A study on the lower tropospheric thermal inversion over the arabian sea using radiosonde and iasi data
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A study on the lower tropospheric thermal inversion over the arabian sea using radiosonde and iasi data +91-9994232214,7806844441, ieeeprojectchennai@gmail.com, www.projectsieee.com, www.ieee-projects-chennai.com IEEE PROJECTS 2016-2017 ----------------------------------- Contact:+91-9994232214,+91-7806844441 Email: ieeeprojectchennai@gmail.com
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Here are the key steps to solve these atmospheric pressure and boiling point calculation problems:
1) H = 11(760 - 721) = 429 m
2) H = 4,070 m, P = 760 - (H/11) = 760 - (4,070/11) = 390 mm Hg
3) H = 2,376 m, B.P. = 100 - (760 - P)/27 = 100 - (760 - (760 - (H/11)))/27 = 100 - (760 - (760 - (2,376/11)))/27 = 95 °C
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The plastic bottle was sealed at an altitude of 14,000 feet and crushed when it reached 9,000 feet, indicating that atmospheric pressure is higher at lower altitudes and lower at higher altitudes. Atmospheric pressure decreases with increasing altitude because there is less air and oxygen above ground level, so places at sea level have higher pressure than places at higher elevations.
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Here are the key steps to solve these atmospheric pressure and boiling point calculation problems:
1) H = 11(760 - 721) = 429 m
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3) H = 2,376 m, B.P. = 100 - (760 - P)/27 = 100 - (760 - (760 - (H/11)))/27 = 100 - (760 - (760 - (2,376/11)))/27 = 95 °C
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Plume types
There are several types of plumes classified based on the environmental lapse rate (ELR) and adiabatic lapse rate (ALR):
1. Coning plume occurs under sub-adiabatic conditions (ELR < ALR) or with high winds, taking on a cone-like structure with limited vertical mixing.
2. Fanning plume occurs under inversion conditions (negative ELR), causing the plume to disperse horizontally rather than rising.
3. Looping plume occurs in super adiabatic environments (ELR > ALR), leading to an unstable atmosphere and the plume taking on a wavy, looping form.
4. Neut
period 4 group 1
The document discusses key weather factors such as air temperature, wind, and humidity. It explains that air temperature is a measure of molecular motion, with higher temperatures indicating more rapid movement. It also describes how wind is caused by differences in air pressure from warm and cool air masses, and can be measured with an anemometer. Finally, it defines relative humidity as the amount of water vapor in the air compared to the maximum possible at a given temperature, with dew point referring to the temperature when air reaches saturation.
Temperature lapse rates
The environmental lapse rate - temperature drop with altitude - in the troposphere; that is the temperature of the environment at different altitudes.
Lapse rate and stability conditions
- Lapse rate is the decrease of air temperature with increasing elevation in the troposphere. It is influenced by factors like dry adiabatic lapse rate (DALR), wet adiabatic lapse rate (WALR), and environmental lapse rate (ELR).
- The stability of the atmosphere depends on the relationship between the ELR and the DALR/WALR. If ELR > DALR, the atmosphere is unstable. If ELR < DALR, the atmosphere is stable. If ELR = DALR, the atmosphere is neutral.
- Radiosondes are instruments used to measure atmospheric variables like temperature, pressure, humidity at different
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1) A planet's atmosphere is determined by its gravity - large planets with strong gravity can hold thicker atmospheres than low-mass planets with weak gravity.
2) Atmospheric pressure depends on the thickness of the atmosphere, which is influenced by a planet's gravity. Stronger gravity holds more gas and increases atmospheric pressure.
3) On Earth, atmospheric pressure is measured using barometers. The mercury barometer measures air pressure through the height mercury is pushed up in a glass tube by atmospheric pressure. The aneroid barometer uses changes in the pressure on an evacuated metal cell to measure air pressure without toxic mercury.
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The document discusses temperature inversions and wind velocity profiles. It describes three main types of temperature inversions - subsidence inversions, radiation inversions, and a combination of the two. Subsidence inversions occur high above emission sources under high pressure systems and can persist for several days. Radiation inversions occur near the surface at night due to cooling of the ground. The document also discusses wind velocity profiles and how wind speed varies with height according to Deacon's power law under different stability conditions. Several examples are provided to calculate wind speed at different heights using this power law equation.
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- Standing waves, also called lee waves or mountain waves, form when stable air flows over hills or mountains and remains virtually stationary. They can cause turbulence and downdrafts on the lee side.
- Lenticular clouds indicate the presence of standing waves caused by moist air rising in the waves. Severe turbulence exists in the rotor zone of standing waves.
Eli video solution 1
An inversion occurs when warm, less dense air moves over cold, dense air causing the temperature to increase with altitude instead of the normal decrease. This creates an absolutely stable environment where the environmental lapse rate is less than the moist adiabatic lapse rate, meaning a rising air parcel will continue to cool with altitude rather than warm, becoming denser than the surrounding air. An inversion therefore represents an absolutely stable atmosphere where any rising air will continue to cool after passing through the inversion layer.
Chapter 3a air conditioning process
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Babelene
Meteorology is the scientific study of the atmosphere and weather forecasting. Significant advances occurred in the 18th century with observing networks, and in the 20th century with the development of computers enabling improved weather forecasting. Meteorology studies temperature, pressure, water vapor and how they interact and change over time at various spatial scales from local to global. It is related to other atmospheric sciences and has applications across many fields. Common weather instruments measure rainfall, temperature, pressure, wind speed and direction, sunshine, and humidity.
Pressure to powerpoint
Atmospheric pressure can be measured using a barometer. The first mercury barometer was developed in 1643 by Evangelista Torricelli. Later, an aneroid barometer was invented in 1843 that functions without liquids. In 2004, Cold Energy obtained a patent for a device that generates electricity by exploiting differences in atmospheric pressure between geographic locations using a pressurized air pipeline. This concept could generate enough renewable energy to power 250,000 homes.
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1) A new study finds that warmer temperatures in the Atlantic Ocean are linked to wetter summers in Northern Europe.
2) The study examined periods from 1931-1960, 1961-1990, and 1990-present where the Atlantic Ocean experienced warm and cool cycles roughly every few decades.
3) When the Atlantic is warmer, it favors milder springs, summers, and autumns for England and Europe, along with more rainfall than usual for Northern and Central Europe.
Atmospheric stability and plume behaviour
This document discusses various atmospheric factors that influence the dispersion of air pollutants, including:
1. Dilution effect, dispersion, gravitational settling, absorption, and rainout naturally reduce pollutant concentrations.
2. Atmospheric stability is determined by comparing the environmental lapse rate to the adiabatic lapse rate, with stable atmospheres inhibiting dispersion.
3. Other factors like wind, pressure systems, temperature inversions, moisture, and maximum mixing depth also impact pollutant plume behavior and dispersion.
Stability & Instability
This document discusses the factors that determine the stability or instability of the atmosphere. It explains that a stable atmosphere occurs when a rising air parcel cools more rapidly than the surrounding environment, causing it to sink back down. An unstable atmosphere happens when a rising parcel cools more slowly than the environment, allowing it to continue ascending. Specifically, stability depends on how the environmental lapse rate compares to the dry and saturated adiabatic lapse rates of a rising air parcel.
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Severe Tropical Cyclone George affected northern Australia from March 2-16, 2007, becoming one of the strongest storms to make landfall in Port Hedland. Several factors contributed to George's intensification and ability to maintain circulation after landfall, including the location of the Intertropical Convergence Zone during March in the Southern Hemisphere, the presence of a cool phase El Niño Southern Oscillation, and the flat terrain of northwest Australia which allowed the circulation to persist over land longer than expected. Analysis of satellite imagery and atmospheric conditions show that a cool phase ENSO was present in early 2007, supporting tropical cyclone formation near Australia, and that George was able to maintain its circulation for over 24 hours after landfall
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Lecture13 oct23-bb(1)
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Chapt35
The document describes the general structure and circulation of the Earth's atmosphere. It discusses how solar heating creates pressure differences that drive global wind patterns. Specifically, it mentions:
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2) The Hadley cell circulation involves warm air rising in the tropics, flowing poleward and sinking at 30° latitude, returning equatorward at the surface.
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Explanation Tropical Storm
Tropical storms form over warm ocean waters through the process of convection where warm, moist air rises, cools and condenses, releasing heat. For a tropical storm to form, specific conditions are needed - sea surface temperatures above 26°C, a moist atmosphere, location away from the equator, a pre-existing low pressure disturbance, and little wind shear between the surface and upper atmosphere. Tropical storms typically form within bands of latitude between the equator and 30 degrees in each of the world's seven tropical cyclone basins during their respective peak seasons.
Capter 5 Climate of Ethiopia and the Horn GeES 1011.pdf
Upon the completion of this chapter, you will be able to:
Distinguish between weather and climate,
Explain the place to place distribution of temperature and rainfall in Ethiopia,
explain the time to time patterns of temperature and rainfall in Ethiopia,
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5.1 The concept of weather and climate
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Climate is a prolonged(30-35years) atmospheric condition observed in a relatively wider geographic area.
Weather condition likely changed hour to hour, in a daily base or weakly but climate is relatively permanent.
Elements of Weather and Climate
Elements(components) of weather and climate are the following variables
Atmospheric temperature (how cold or hot is the atmosphere)
Precipitation (any kind of moisture falling from the atmosphere to the ground, mostly rainfall)
Air pressure (the weight exerted by the air)
Humidity (the level or proportion of water vapor within the atmosphere)
Sunshine (the duration and intensity of solar heat as well as light)
Wind (horizontal motion of air)
SPACE DYNAMIC
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78239585 orals-met
1. Atmospheric pressure is the pressure exerted by the weight of the earth's atmosphere. It is measured in hectopascals (hPa), with 1 hPa equal to 1 millibar.
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3. Dew point temperature is the temperature at which air becomes saturated with water vapor and fog can form. It is an important measurement for mariners to consider when deciding whether to ventilate cargo holds.
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2) Lapse rates which describe how temperature changes with altitude. Inversions and stable/unstable conditions impact vertical air movement.
3) Maximum mixing depth, the vertical extent of mixing which influences pollutant dispersion and urban air pollution episodes.
Air Pollution and Meteorology
This document discusses how meteorological conditions influence the transport and dispersion of air pollutants. It covers topics such as wind patterns from macro to micro scales; lapse rates and their relationship to atmospheric stability; types of inversions like subsidence and radiation inversions; and the maximum mixing depth which determines the vertical extent of pollutant dispersion. Diagrams are included to illustrate concepts like wind profiles, wind roses, stability conditions, and mixing depths.
Chapter 3
This chapter discusses how meteorological conditions influence the transport and dispersion of air pollutants. It covers key topics such as:
1) Wind patterns from global to micro scales that determine pollutant movement.
2) Lapse rates which describe how temperature changes with altitude. Inversions and stable/unstable conditions impact vertical mixing.
3) Maximum mixing depth, the vertical extent of mixing which affects pollutant dispersion and influences air quality.
Unit 5
This document provides an overview of the Earth's atmosphere and climate. It discusses the different layers of the atmosphere, including the troposphere, stratosphere, mesosphere, thermosphere, and exosphere. It describes properties of air like composition, temperature, atmospheric pressure, and humidity. It explains concepts of weather and climate, factors that influence weather like pressure, temperature, wind, and precipitation. It also outlines the Earth's climate zones of cold, hot, and temperate, and identifies nine climate types based on temperature and precipitation patterns. Climographs are introduced as a way to graphically represent annual temperature and precipitation data to identify a location's climate.
Understanding the Weather Map
This presentation was prepared for an ESL (English as a Second Language) 1st year Science Class.
Images were compiled from various google sites.
Atmospheric circulation-Climatology Chapter
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Cyclones
Cyclones are large revolving storms caused by winds circulating around a low pressure center. They are classified according to location and scale. Tropical cyclones form over warm tropical waters and have organized thunderstorms and surface winds. They go through formative, mature, and decay stages and can last several weeks, powered by heat from ocean evaporation. The Philippines experiences around 20 typhoons annually from July to September, which often cause heavy damage and loss of life.
Factors Affecting the Climate Grade 9 Quarter 3 Week 4
1. The document discusses various factors that affect climate, including latitude, altitude, topography, ocean currents, wind systems, and the Earth's movement.
2. Specific wind systems that influence the Philippines' climate are discussed, such as the northeast and southwest monsoons.
3. Different factors like latitude, altitude, proximity to oceans, and landforms cause areas to experience varying weather patterns and temperatures.
General Circulation of the Atmosphere
Air Circulation models, three model cells, planetary & local wind are shown here with flexible example.
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Eric Nizeyimana's document 2006 from gicumbi to ttc nyamata handball play
Eric Nizeyimana's document 2006 from gicumbi to ttc nyamata handball play
ML Based Model for NIDS MSc Updated Presentation.v2.pptx
ML Based Model for NIDS MSc Updated Presentation.v2.pptx
basic-wireline-operations-course-mahmoud-f-radwan.pdf
basic-wireline-operations-course-mahmoud-f-radwan.pdf
Optimizing Gradle Builds - Gradle DPE Tour Berlin 2024
Optimizing Gradle Builds - Gradle DPE Tour Berlin 2024
BPV-GUI-01-Guide-for-ASME-Review-Teams-(General)-10-10-2023.pdf
BPV-GUI-01-Guide-for-ASME-Review-Teams-(General)-10-10-2023.pdf
5214-1693458878915-Unit 6 2023 to 2024 academic year assignment (AutoRecovere...
5214-1693458878915-Unit 6 2023 to 2024 academic year assignment (AutoRecovere...
DEEP LEARNING FOR SMART GRID INTRUSION DETECTION: A HYBRID CNN-LSTM-BASED MODEL
DEEP LEARNING FOR SMART GRID INTRUSION DETECTION: A HYBRID CNN-LSTM-BASED MODEL
A study on the lower tropospheric thermal inversion over the arabian sea using radiosonde and iasi data
- 1. A Study on the Lower Tropospheric Thermal Inversion Over the Arabian Sea Using Radiosonde and IASI Data Abstract: Over the temperature inversion regions, tropospheric temperature increases with height and clouds are unable to grow vertically. Over the western Arabian Sea, thermal inversion (TI) is seen at the lower troposphere during the Indian summer monsoon season of June to September. Characteristics of this TI are studied using radiosonde data collected over two stations viz., Muscat (23.5°N; 58.5°E) and Salalah (17.0°N; 54.1°E), located close to the TI region and compared with satellite data. Results suggest that the inversion pattern is highly variable on day-to-day basis over Muscat but is nearly constant over Salalah. Three distinct inversion patterns are identified over Muscat. They are: Type-1: temperature increases with height from surface to about 900 hPa and decreases thereafter; Type-2: temperature decreases with height in a shallow region close to the surface followed by an increase up to about 900 hPa and decreases thereafter; and Type- 3: multiple inversions up to about 850 hPa. Salalah always showed type-2 inversion with peak temperature around 950 hPa. Statistics of the occurrence of different inversion types are computed for Muscat and Salalah. This paper also evaluates the ability of Infrared Atmospheric Sounding Interferometer (IASI) onboard MetOP satellite in identifying the TI over the Arabian Sea. IASI data are able to capture type-1 and type-2 inversions over Muscat but is unable to capture the type-3 inversions due to its coarser vertical resolution. IASI data are also unable to capture the sharp inversion over Salalah for the same reason.