This document discusses the climate and weather patterns of India. It defines weather as the short-term atmospheric conditions over an area, while climate describes conditions over 30+ years for a large region. The monsoon winds strongly influence India's climate, bringing rain from June to September. Different parts of India experience significant variation in temperature, precipitation, and seasons due to geographic factors like latitude, distance from the sea, ocean currents, and relief features. The document provides details on the seasonal reversal of winds known as the monsoon, as well as the onset and withdrawal periods for the southwest and northeast monsoons respectively.
The document discusses India's monsoon seasons. It describes the weather patterns and rainfall during the winter season from December to February, the hot summer season from March to May, the advancing monsoon season in early June, the features of the Indian monsoon, and the retreating/post-monsoon season from October to November. The monsoon brings abundant rainfall to much of India from June to September, but can also cause floods and droughts. It impacts agriculture and binds the country together.
The document discusses the natural vegetation found in India, which varies depending on climate conditions like rainfall. It identifies five main types of natural vegetation in India:
1. Tropical evergreen forests, found in areas with over 200 cm of rainfall like the Western Ghats, remain warm and wet throughout the year with tall trees reaching 60 meters.
2. Tropical deciduous forests are located in regions with under 200 cm rainfall, where trees shed their leaves during the dry season.
3. Thorny bushes are found in areas with 50-100 cm rainfall like western Rajasthan that have adapted to survive on little water.
4. Mountain vegetation varies with altitude in the Himalayas.
The document discusses the main factors affecting India's climate, including latitude, altitude, direction of mountains, distance from the sea, and winds. It then provides information on India's average temperature in summer, the advance of the monsoon, annual rainfall patterns, and average rainfall and monsoon wind directions in January and July. Key climatic terms such as cyclone, leeward side, pastoralists, subcontinent, and western disturbances are also defined.
The document summarizes weather and climate patterns in India. It describes how the Himalayan mountains prevent cold winds from Central Asia, leading to milder winters compared to central Asia. It outlines the seasonal weather patterns, with the cold season from November to February in the north. Summer months from March to May see rising temperatures as the heat belt shifts north. Strong dry winds called "loo" occur in the north during summer days. The southwest monsoon arrives in early June, bringing abundant rainfall to most of the country over the next month from moisture-laden winds originating from the southern oceans.
A monsoon is a seasonal change in wind direction that typically brings a marked change in local weather. It refers mainly to the Asian monsoon affecting India and Southeast Asia. The monsoon winds are caused when temperature differences between oceans and continents lead to winds blowing from land to ocean most of the year, but from ocean to land during certain months, bringing moist air and monsoon rains. Many parts of the world experience monsoons, most notably Asia where the monsoons are critical for agriculture and life in regions like India.
India has a monsoon climate characterized by distinct seasonal patterns. The climate varies significantly across regions due to factors like latitude, altitude, distance from the sea, and monsoon winds and rainfall. Summer temperatures exceed 45°C in parts of Rajasthan but remain around 20°C in Jammu and Kashmir. Winters dip below -45°C in J&K but stay around 22°C in Thiruvananthapuram. Most regions receive rainfall from June to September brought by the southwest monsoons, while some areas like Tamil Nadu see rains in October and November from northeast monsoons.
This document discusses the climate and weather patterns of India. It defines weather as the short-term atmospheric conditions over an area, while climate describes conditions over 30+ years for a large region. The monsoon winds strongly influence India's climate, bringing rain from June to September. Different parts of India experience significant variation in temperature, precipitation, and seasons due to geographic factors like latitude, distance from the sea, ocean currents, and relief features. The document provides details on the seasonal reversal of winds known as the monsoon, as well as the onset and withdrawal periods for the southwest and northeast monsoons respectively.
The document discusses India's monsoon seasons. It describes the weather patterns and rainfall during the winter season from December to February, the hot summer season from March to May, the advancing monsoon season in early June, the features of the Indian monsoon, and the retreating/post-monsoon season from October to November. The monsoon brings abundant rainfall to much of India from June to September, but can also cause floods and droughts. It impacts agriculture and binds the country together.
The document discusses the natural vegetation found in India, which varies depending on climate conditions like rainfall. It identifies five main types of natural vegetation in India:
1. Tropical evergreen forests, found in areas with over 200 cm of rainfall like the Western Ghats, remain warm and wet throughout the year with tall trees reaching 60 meters.
2. Tropical deciduous forests are located in regions with under 200 cm rainfall, where trees shed their leaves during the dry season.
3. Thorny bushes are found in areas with 50-100 cm rainfall like western Rajasthan that have adapted to survive on little water.
4. Mountain vegetation varies with altitude in the Himalayas.
The document discusses the main factors affecting India's climate, including latitude, altitude, direction of mountains, distance from the sea, and winds. It then provides information on India's average temperature in summer, the advance of the monsoon, annual rainfall patterns, and average rainfall and monsoon wind directions in January and July. Key climatic terms such as cyclone, leeward side, pastoralists, subcontinent, and western disturbances are also defined.
The document summarizes weather and climate patterns in India. It describes how the Himalayan mountains prevent cold winds from Central Asia, leading to milder winters compared to central Asia. It outlines the seasonal weather patterns, with the cold season from November to February in the north. Summer months from March to May see rising temperatures as the heat belt shifts north. Strong dry winds called "loo" occur in the north during summer days. The southwest monsoon arrives in early June, bringing abundant rainfall to most of the country over the next month from moisture-laden winds originating from the southern oceans.
A monsoon is a seasonal change in wind direction that typically brings a marked change in local weather. It refers mainly to the Asian monsoon affecting India and Southeast Asia. The monsoon winds are caused when temperature differences between oceans and continents lead to winds blowing from land to ocean most of the year, but from ocean to land during certain months, bringing moist air and monsoon rains. Many parts of the world experience monsoons, most notably Asia where the monsoons are critical for agriculture and life in regions like India.
India has a monsoon climate characterized by distinct seasonal patterns. The climate varies significantly across regions due to factors like latitude, altitude, distance from the sea, and monsoon winds and rainfall. Summer temperatures exceed 45°C in parts of Rajasthan but remain around 20°C in Jammu and Kashmir. Winters dip below -45°C in J&K but stay around 22°C in Thiruvananthapuram. Most regions receive rainfall from June to September brought by the southwest monsoons, while some areas like Tamil Nadu see rains in October and November from northeast monsoons.
it`s easy to get full marks in exam by completing question of this question bank!!try it get a full scope to be the topper of the class!!@@ if u like it very much then u can share it ! to any body else who need helps in this subject:: THNX FOR SEEING MY PROJECT!(my email::ansumanpanigrahi321@gmail.com) mail me if u want further more chapter for help~!! with images and lot`s of animation
Monsoon is a seasonal change in winds and precipitation associated with differing heating of land and sea. There are three main types of monsoon: summer monsoon brings heavy rain between April and September as warm air blows from the southwest Indian Ocean toward countries like India; winter monsoon has dominant easterly winds and a strong tendency toward drought; and a dry monsoon occurs between October and April in South and Southeast Asia with rain-bearing winds from May to September and dry winds the rest. Monsoons result from differing annual temperature trends over land and water.
India is home to an extraordinary variety of climatic regions, ranging from tropical in the south to temperate in the Himalayan north, where elevated regions receive sustained winter snowfall. The nation's climate is strongly influenced by the Himalayas and the Thar Desert.Though the Tropic of Cancer—the boundary between the tropics and subtropics—passes through the middle of India, the bulk of the country can be regarded as climatically tropical.
India has significant climate variations due to its large size and diverse topography. The monsoon winds and Himalayan mountains play a key role in determining India's regional climates. The monsoons are vital, providing most of India's annual rainfall from June to September and influencing the agricultural cycle. However, monsoon rainfall is uneven in amount and timing, sometimes causing droughts or floods. The climate zones range from tropical in the south to cooler temperate in the north.
1) Climate refers to long term weather patterns over a large area, while weather describes short term atmospheric conditions.
2) India's climate is influenced by monsoon winds which arrive in June and bring rainfall until September, affecting agriculture and life across the country.
3) Several factors influence India's climate, including latitude, altitude, distance from oceans, winds and ocean currents, and mountain relief. Climate varies significantly from northern to southern India and across different seasons.
The hot weather season in India lasts from March to May. Temperatures are highest during this time, reaching 38°C in March in the Deccan plateau, around 42°C in parts of Gujarat and Madhya Pradesh in April, and commonly reaching 45°C in northwestern India in May. Coastal areas experience lower temperatures due to ocean influences. Towards the end of May, a low pressure area develops over northern India, bringing strong hot winds called "loo" and dust storms. Precipitation is low except for some thunderstorms and nor'westers that provide temporary relief and small amounts of rainfall. Local winds include "mango showers" and "kaal baishak
India has a diverse climate due to its large size and varied topography. Several factors influence India's climate including latitude, altitude, pressure systems, distance from the sea, ocean currents, and relief features. The country experiences distinct seasonal patterns driven by the monsoon winds and weather systems. The monsoon arrives in June and brings heavy rainfall to most parts of the country until September, while winter from December to February is generally dry except in some coastal areas. Regional variations in temperature and precipitation exist across India.
India belongs to the tropical monsoon climate zone. Since the Indian subcontinent is separated from the rest of Asia by the lofty Himalayan ranges, they block the cold air masses moving southwards from Central Asia. The climatic conditions of India are highlighted in this module.
Pakistan has four main climatic zones based on its diverse topography:
1) A highland climate in the northern, northwestern, and western mountains with cold winters, mild summers, and high rainfall.
2) A semi-arid to arid lowland climate in the Indus Plain with hot summers, cool winters, and monsoon rainfall varying from north to south.
3) A coastal climate along the southern coast with sea breezes moderating temperatures and humidity over 50% in spring and summer, and little rainfall.
4) An arid climate in southwestern Balochistan and the southeastern desert with extreme heat, dryness, and dust storms.
INDIA CLIMATE VEGETATION AND WILDLIFE MADE BY (S.CHIDAMBARANATHAN)3chidam
This document discusses various topics related to weather, climate, and vegetation in India. It covers different seasons and climates in India, the factors that influence weather, the major types of natural vegetation including tropical rainforests and their characteristics. It also discusses mountain vegetation, mangrove forests, and wildlife found in Indian forests. The document contains revision questions and answers related to these topics.
NCERT Geography Notes cl ix ch 4 part iiNidhi Mathur
The mechanism of the Indian monsoon depends on changes in pressure and wind conditions due to the apparent movement of the sun. During winter, high pressure develops over land causing winds to blow from land to sea. In summer, low pressure develops over interior Asia and northwestern India causing winds to blow from the southern oceans towards India. These southwest monsoon winds carry large amounts of moisture from warm oceans, causing widespread rainfall over mainland India. Several factors influence the monsoon mechanism, including differential heating of land and water, the shifting of the ITCZ, high pressure east of Madagascar, heating of the Tibetan Plateau, and movement of jet streams. The El Nino Southern Oscillation also affects the Indian monsoon
NCERT Geography Notes cl9 ch4 climate as pptNidhi Mathur
The document differentiates between weather and climate. Weather refers to short term atmospheric conditions over a small area, such as sunny or cloudy days, whereas climate describes average conditions over a long period of time, such as decades, in a large area. It also discusses regional variations in India's climate with examples like higher temperatures in Rajasthan versus cooler temperatures in Jammu and Kashmir. Factors affecting a region's climate mentioned include latitude, altitude, pressure/wind systems, distance from the sea, ocean currents, and relief features.
The document summarizes the onset, progression, and retreat of the Indian monsoon season. It notes that the monsoon lasts from early June to mid-September, arriving first in Kerala on June 1st before progressing northward. The monsoon divides into two branches - one from the Arabian Sea and one from the Bay of Bengal. By mid-July, the monsoon has reached northern parts of India. The monsoon's retreat begins in early September, first withdrawing from northwestern states and reaching the peninsula by mid-October before withdrawing completely in early December. The document also discusses regional rainfall patterns like winter monsoons and western disturbances.
This document analyzes the relationship between the Indian summer monsoon and the Northern and Southern Annular Modes. It finds that the Southern Annular Mode in June and the North Atlantic Oscillation in April can influence Indian monsoon rainfall, with a stronger effect when the SAM is positive and NAO is negative. This combination is linked to negative rainfall anomalies in southwest and central India but positive anomalies in northeast India, resembling monsoon break conditions. The study indicates these large-scale atmospheric modes may help predict July-August rainfall patterns over India.
The document discusses the climate and weather patterns of Pakistan. It describes four main seasons in Pakistan - winter, early summer, late summer, and post-monsoon. Rainfall in Pakistan comes from monsoon winds, western depressions, convectional currents, relief rainfall, and tropical cyclones. Pakistan has several climatic zones including the highland zone with cold winters and mild summers, the arid zone with hot and dry conditions, the lowland zone with hot summers and cool winters, and the coastal zone with moderate temperatures influenced by the sea. Factors like latitude, altitude, and proximity to the sea or desert affect temperatures across Pakistan. Flooding sometimes occurs when excessive monsoon rains cause rivers to
This document summarizes the climate of India, focusing on the tropical monsoon climate and seasonal variations. It discusses key factors like the Indian monsoon winds which are influenced by differential heating/cooling of land and sea and the movement of pressure systems. India experiences a hot summer season from March to May with high temperatures, a rainy season from June to September brought by the southwest monsoons, and a mild winter season from November to February in the north with variable winds and occasional rainfall. The climate varies significantly by region due to factors like latitude, altitude, proximity to oceans, and monsoon patterns.
Pakistan climate A Lecture by Allah Dad Khan Visiting Professor AUPeshawarMr.Allah Dad Khan
Pakistan has a climate that varies widely by region. It faces increasing vulnerability to climate change impacts like more frequent natural disasters over shorter periods. According to some indexes, Pakistan ranks among the most vulnerable countries to climate change effects. The country experiences extremes ranging from very hot, dry conditions near coastal areas to cooler temperatures in the mountainous northeast. It also has significant seasonal variation with a hot, wet summer monsoon season and a cold, dry winter.
This document summarizes the key aspects of monsoons in India. It describes that monsoons are seasonal winds that blow in a particular direction seasonally. The southwest monsoon brings moisture from the sea to land in India from June to September, while the northeast monsoon reverses the pattern from December to February. It then explains several mechanisms that drive the monsoons, including differential heating of land and sea, shifting of the Intertropical Convergence Zone, heating of the Tibetan Plateau, and high pressure systems. The southern oscillation and El Nino patterns can also impact monsoon rains in India.
According to a technology integration specialist, 21st century skills students need include discerning information, finding answers to problems, and being comfortable using various applications. Educational technology should make instruction student-centered, education collaborative, and learning contextual. The roles of educational technology are to improve teaching and analyze the teaching-learning process, improve learning and enhance educational goals, train teachers, develop curriculum and teaching-learning materials, strategies and aids, help with overall improvement, and identify community needs.
The Division Transit Project will improve bus service along SE Division Street between Downtown Portland and Gresham. It will use longer buses that can hold 60% more passengers. It will add stations with amenities like weather protection and allow multiple-door boarding for quicker stops. Traffic signals will prioritize buses to reduce travel times by up to 20%. The project aims to improve reliability and increase ridership on one of TriMet's busiest lines serving over 10,000 daily riders. Construction will begin in 2017 with new service starting in 2021.
it`s easy to get full marks in exam by completing question of this question bank!!try it get a full scope to be the topper of the class!!@@ if u like it very much then u can share it ! to any body else who need helps in this subject:: THNX FOR SEEING MY PROJECT!(my email::ansumanpanigrahi321@gmail.com) mail me if u want further more chapter for help~!! with images and lot`s of animation
Monsoon is a seasonal change in winds and precipitation associated with differing heating of land and sea. There are three main types of monsoon: summer monsoon brings heavy rain between April and September as warm air blows from the southwest Indian Ocean toward countries like India; winter monsoon has dominant easterly winds and a strong tendency toward drought; and a dry monsoon occurs between October and April in South and Southeast Asia with rain-bearing winds from May to September and dry winds the rest. Monsoons result from differing annual temperature trends over land and water.
India is home to an extraordinary variety of climatic regions, ranging from tropical in the south to temperate in the Himalayan north, where elevated regions receive sustained winter snowfall. The nation's climate is strongly influenced by the Himalayas and the Thar Desert.Though the Tropic of Cancer—the boundary between the tropics and subtropics—passes through the middle of India, the bulk of the country can be regarded as climatically tropical.
India has significant climate variations due to its large size and diverse topography. The monsoon winds and Himalayan mountains play a key role in determining India's regional climates. The monsoons are vital, providing most of India's annual rainfall from June to September and influencing the agricultural cycle. However, monsoon rainfall is uneven in amount and timing, sometimes causing droughts or floods. The climate zones range from tropical in the south to cooler temperate in the north.
1) Climate refers to long term weather patterns over a large area, while weather describes short term atmospheric conditions.
2) India's climate is influenced by monsoon winds which arrive in June and bring rainfall until September, affecting agriculture and life across the country.
3) Several factors influence India's climate, including latitude, altitude, distance from oceans, winds and ocean currents, and mountain relief. Climate varies significantly from northern to southern India and across different seasons.
The hot weather season in India lasts from March to May. Temperatures are highest during this time, reaching 38°C in March in the Deccan plateau, around 42°C in parts of Gujarat and Madhya Pradesh in April, and commonly reaching 45°C in northwestern India in May. Coastal areas experience lower temperatures due to ocean influences. Towards the end of May, a low pressure area develops over northern India, bringing strong hot winds called "loo" and dust storms. Precipitation is low except for some thunderstorms and nor'westers that provide temporary relief and small amounts of rainfall. Local winds include "mango showers" and "kaal baishak
India has a diverse climate due to its large size and varied topography. Several factors influence India's climate including latitude, altitude, pressure systems, distance from the sea, ocean currents, and relief features. The country experiences distinct seasonal patterns driven by the monsoon winds and weather systems. The monsoon arrives in June and brings heavy rainfall to most parts of the country until September, while winter from December to February is generally dry except in some coastal areas. Regional variations in temperature and precipitation exist across India.
India belongs to the tropical monsoon climate zone. Since the Indian subcontinent is separated from the rest of Asia by the lofty Himalayan ranges, they block the cold air masses moving southwards from Central Asia. The climatic conditions of India are highlighted in this module.
Pakistan has four main climatic zones based on its diverse topography:
1) A highland climate in the northern, northwestern, and western mountains with cold winters, mild summers, and high rainfall.
2) A semi-arid to arid lowland climate in the Indus Plain with hot summers, cool winters, and monsoon rainfall varying from north to south.
3) A coastal climate along the southern coast with sea breezes moderating temperatures and humidity over 50% in spring and summer, and little rainfall.
4) An arid climate in southwestern Balochistan and the southeastern desert with extreme heat, dryness, and dust storms.
INDIA CLIMATE VEGETATION AND WILDLIFE MADE BY (S.CHIDAMBARANATHAN)3chidam
This document discusses various topics related to weather, climate, and vegetation in India. It covers different seasons and climates in India, the factors that influence weather, the major types of natural vegetation including tropical rainforests and their characteristics. It also discusses mountain vegetation, mangrove forests, and wildlife found in Indian forests. The document contains revision questions and answers related to these topics.
NCERT Geography Notes cl ix ch 4 part iiNidhi Mathur
The mechanism of the Indian monsoon depends on changes in pressure and wind conditions due to the apparent movement of the sun. During winter, high pressure develops over land causing winds to blow from land to sea. In summer, low pressure develops over interior Asia and northwestern India causing winds to blow from the southern oceans towards India. These southwest monsoon winds carry large amounts of moisture from warm oceans, causing widespread rainfall over mainland India. Several factors influence the monsoon mechanism, including differential heating of land and water, the shifting of the ITCZ, high pressure east of Madagascar, heating of the Tibetan Plateau, and movement of jet streams. The El Nino Southern Oscillation also affects the Indian monsoon
NCERT Geography Notes cl9 ch4 climate as pptNidhi Mathur
The document differentiates between weather and climate. Weather refers to short term atmospheric conditions over a small area, such as sunny or cloudy days, whereas climate describes average conditions over a long period of time, such as decades, in a large area. It also discusses regional variations in India's climate with examples like higher temperatures in Rajasthan versus cooler temperatures in Jammu and Kashmir. Factors affecting a region's climate mentioned include latitude, altitude, pressure/wind systems, distance from the sea, ocean currents, and relief features.
The document summarizes the onset, progression, and retreat of the Indian monsoon season. It notes that the monsoon lasts from early June to mid-September, arriving first in Kerala on June 1st before progressing northward. The monsoon divides into two branches - one from the Arabian Sea and one from the Bay of Bengal. By mid-July, the monsoon has reached northern parts of India. The monsoon's retreat begins in early September, first withdrawing from northwestern states and reaching the peninsula by mid-October before withdrawing completely in early December. The document also discusses regional rainfall patterns like winter monsoons and western disturbances.
This document analyzes the relationship between the Indian summer monsoon and the Northern and Southern Annular Modes. It finds that the Southern Annular Mode in June and the North Atlantic Oscillation in April can influence Indian monsoon rainfall, with a stronger effect when the SAM is positive and NAO is negative. This combination is linked to negative rainfall anomalies in southwest and central India but positive anomalies in northeast India, resembling monsoon break conditions. The study indicates these large-scale atmospheric modes may help predict July-August rainfall patterns over India.
The document discusses the climate and weather patterns of Pakistan. It describes four main seasons in Pakistan - winter, early summer, late summer, and post-monsoon. Rainfall in Pakistan comes from monsoon winds, western depressions, convectional currents, relief rainfall, and tropical cyclones. Pakistan has several climatic zones including the highland zone with cold winters and mild summers, the arid zone with hot and dry conditions, the lowland zone with hot summers and cool winters, and the coastal zone with moderate temperatures influenced by the sea. Factors like latitude, altitude, and proximity to the sea or desert affect temperatures across Pakistan. Flooding sometimes occurs when excessive monsoon rains cause rivers to
This document summarizes the climate of India, focusing on the tropical monsoon climate and seasonal variations. It discusses key factors like the Indian monsoon winds which are influenced by differential heating/cooling of land and sea and the movement of pressure systems. India experiences a hot summer season from March to May with high temperatures, a rainy season from June to September brought by the southwest monsoons, and a mild winter season from November to February in the north with variable winds and occasional rainfall. The climate varies significantly by region due to factors like latitude, altitude, proximity to oceans, and monsoon patterns.
Pakistan climate A Lecture by Allah Dad Khan Visiting Professor AUPeshawarMr.Allah Dad Khan
Pakistan has a climate that varies widely by region. It faces increasing vulnerability to climate change impacts like more frequent natural disasters over shorter periods. According to some indexes, Pakistan ranks among the most vulnerable countries to climate change effects. The country experiences extremes ranging from very hot, dry conditions near coastal areas to cooler temperatures in the mountainous northeast. It also has significant seasonal variation with a hot, wet summer monsoon season and a cold, dry winter.
This document summarizes the key aspects of monsoons in India. It describes that monsoons are seasonal winds that blow in a particular direction seasonally. The southwest monsoon brings moisture from the sea to land in India from June to September, while the northeast monsoon reverses the pattern from December to February. It then explains several mechanisms that drive the monsoons, including differential heating of land and sea, shifting of the Intertropical Convergence Zone, heating of the Tibetan Plateau, and high pressure systems. The southern oscillation and El Nino patterns can also impact monsoon rains in India.
According to a technology integration specialist, 21st century skills students need include discerning information, finding answers to problems, and being comfortable using various applications. Educational technology should make instruction student-centered, education collaborative, and learning contextual. The roles of educational technology are to improve teaching and analyze the teaching-learning process, improve learning and enhance educational goals, train teachers, develop curriculum and teaching-learning materials, strategies and aids, help with overall improvement, and identify community needs.
The Division Transit Project will improve bus service along SE Division Street between Downtown Portland and Gresham. It will use longer buses that can hold 60% more passengers. It will add stations with amenities like weather protection and allow multiple-door boarding for quicker stops. Traffic signals will prioritize buses to reduce travel times by up to 20%. The project aims to improve reliability and increase ridership on one of TriMet's busiest lines serving over 10,000 daily riders. Construction will begin in 2017 with new service starting in 2021.
Froilan Esplaguera Abella is a System Specialist currently working at NCS Pte. Ltd. supporting over 6,500 computers at Khoo Teck Puat Hospital. He has over 10 years of experience in customer service, technical support, and systems administration roles. His skills include Windows, networking, virtualization, patch management, and troubleshooting various hardware and software issues. He holds several certifications including ITIL, MCSA, and has a Bachelor's degree in Information Technology.
Marco culture is defined by getting results, taking risks, and continuous improvement. They have achieved high customer satisfaction ratings and service resolution rates. Marco seeks to innovate, challenge benchmarks, and implement new technologies. They value transparency, customer focus, and developing their employees.
10 Ways Your Boss Kills Employee MotivationOfficevibe
This document outlines 10 ways that bosses can kill employee motivation, including micromanaging employees, focusing only on mistakes, dismissing new ideas, holding useless meetings, making empty promises, telling inappropriate jokes, not keeping their word, measuring employee success in the wrong way, setting unrealistic deadlines, and playing favorites. The document encourages bosses to listen to employee concerns to better motivate them.
- The gig economy as currently defined will not last long term, as tasks like ridesharing and delivery are likely to be automated. However, skilled professionals using platforms like Thumbtack to find clients will persist and proliferate.
- Technology is empowering skilled tradespeople by allowing them to connect directly with customers and run their businesses more efficiently without traditional employers. Skilled professionals are less reliant on college degrees and are building middle-class lifestyles through online skills marketplaces.
- Policymakers should support independent workers through policies that provide safety nets and make it easier for skilled professionals to succeed without full-time employment.
Recovery: Job Growth and Education Requirements Through 2020CEW Georgetown
Recovery: Job Growth and Education Requirements Through 2020: Projections of jobs and education requirements through 2020. This report shows where the jobs will be by education level, occupation and industry. Recovery 2020 is an update to our Help Wanted: Projections of Jobs and Education Requirements Through 2018.
African Americans: College Majors and Earnings CEW Georgetown
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The Online College Labor Market: Where the Jobs Are More than 80 percent of job openings for workers with a bachelor’s degree or higher are posted online. This report analyzes the demand for college talent in the job market by examining online job advertisements for college degree-holders by education, occupations, and industries.
BigWeatherGear Group and Corporate Services Brochure 2013Kristin Matson
Thank you for your interest in Bigweathergear.com Group Sales. We have been in business for over 20 years selling high quality outdoor gear. We specialize in Government, Corporate, and Group volume orders. Our staff of experts can help you fill your gear needs whether they are basic or very specific. We have custom logo applications available on most of the products we carry.
How to run system administrator recruitment process? By creating platform based on open source parts in just 2 nights! I gave this talk in Poland / Kraków OWASP chapter meeting on 17th October 2013 at our local Google for Entrepreneurs site. It's focused on security and also shows how to create recruitment process in CTF / challenge way.
This story covers mostly security details of this whole platform. There's great chance, that I will give another talk about this system but this time focusing on technical details. Stay tuned ;)
Creative Traction Methodology - For Early Stage StartupsTommaso Di Bartolo
The document discusses the Creative Traction Methodology (CTM) for gaining traction for new products and ideas. CTM has three parts: 1) The Idea Release Life Cycle which emphasizes validating ideas before development and engaging communities early. 2) Ransack Tools which means leveraging new growth hacking strategies and tools. 3) Act Creatively which involves lateral thinking with no biases to attract niche audiences and validate assumptions through experimentation. The document provides examples and case studies for applying each part of CTM.
SXSW Interactive is amazing this year! I’m talking VR, AR, IoT, enter next acronym here, and even the P.O.T.U.S. made an appearance.
SXSW plays an increasingly important role in revolutionizing interactive media. While often known as a hotbed for tech startups, it’s the discussions around practical applications of such media, the opportunities they present, and the surrounding implications that have attracted the attention of a growing number of brands, platforms, and creators each year.
In this webinar we share key takeaways from SXSW 2016 and discuss what each means for the year ahead.
Digitized Student Development, Social Media, and IdentityPaul Brown
Originally presented at the ACPA 2016 International Convention in Montreal, Canada. This presentation provides an overview of my research on college student development in digital/social spaces.
This document outlines Bill Aulet's presentation on improving entrepreneurship education. It discusses defining entrepreneurship, assessing student needs through personas, and designing a comprehensive curriculum with modular "tiles" addressing each persona's needs. The goal is to make entrepreneurship education more rigorous, practical, and tailored through open-source sharing of best practices. This will help address the increasing demand for high-quality entrepreneurship training.
Winter is characterized as the coldest season of the year with the shortest days and minimum temperatures. In the Northern Hemisphere, the winter months are December, January and February, while in the Southern Hemisphere they are June, July and August. Key features of winter include long nights, short days, and high snowfall in some areas which can cause transportation problems during blizzards or winter storms.
This document discusses factors that affect climate and weather patterns in the Philippines. It explains that climate is the average weather over time and is influenced by latitude, altitude, proximity to bodies of water, ocean currents, and topography. Temperature and rainfall are most affected by latitude, with equatorial regions experiencing higher temperatures and rainfall. Altitude, land/water distribution, winds, and monsoon patterns also impact regional climates. The Philippines experiences two pronounced monsoon seasons - the northeast monsoon from December to January and the southwest monsoon from July to September.
This document provides information on the six continents of Earth: America, Asia, Africa, Europe, Oceania, and Antarctica. It describes the key characteristics of each continent such as location, regions, climate, bodies of water, and relief. America is the second largest continent divided into North America, Central America, and South America. Asia is the largest continent with varied climate and relief like the Himalayan mountains. Africa is the third largest continent with savannahs and the Sahara desert. Europe is the second smallest continent located in the northern hemisphere. Oceania consists of islands in the Pacific Ocean including Australia. Antarctica is the southernmost continent covered in ice that experiences winter darkness and summer daylight.
Climate refers to the average weather conditions in an area over a long period of time, while weather describes the short-term atmospheric conditions. India's climate is influenced by its latitude, altitude, and pressure and wind systems. The country experiences four main seasons: hot weather, advancing monsoon, retreating monsoon, and cold weather. Major factors like the ITCZ, monsoon winds, and rainfall distribution patterns affect India's seasonal climate.
- The climate of India is dominated by the monsoon system, which brings heavy rainfall during summer months (June-September).
- There is significant regional variation in temperatures across India, with the northern parts experiencing hot summers over 50°C and cold winters below -45°C, while the southern parts generally have more moderate climates.
- The key factors influencing India's climate are its latitude, with the Tropic of Cancer dividing the country into tropical and subtropical zones, as well as its altitude and proximity to the Himalayas and oceans, which provide temperature and rainfall effects.
India has a monsoon type climate characterized by distinct seasonal patterns. The climate is influenced by factors like latitude, altitude, pressure systems, distance from the sea, and ocean currents. The monsoon winds bring heavy rainfall during summer but their arrival and retreat is often irregular, causing uncertainties in agricultural activities. The monsoon binds the country together by providing water for farming across most regions, though some areas receive heavy rainfall while others experience drought.
1) The document discusses different types of weather and climate patterns found in India, including the four main seasons of winter, summer, monsoon, and post-monsoon.
2) It also describes different types of natural vegetation found in India based on climate, including tropical and deciduous forests, thorny bushes, mountain vegetation, and mangrove forests. Common tree species associated with each type are mentioned.
3) The document concludes by discussing the importance of forests in providing resources to humans and serving as wildlife habitats. India's national bird, the peacock, is highlighted. The document contains exercises for students to test their understanding.
This document discusses the climate and natural vegetation found in India. It describes the four main seasons in India - winter, summer, monsoon, and post-monsoon - and characteristics of each. It also outlines the different types of natural vegetation zones in India, including tropical rainforests, deciduous forests, thorny bushes, mountain vegetation, and mangrove forests. Specific trees and plants found in each zone are highlighted. The document emphasizes the importance of forests for providing oxygen, fuel, medicine, and habitat for wildlife.
This document discusses the factors affecting India's climate and the seasonal patterns of weather in India. It describes:
1) The key geographic factors that influence India's climate, including its location, latitude, relief features like the Himalayas and Western Ghats, surface winds, air currents, and ocean patterns.
2) The seasonal patterns of weather in India - the hot weather season from March to May, the advancing monsoon from June to September, the retreating monsoon from October to November, and the cold weather season from December to February.
3) The characteristic weather features of each season, including monsoon winds, rainfall distribution, temperature variations in different regions, and seasonal precipitation patterns across India
This document summarizes the climate of Pakistan. It discusses various climatic zones based on topography, including highland, lowland, coastal, and arid climates. It also describes the four main climatic elements - air pressure, winds, temperature, and rainfall. Different climatic regions experience different weather patterns due to variations in these elements. For example, northern areas receive monsoon rains while coastal areas experience sea breezes that bring moisture. The document also covers climate-related phenomena like droughts and floods that impact Pakistan.
A full teaching learning slides on climate of Pakistan aimed for the support of 0 level students and teachers in the subject Environment of Pakistan 2059/2
Wind is caused by differences in air pressure and moves from high to low pressure areas. The circulation of air on Earth is affected by unequal heating and the planet's rotation. This causes trade winds between 0-30° latitude and prevailing westerlies between 30-60° N latitude. Monsoon winds reverse direction with the seasons, bringing moisture over land in summer. Deserts form due to lack of precipitation and various climatic and geographic factors. They are characterized by sand dunes and features like oases and dry lake beds, and are home to plants and animals adapted to arid conditions.
This document discusses weather, climate, climate zones, and flora and fauna. It defines weather as the current atmospheric conditions, while climate describes average conditions over time for a region. It outlines several climate zones including polar, temperate, and tropical regions. Significant lines of latitude that define zones are listed. Weather stations are described as making continuous measurements to compare readings. Flora refers to plant life classified by region, and fauna represents the indigenous animal life, including classifications for different types of animals.
The document discusses the different seasons in India and their characteristics. It describes the rainy season from June to September, bringing relief from the heat and allowing crops to grow. The rainy season fills tanks and rivers and makes roads muddy. It then discusses the benefits of the rainy season for agriculture, vegetation, and hydroelectricity. It also briefly touches on the characteristics of winter, spring, summer, and autumn seasons in India and other parts of the world.
The document discusses humidity, rainfall, and climate in the Philippines. It provides the following key points:
1) Relative humidity is high in the Philippines due to evaporation from surrounding seas, rich vegetation, and seasonal winds and rains. Humidity remains high throughout the year across the islands.
2) Rainfall varies regionally due to topography and wind patterns. Northeast monsoon rains from November to February bring heavier rainfall to eastern parts of the country.
3) Four main climate types are recognized based on rainfall patterns - ranging from distinct wet/dry seasons to more uniformly distributed rainfall throughout the year.
The climate of South Asia is largely controlled by seasonal monsoon winds and rainfall patterns. During the summer, moist winds from the ocean blow inland, bringing heavy rains that are critical for agriculture but can also cause damaging floods. The monsoon rains were celebrated in ancient Indian poetry and provided the water necessary for crops, but also posed risks if the rains were too heavy or came at the wrong times. The monsoon winds further influenced maritime trade, as ships from other regions timed their voyages to use the winds to reach South Asian ports.
South Asian History {Climate of south Asia}ShahMuhammad55
The climate of South Asia is largely controlled by seasonal monsoon winds and rainfall patterns. During the summer, moist winds from the ocean blow inland, bringing heavy rains that are critical for agriculture but can also cause damaging floods. The monsoon rains were celebrated in ancient Indian poetry and provided the water necessary for crops, but also posed risks if the rains were too heavy or came at the wrong times. The monsoon winds further influenced trade and cultural exchanges, as sailors used the summer winds to reach South Asian ports and then waited for the winter winds to return them to their homelands.
South Asian History {Climate of south asia}ShahMuhammad55
The climate of South Asia is largely controlled by seasonal monsoon winds and rainfall patterns. During the summer, moist winds from the ocean blow inland, bringing heavy rains that are critical for agriculture but can also cause damaging floods. The monsoon rains were celebrated in ancient Indian poetry and provided the water necessary for crops, but also posed risks if the rains were too heavy or came at the wrong times. The monsoon winds further influenced trade and cultural exchange, as sailors used the summer winds to reach South Asian ports and then waited for the winter winds to return them to their homelands.
The document summarizes India's climate and seasonal patterns. It discusses factors like the Himalayas, monsoon winds, varied terrain, and surrounding seas that influence India's climate. The monsoon season from June to September brings heavy rainfall to much of the country. Winter from December to February sees rainfall from western disturbances in parts of North India. The climate varies regionally from tropical in the south to temperate in the north. Seasons include a hot dry summer and monsoon followed by retreating and northeast monsoon periods.
The document discusses the physiography and physical geography of India. It divides India into several physiographic divisions: the Northern and Northeastern Mountains (the Himalayas), the Northern Plain, the Peninsular Plateau, the Indian Desert, and the Coastal Plains. It provides detailed descriptions of each division, including the mountain ranges, rivers, vegetation, and other features of each region.
How to Make a Field Mandatory in Odoo 17Celine George
In Odoo, making a field required can be done through both Python code and XML views. When you set the required attribute to True in Python code, it makes the field required across all views where it's used. Conversely, when you set the required attribute in XML views, it makes the field required only in the context of that particular view.
This presentation was provided by Steph Pollock of The American Psychological Association’s Journals Program, and Damita Snow, of The American Society of Civil Engineers (ASCE), for the initial session of NISO's 2024 Training Series "DEIA in the Scholarly Landscape." Session One: 'Setting Expectations: a DEIA Primer,' was held June 6, 2024.
How to Build a Module in Odoo 17 Using the Scaffold MethodCeline George
Odoo provides an option for creating a module by using a single line command. By using this command the user can make a whole structure of a module. It is very easy for a beginner to make a module. There is no need to make each file manually. This slide will show how to create a module using the scaffold method.
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
Executive Directors Chat Leveraging AI for Diversity, Equity, and InclusionTechSoup
Let’s explore the intersection of technology and equity in the final session of our DEI series. Discover how AI tools, like ChatGPT, can be used to support and enhance your nonprofit's DEI initiatives. Participants will gain insights into practical AI applications and get tips for leveraging technology to advance their DEI goals.
Walmart Business+ and Spark Good for Nonprofits.pdfTechSoup
"Learn about all the ways Walmart supports nonprofit organizations.
You will hear from Liz Willett, the Head of Nonprofits, and hear about what Walmart is doing to help nonprofits, including Walmart Business and Spark Good. Walmart Business+ is a new offer for nonprofits that offers discounts and also streamlines nonprofits order and expense tracking, saving time and money.
The webinar may also give some examples on how nonprofits can best leverage Walmart Business+.
The event will cover the following::
Walmart Business + (https://business.walmart.com/plus) is a new shopping experience for nonprofits, schools, and local business customers that connects an exclusive online shopping experience to stores. Benefits include free delivery and shipping, a 'Spend Analytics” feature, special discounts, deals and tax-exempt shopping.
Special TechSoup offer for a free 180 days membership, and up to $150 in discounts on eligible orders.
Spark Good (walmart.com/sparkgood) is a charitable platform that enables nonprofits to receive donations directly from customers and associates.
Answers about how you can do more with Walmart!"
বাংলাদেশের অর্থনৈতিক সমীক্ষা ২০২৪ [Bangladesh Economic Review 2024 Bangla.pdf] কম্পিউটার , ট্যাব ও স্মার্ট ফোন ভার্সন সহ সম্পূর্ণ বাংলা ই-বুক বা pdf বই " সুচিপত্র ...বুকমার্ক মেনু 🔖 ও হাইপার লিংক মেনু 📝👆 যুক্ত ..
আমাদের সবার জন্য খুব খুব গুরুত্বপূর্ণ একটি বই ..বিসিএস, ব্যাংক, ইউনিভার্সিটি ভর্তি ও যে কোন প্রতিযোগিতা মূলক পরীক্ষার জন্য এর খুব ইম্পরট্যান্ট একটি বিষয় ...তাছাড়া বাংলাদেশের সাম্প্রতিক যে কোন ডাটা বা তথ্য এই বইতে পাবেন ...
তাই একজন নাগরিক হিসাবে এই তথ্য গুলো আপনার জানা প্রয়োজন ...।
বিসিএস ও ব্যাংক এর লিখিত পরীক্ষা ...+এছাড়া মাধ্যমিক ও উচ্চমাধ্যমিকের স্টুডেন্টদের জন্য অনেক কাজে আসবে ...
2. CLIMATE
THE WEATHER CONDITIONS PREVAILING IN AN AREA IN GENERAL OR OVER
A LONG PERIOD IS CALLED A CLIMATE.
THERE ARE MAINLY 4 TYPES OF SEASONS :-
1. SUMMER
2. WINTER
3. MONSOON
4. AUTUMN
6. SUMMER BEGINS ON THE DAY OF THE SUMMER SOLSTICE AND ENDS ON THE
DAY OF THE AUTUMNAL EQUINOX.
THE DAYS ARE LONGER AND THE NIGHTS ARE SHORTER.
WHEN IT IS SUMMER IN SOUTHERN HEMISPHERE, IT IS WINTER IN NORTHERN
HEMISPHERE, AND VICE VERSA.
IT IS THE WHOLE MONTHS OF DECEMBER, JANUARY, AND FEBRUARY IN
SOUTHERN HEMISPHERE, AND THE WHOLE MONTHS OF JUNE, JULY, AND
AUGUST IN THE NORTHERN HEMISPHERE.
7. COMPARED TO NORTHERN INDIA, PENINSULAR INDIA, REMAINS
COOLER DUE TO THE INFLUENCE OF THE OCEANS.
THE ‘LOO’ , ‘DUST STORMS’ AND ‘THUNDER STORMS’ ARE THE MOST
STRIKING FEATURES OF THE SUMMER SEASON IN INDIA.
MANY TREES, SHRUBS, AND FLOWERS GROW THE MOST DURING THE
SUMMER
8. DISADVANTAGE
RIVERS, STREAMS AND PONDS DRY UP IN SUMMER AND CAUSE SCARCITY OF WATER.
EVEN BIRDS AND BEAST FEEL THIRSTY AND RUN FROM PLACE TO PLACE.
MANY PEOPLE, BIRDS AND BEASTS DIE AS A RESULT OF SUNSTROKE.
MANY FATAL DISEASES, SUCH AS CHOLER, SMALL-POX, ETC. BREAK OUT OF SUMMER SEASON.
THE PLANTS, HERBS AND SHRUBS GET DRIED UP BECAUSE OF THE SCORCHING SUN AND HOT
WINDS.
9.
10. WINTER IS THE COLDEST SEASON OF THE YEAR IN POLAR AND TEMPERATE
CLIMATES, BETWEEN AUTUMN AND SPRING.
IT BEGINS FROM MID-NOVEMBER IN NORTHERN INDIA AND LASTS TILL FEBRUARY.
DECEMBER AND JANUARY ARE THE COLDEST MONTH IN NORTHERN HEMISPHERE.
THE TEMPERATURE DECREASES FROM SOUTH TO THE NORTH.
FROST IS COMMON IN THE NORTH AND THE HIGHER SLOPES OF THE HIMALAYAS
EXPERIENCE SNOWFALL DURING THE WINTER MONTHS.
11. THE DAYS ARE SHORTER AND THE NIGHTS ARE LONGER IN WINTER.
ASIATIC SPARROW – HAWK, HARRIERS, PEREGRINE FALCON, OSPREY, PACIFIC GOLDEN
FLOWER, AND SOME OTHER BIRDS MIGRATE IN WINTER.
TOTAL AMOUNT OF WINTER RAINFALL LOCALLY KNOWN AS ‘MAHAWAT’ IS SMALL. THEY
ARE OF IMMENSE IMPORTANCE FOR THE CULTIVATION OF ‘RABI’ CROPS.
THE SOUTHERN REGIONS OF INDIA DO NOT EXPERIENCE COLD WEATHER.
THE PENINSULAR REGION DOES NOT HAVE WELL DEFINED COLD SEASON.
12. DISADVANTAGE
PEOPLE LOSE MUCH OF THEIR TIME TO DO SOMETHING MAINLY
HOUSEHOLD THAT INCLUDE WEATHER, SUCH AS TO WASH CLOTHES
AND DISHES. WE NEED MUCH TIME TO WEAR CLOTHES TO KEEP
WARM.
PEOPLE SUFFER FROM COMMON COLD, INFLUENZA, PNEUMONIA, ETC.
14. MONSOON IS TRADITIONALLY DEFINED AS A SEASONAL REVERSING WIND
ACCOMPANIED BY CORRESPONDING CHANGES IN PRECIPITATION.
IT OCCURS IN JUNE, JULY, AUGUST AND SEPTEMBER.
IT IS REFER AS RAINY PHASE OF A SEASONALLY CHANGING PATTERN.
THE MAJOR MONSOON SYSTEMS OF THE WORLD CONSIST OF THE WESTERN AFRICAN
AND ASIA- AUSTRALIAN MONSOONS.
THE SOUTH-WEST MONSOON WINDS ARE CALLED ‘NAIRUTYA MAARUT’ IN INDIA.
15. MONSOON ALSO OCCUR IN OTHER REGIONS SUCH AS IN NORTH AMERICA, SUB-
SAHARAN AFRICA, BRAZIL AND EAST ASIA.
EVERYTHING BECOMES LUSH AND GREEN IN TROPICAL.
THE SOOTHING SOUND OF RAIN PATTERING ON A TIN ROOF WHEN ITS FALLING
LIGHTLY.
THE RAINS BLOW IN FROM THE INDIAN OCEAN AND ARABIAN SEA IN THE SOUTH-
WEST BRINGING HEAVY RAINFALL TO THE AREA.
IT GOES ON DECREASING FROM EAST TO WEST.
16. DISADVANTAGE
IT CREATES THE SWARMS OF FLIES AND MOSQUITOES.
THE MORE FREQUENT POWER OUTTAGES.
IT TAKES DAYS FOR YOUR FRESHLY WASHED CLOTHES TO DRY.
DIRTY ROADS TURN INTO PONDS, RIVERS, AND/OR SWAMPS.
THE ROOF LEAKS.
OUTBREAKS OF MALARIA, DENGUE AND DYSENTERY.
17.
18. THE WORD AUTUMN COMES FROM THE ANCIENT ETRUSCAN
THE SEASON AFTER SUMMER AND BEFORE WINTER, IN THE NORTHERN
HEMISPHERE FROM SEPTEMBER TO NOVEMBER AND IN THE SOUTHERN
HEMISPHERE FROM MARCH TO MAY.
IT IS ALSO KNOWN AS ‘FALL’ IN NORTH AMERICA.
THE AUTUMNAL EQUINOX SIGNIFIES THE START OF AUTUMN, AND IT ENDS IN
THE WINTER SOLSTICE.
19. THE MAIN FEATURE IS THE SHEDDING OF LEAVES FROM DECIDUOUS TREES.
SOME CULTURES REGARD THE AUTUMNAL EQUINOX AS “MID - AUTUMN”.
MANY ANIMALS BEGIN TO PREPARE FOR THE WINTER BY STORING FOOD IN THEIR
NEST AND DENS OR FAT ON THEIR BODIES.
IN AUTUMN, THERE IS LESS SUNLIGHT BECAUSE THE DAYS ARE SHORTER.