere. These data are obtained by using an instrument called as radiosonde which is attached to the helium filled weather balloon to measure the meteorological data as it ascends up into the atmosphere. For more than 100 years, weather balloons have given valuable information for climate and meteorological research. In this paper, the radiosonde module is designed with negligible risk of failure and cost effectiveness. The instruments to be fixed along with the weather balloon are logging camera, temperature sensor, pressure sensor, humidity sensor, global positioning system (GPS) module and a power source. This module is used to measure and log the basic weather parameters such as pressure, temperature, humidity and this also captures the picture of a particular locality with the help of a microcontroller. This proposed work is useful for observing high altitude weather data which is essential for predicting natural disasters. Further more, it is helpful to analyze the climatological and weather details of a particular region it also plays an important role in estimating agricultural models.
TRACKING ANALYSIS OF HURRICANE GONZALO USING AIRBORNE MICROWAVE RADIOMETERjmicro
There is a huge consideration in the use of microwave airborne radiometry for remote sensing instead of satellite, the important role of airborne way is how to provide high accuracy real time data. The airborne hurricane tracking is an important method compared with the space borne method, which is developed by NASA Marshall Space Flight center to provide high resolution measurements. By flying special aircraft equipment using synthetic thinned array radiometry technology and included all critical measurements such as hurricane eye location, speed of wind and the pressure. This paper describes the data analysis of best track positions for Hurricane Gonzalo based on the date collected by airborne microwave radiometry. Significant analysis comes from comparing the airborne data with the surface observations from ship reports. The vast majority is to estimate peak intensity and minimum central pressure of Gonzalo from 12 to 19 October 2014, based on blend of SFMR flight-level winds and pressure retrievals from observing brightness temperatures. SFMR: Stepped-Frequency Microwave Radiometer is a highly developed tool developed by the Langley Research Center that is designed to measure the wind speed at the ocean’s surface, and the rain fall rates within the storm accurately and continuously. The work also addresses the realistic details of the locations and the valuable information about the pressure and wind speed, which is very critical to predict the growth and movement to get the idea for future monitoring of the hurricane disasters. Also presents a conceptual of step frequency microwave radiometer in airborne side. The objective of this research is tracking analysis techniques based on comparing the satellite, ship and airborne reports to get higher accuracy. The system operates at four spaced frequencies in the range between 4 GHz and 7 GHz provides wide measurements between ± 45 incidence angle. Gonzalo 2014 is an example; the best results of retrieved wind speed, locations and pressure are presented. There are several national projects have been developed for earth observation, such as fire, hurricane and border surveillance. In this work, the efficient high resolution techniques of C-band, four-frequency, the work also addresses a valuable information comes from the airborne system and the prediction way of the growth and movement of hurricanes. In passive microwave remote sensing from space at C band has the penetrating advantages of atmosphere. Airborne system is able to work in full Polari-metric in four bands, C, X, S, L and P-band, which cover the wavelengths from 3 to 85 cm. The modes of measurement contain single channel operation wavelength and polarization.
Meteorological instruments are used to measure various atmospheric conditions. Key instruments include thermometers for temperature (degrees Celsius/Fahrenheit), barometers for pressure (hPa, mb), anemometers for wind speed (m/s, km/h), rain gauges for precipitation (mm), and hygrometers for humidity (percent relative humidity). Other instruments such as ceilometers, disdrometers, and weather balloons equipped with radiosondes are used to profile clouds, precipitation, and wind conditions at varying altitudes above ground level. Measurement units vary depending on the parameter and instrument but generally relate to the International System of Units.
Meteorological instruments are used to measure various atmospheric conditions. Key instruments include thermometers for temperature (degrees Celsius/Fahrenheit), barometers for pressure (hPa, mb), anemometers for wind speed (m/s, km/h), rain gauges for precipitation (mm), and hygrometers for humidity (percent relative humidity). Other instruments such as ceilometers, disdrometers, and weather balloons equipped with radiosondes are used to profile clouds, precipitation, and wind conditions at varying altitudes above ground level. Measurement units vary depending on the parameter and instrument but generally relate to the International System of Units.
Meteorological instruments are used to measure various atmospheric conditions. Key instruments include thermometers for temperature (degrees Celsius/Fahrenheit), barometers for pressure (hPa, mb), anemometers for wind speed (m/s, km/h), rain gauges for precipitation (mm), and hygrometers for humidity (percent relative humidity). Other instruments such as ceilometers, disdrometers, and weather balloons equipped with radiosondes are used to observe clouds, raindrops, and wind/temperature/pressure profiles at different altitudes. Measurements from these instruments provide critical data for weather forecasts and climate studies.
This document discusses meteorological instrumentation used to measure various weather conditions. It begins with a brief history of early weather measurement devices like the rain gauge, anemometer, and hygrometer developed in the 15th century. It then describes common instruments used today like the thermometer, barometer, anemometer, and hygrometer. The document also covers remote sensing tools like weather radars and satellites. It provides details on various types of specific instruments and concludes with information about weather stations and surface weather observations.
weather forecasting, types, advantages, role, drought climatology, weather forecasting tools, use in agriculture, role in agriculture, nowcasting, medium, long range,Indian meteorological department
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Chemical analysis data of water samples can not be used directly for understanding. They are to be used for various calculations in order to determine the quality parameters that have a lot of significances. A. Balasubramanian and D. Nagaraju, of the Department of Studies in Earth Science, Centre for Advanced Studies, University of Mysore, Mysore-570006, Karnataka, India have recently brought out a software and its application manual as a good book for reference and execution. The Name of the software is WATCHIT meaning Water Chemistry Interpretation Techniques. This software computes more than 100 parameters pertaining to water quality interpretations. The software follows its own method of approach to determine the required results. Systems International Units are used. Limited input parameters are required. This is suitable for all scientific research, government water quality data interpretations and for understanding the quality of water before using it.
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2. 2
Weather monitoring Stations :
Weather monitoring Stations should be located
to give representative climatic characteristics
that are consistent with all types of terrain, such
as plains, mountains, plateaus, coasts and
islands, and surface cover such as forests, urban
areas, farming areas and deserts within the area
concerned.
3. 3
Station density should be dependent upon the
purposes for making the observations and the
uses of the data.
The density and distribution of climatological
stations to be established in a land network
within a given area depend on the
meteorological elements to be observed, the
topography and land use in the area, and the
requirements for information about the specific
climatic elements concerned.
4. 4
The rate of variation of climatic elements across
an area will differ from element to element.
CLIMATIC ELEMENTS:
Surface and subsurface elements:
A principal climatological station usually
provides a broader range of observations of
weather, wind, cloud characteristics, humidity,
temperature, atmospheric pressure,
precipitation, snow cover, sunshine and solar
radiation.
5. 5
In order to define the climatology of
precipitation, wind, or any other specific
element, it is sometimes necessary to operate a
station to observe one or a subset of these
elements, especially where the topography is
varied. It is desirable to have a network of these
stations in each country, representing key
climate zones and areas of vulnerability.
6. 6
The observations from these networks and
stations are required for the timely preparation
of weather and climate analyses, forecasts,
warnings, climate services, and research.
In addition to surface elements, subsurface
elements such as soil temperature and moisture
are particularly important for application to
agriculture, forestry, land-use planning and
land-use management.
7. 7
Other elements that should be measured to
characterize the physical environment for
agricultural applications include evaporation
from soil and water surfaces, sunshine, short-
and long-wave radiation, plant transpiration,
runoff and water table, and weather
observations (especially hail, lightning, dew and
fog).
8. 8
Upper-air elements:
Upper-air observations are an integral
component of the Global Observing System.
Climatic Elements measured by remote sensing.
INSTRUMENTATION:
Climatological stations that are part of a
national network should be equipped with
standard approved instruments.
9. 9
Calibration of instruments:
It is of paramount importance, for determining
the spatial and temporal variations of climate,
that the relative accuracy of measurement of
individual sensors in use in a network at one
time be measured and periodically checked, and
similarly, that the performance of replacement
sensors and systems can be related to that of
those replaced.
10. 10
The Siting of Climatological Stations:
The representativeness and homogeneity of
climatological records are closely related to the
location of the observing site. A station sited on
or near a steep slope, ridge, cliff, hollow,
building, wall or other obstruction is likely to
provide data that are more representative of the
site alone and not of a wider area.
11. 11
A station that is or will be affected by the
growth of vegetation, including even limited
tree growth near the sensor, growth of tall crops
or woodland nearby, erection of buildings on
adjacent land, or increases (or decreases) in
road or air traffic (including those due to
changes in the use of runways or taxiways) will
provide neither broadly representative nor
homogeneous data.
12. 12
A climatological observing station should be
sited at a location that permits the correct
exposure of the instrumentation and allows for
the widest possible view of the sky and
surrounding country if visual data are required.
Prevention of unauthorized entry is a very
important consideration, and may require
enclosure by a fence. Security is needed.
13. 13
1. Synoptic stations reports are complied every
three hours in an international numerical code
by staff of the Fiji Meteorological Service. The
weather stations are vastly networked, and are
distributed over the main islands of the Fiji
group as well as, other remote islands.
2. Climatological Stations provide more
detailed information on elements like,
temperatures (air/soil), humidity, rainfall,
radiation, sunshine hour and wind.
14. 14
3. The Automatic Weather Station (AWS) is
defined a station which automatically transmits
or records observations obtained by measuring
instruments. The data derived from AWS
include the dates, time of observation, station
indicators, wind speed, direction, temperature,
relative humidity, MSL pressure and rainfall
data.
15. 15
4. Rainfall Stations provide rainfall data that
are measured every day at 9.00am. These
stations are manned by workers of either
corporate organizations, or other government
departments and are normally called voluntary
observers.
5. Radar observations : Weather and wind-
profiling radars are proving to be extremely
valuable in providing data of high-resolution in
16. 16
both space and time, especially in the lower
layers of the atmosphere.
Weather radars are used extensively as part of
national, and increasingly of regional networks,
mainly for short-range forecasting of severe
weather phenomena.
17. 17
Weather radars are particularly useful for
estimation of rainfall amounts and, when
Doppler capable, wind measurements. Wind
profiler radars are especially useful in making
observations between balloon-borne soundings,
and have great potential as a part of integrated
observing networks.
18. 18
6. Observing stations at sea :
Over the oceans, the GOS relies on ships,
moored and drifting buoys, and stationary
platforms.
Observations made by about 7 000 ships
recruited under the WMO Voluntary Observing
Ship Programme, collect the same variables as
land stations with the important additions of sea
19. 19
surface temperature and wave height and
period.
The operational drifting buoy programme
comprises about 900 drifting buoys providing
12 000 sea surface temperature and surface air
pressure reports per day.
20. 20
7. Observations from aircraft :
Over 3 000 aircraft provide reports of pressure,
winds, and temperature during flight. The
Aircraft Meteorological Data Relay (AMDAR)
system makes high-quality observations of
winds and temperatures at cruising level, as
well as at selected levels in ascent and descent.
21. 21
The amount of data from aircraft has increased
dramatically in recent years to an estimated 300
000 reports per day.
8. Observations from satellites
The environmental and meteorological space-
based Global Observing System includes
constellations of operational Geostationary and
Low Earth Orbit (near-polar-orbiting)
observation satellites.
22. 22
Meteorological observations of Variables
- temperature (at various heights above the
ground or sea surface),
- atmospheric pressure or air pressure
- humidity or relative humidity, dew point
temperature
- wind speed and direction
- precipitation (amount and duration), snow
cover
23. 23
- solar radiation (short wavelength, UV-a, UV-
b, sunshine duration),
- horizontal visibility
- evaporation,
- soil moisture content, soil temperature
(various depths),
- upper air pressure, temperature, humidity
- upper air wind ,
- weather state (present weather, past weather) ,
24. 24
- clouds (type, sort and height) and degree of
coverage ,
- ozone
- composition of the atmosphere
- sea water temperature;
- waves and swell (height, direction, period);
- lightning.
25. 25
The observations are generally “ground based”,
i.e. that they are measured on or at the surface
level of the ground or sea.
A number of meteorological variables
(temperature, relative humidity, wind, pressure,
etc.) are also measured at greater altitudes:
- by releasing balloons with radio sondes (up to
altitudes of more than 15 km);
26. 26
- at various levels on the Cabauw measuring
mast (up to a height of 200 m).
Meteorological observations are carried out in
principle as a continuous process, in which the
frequency of observation can vary from a
fraction of a second up to periods of 24 hours.
Observations are made using instruments,
manually, visually or by ear.
27. 27
A value is not directly determined for a number
of meteorological variables, but is rather
derived from other variables that have been
directly observed or measured.
Examples are evaporation (calculated from
temperature and global solar radiation), dew
point temperature (calculated from temperature
and relative humidity) and sunshine duration
(calculated from global shortwave radiation).
28. 28
Important weather information is acquired
using remote sensing techniques (e.g. radar
systems for detecting showers), satellite
observations, observations made on board ships,
measuring buoys at sea and observations made
from aircraft (AMDARs).
29. 29
Type of observing station:
The observational network shall include
comprise the following types of
meteorological stations:
a) Manned weather station: visual and
instrumental observations;
b) Automatic weather station (AWS):
exclusively instrumental observations;
30. 30
c) Wind measuring mast: instrumental
observations of wind direction and speed only;
d) measuring mast: instrumental observations at
heights from 20 m to 200 m;
e) precipitation stations: (manual) observations
of precipitation amount and snow cover;
f) lightning detection masts: observations of
lightning discharges.
31. 31
Times of observations & Regularity:
The distinguishing feature of a meteorological
station is that the variables concerned are
measured or are observed there regularly in
order to provide a (real-time) picture of the
actual weather situation in that region.
32. 32
The observational data collected from a
weather station is to be validated (using pre-
determined objective procedures) and
systematically archived for later analysis of
specific events and for climatological purposes.
A selection of the data is also used for the
analysis and verification of operational weather
models.
33. 33
Conditions relating to the layout of the
measurement site of a weather station:
A measurement site is surrounded by a fence to
prevent unauthorized access. The measuring
instruments are positioned on the site in such a
way as not to interfere with each other. The
neighbourhood of the measurement site must be
free of objects that could affect the
measurements.
34. 34
Spatial distribution of the measuring stations
and the representativeness of the
observations
Diagram of an automatic weather station
Observations at ordinary climatological and
precipitation stations should be made at least
once (and preferably twice) each day at fixed
hours that remain unchanged throughout the
year.
35. 35
At principal climatological stations,
observations must be made at least three times
daily in addition to an hourly tabulation from
autographic records, but non-autographic
observations are usually taken hourly.
If changes are made to the times of observations
across a network, simultaneous observations
should be carried out at a basic network of
representative stations for a period covering the
36. 36
major climatic seasons in the area at the old and
new times of observation.
Logging and reporting of observations
On-site quality control
Report monitoring at collection centres
Station documentation and metadata
Basic station metadata should include station
name and station index number (or numbers);
geographical coordinates;
37. 37
elevation above mean sea level;
administrator or owner;
types of soil, physical constants and profile of
soil;
types of vegetation and condition;
local topography description;
description of surrounding land use;
photographs and diagrams of the
instrumentation,
site and surrounding area;
38. 38
type of AWS, manufacturer, model and serial
number;
observing programme of the station (elements
measured, reference time, times at which
observations and measurements are made and
reported, and the datum level to which
atmospheric pressure data of the station refer);
and contact information, such as name and
mailing address, electronic mail address, and
telephone numbers.
39. 39
Instrument metadata should include sensor
type, manufacturer, model and serial number;
principle of operation; method of measurement
and observation; type of detection system;
performance characteristics; unit of
measurement and measuring range; resolution,
accuracy (uncertainty), time constant, time
resolution and output averaging time; siting and
exposure (location, shielding and height above
or below ground); date of installation; data
40. 40
acquisition (sampling interval and averaging
interval and type); correction procedures;
calibration data and time of calibration;
preventive and corrective maintenance
(recommended and scheduled maintenance and
calibration procedures, including frequency, and
a description of procedures); and results of
comparison with travelling standards.
41. 41
The Design of Climatological Networks
A network of stations is several stations of the
same type (such as a set of precipitation
stations, radiation measuring stations or
climatological stations), which are administered
as a group.
Each network should be optimized to provide
the data and perform as required at an
acceptable cost.
42. 42
It has been common practice to assume that at
least ten years of daily observations are
necessary to produce the relevant base statistical
parameters for most elements, and at least thirty
years for precipitation.
The identification of redundant stations
allows network managers to explore options for
optimizing the network, for example, by
eliminating the redundant stations to reduce
costs or by using the resources to establish
43. 43
stations at locations where observations are
needed for a more effective realization of the
network objectives.
A sparse network is sufficient for the study of
surface pressure, a fairly dense network for the
study of maximum and minimum temperature,
and very dense networks for examining the
climatology of precipitation, wind, frost and
fog, especially in regions of significant
topography.
44. 44
The measurement network comprises of
various equipment. The measurement network
consists of a substantial number of weather
stations on land and in the Sea. Observations
and (automatic) measurements of
meteorological variables should be carried out
at these stations.
The observing stations and the instrumentation
used meet the requirements set by the World
Meteorological Organization (WMO):
45. 45
There should be a team of station inspectors
monitor the quality of the observations by
regularly checking the measuring equipment
and the environment at the measurement site.
The observational data is carefully verified,
validated, stored and processed for a large
number of applications.