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.
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.
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.
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.
#Arunsakthi #SST #Geography #Climate This is not for commercial purpose This only for students who are pressurized by their teachers to make presentation on this topic [coz,this is made by one of student who have also gone through these pressures(Arunsakthi)]
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
All of the presentations that i have uploaded are made by me for school projects from 9-12 grade.For most of them you actually need to have learned something to recite and what you see on the presentations are just hints.
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.
#Arunsakthi #SST #Geography #Climate This is not for commercial purpose This only for students who are pressurized by their teachers to make presentation on this topic [coz,this is made by one of student who have also gone through these pressures(Arunsakthi)]
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
All of the presentations that i have uploaded are made by me for school projects from 9-12 grade.For most of them you actually need to have learned something to recite and what you see on the presentations are just hints.
This presentation is a combination of different slides which I re-purposed. I included a reference of all the slides I used at the end of my presentation.
This is a biosphere powerpoint I've created for a middle school level science class. It's full of fun animated cartoons and facts on both aquatic and terrestrial biomes.
Class IX - Climate
This lesson throws light upon the details of lesson climate, of CBSE board.
This ppt can be used to revise the lesson in a better manner.
it has details on coriolis force, ferrel's law, monsoon winds
Connector Corner: Automate dynamic content and events by pushing a buttonDianaGray10
Here is something new! In our next Connector Corner webinar, we will demonstrate how you can use a single workflow to:
Create a campaign using Mailchimp with merge tags/fields
Send an interactive Slack channel message (using buttons)
Have the message received by managers and peers along with a test email for review
But there’s more:
In a second workflow supporting the same use case, you’ll see:
Your campaign sent to target colleagues for approval
If the “Approve” button is clicked, a Jira/Zendesk ticket is created for the marketing design team
But—if the “Reject” button is pushed, colleagues will be alerted via Slack message
Join us to learn more about this new, human-in-the-loop capability, brought to you by Integration Service connectors.
And...
Speakers:
Akshay Agnihotri, Product Manager
Charlie Greenberg, Host
JMeter webinar - integration with InfluxDB and GrafanaRTTS
Watch this recorded webinar about real-time monitoring of application performance. See how to integrate Apache JMeter, the open-source leader in performance testing, with InfluxDB, the open-source time-series database, and Grafana, the open-source analytics and visualization application.
In this webinar, we will review the benefits of leveraging InfluxDB and Grafana when executing load tests and demonstrate how these tools are used to visualize performance metrics.
Length: 30 minutes
Session Overview
-------------------------------------------
During this webinar, we will cover the following topics while demonstrating the integrations of JMeter, InfluxDB and Grafana:
- What out-of-the-box solutions are available for real-time monitoring JMeter tests?
- What are the benefits of integrating InfluxDB and Grafana into the load testing stack?
- Which features are provided by Grafana?
- Demonstration of InfluxDB and Grafana using a practice web application
To view the webinar recording, go to:
https://www.rttsweb.com/jmeter-integration-webinar
LF Energy Webinar: Electrical Grid Modelling and Simulation Through PowSyBl -...DanBrown980551
Do you want to learn how to model and simulate an electrical network from scratch in under an hour?
Then welcome to this PowSyBl workshop, hosted by Rte, the French Transmission System Operator (TSO)!
During the webinar, you will discover the PowSyBl ecosystem as well as handle and study an electrical network through an interactive Python notebook.
PowSyBl is an open source project hosted by LF Energy, which offers a comprehensive set of features for electrical grid modelling and simulation. Among other advanced features, PowSyBl provides:
- A fully editable and extendable library for grid component modelling;
- Visualization tools to display your network;
- Grid simulation tools, such as power flows, security analyses (with or without remedial actions) and sensitivity analyses;
The framework is mostly written in Java, with a Python binding so that Python developers can access PowSyBl functionalities as well.
What you will learn during the webinar:
- For beginners: discover PowSyBl's functionalities through a quick general presentation and the notebook, without needing any expert coding skills;
- For advanced developers: master the skills to efficiently apply PowSyBl functionalities to your real-world scenarios.
Search and Society: Reimagining Information Access for Radical FuturesBhaskar Mitra
The field of Information retrieval (IR) is currently undergoing a transformative shift, at least partly due to the emerging applications of generative AI to information access. In this talk, we will deliberate on the sociotechnical implications of generative AI for information access. We will argue that there is both a critical necessity and an exciting opportunity for the IR community to re-center our research agendas on societal needs while dismantling the artificial separation between the work on fairness, accountability, transparency, and ethics in IR and the rest of IR research. Instead of adopting a reactionary strategy of trying to mitigate potential social harms from emerging technologies, the community should aim to proactively set the research agenda for the kinds of systems we should build inspired by diverse explicitly stated sociotechnical imaginaries. The sociotechnical imaginaries that underpin the design and development of information access technologies needs to be explicitly articulated, and we need to develop theories of change in context of these diverse perspectives. Our guiding future imaginaries must be informed by other academic fields, such as democratic theory and critical theory, and should be co-developed with social science scholars, legal scholars, civil rights and social justice activists, and artists, among others.
Accelerate your Kubernetes clusters with Varnish CachingThijs Feryn
A presentation about the usage and availability of Varnish on Kubernetes. This talk explores the capabilities of Varnish caching and shows how to use the Varnish Helm chart to deploy it to Kubernetes.
This presentation was delivered at K8SUG Singapore. See https://feryn.eu/presentations/accelerate-your-kubernetes-clusters-with-varnish-caching-k8sug-singapore-28-2024 for more details.
Essentials of Automations: Optimizing FME Workflows with ParametersSafe Software
Are you looking to streamline your workflows and boost your projects’ efficiency? Do you find yourself searching for ways to add flexibility and control over your FME workflows? If so, you’re in the right place.
Join us for an insightful dive into the world of FME parameters, a critical element in optimizing workflow efficiency. This webinar marks the beginning of our three-part “Essentials of Automation” series. This first webinar is designed to equip you with the knowledge and skills to utilize parameters effectively: enhancing the flexibility, maintainability, and user control of your FME projects.
Here’s what you’ll gain:
- Essentials of FME Parameters: Understand the pivotal role of parameters, including Reader/Writer, Transformer, User, and FME Flow categories. Discover how they are the key to unlocking automation and optimization within your workflows.
- Practical Applications in FME Form: Delve into key user parameter types including choice, connections, and file URLs. Allow users to control how a workflow runs, making your workflows more reusable. Learn to import values and deliver the best user experience for your workflows while enhancing accuracy.
- Optimization Strategies in FME Flow: Explore the creation and strategic deployment of parameters in FME Flow, including the use of deployment and geometry parameters, to maximize workflow efficiency.
- Pro Tips for Success: Gain insights on parameterizing connections and leveraging new features like Conditional Visibility for clarity and simplicity.
We’ll wrap up with a glimpse into future webinars, followed by a Q&A session to address your specific questions surrounding this topic.
Don’t miss this opportunity to elevate your FME expertise and drive your projects to new heights of efficiency.
GraphRAG is All You need? LLM & Knowledge GraphGuy Korland
Guy Korland, CEO and Co-founder of FalkorDB, will review two articles on the integration of language models with knowledge graphs.
1. Unifying Large Language Models and Knowledge Graphs: A Roadmap.
https://arxiv.org/abs/2306.08302
2. Microsoft Research's GraphRAG paper and a review paper on various uses of knowledge graphs:
https://www.microsoft.com/en-us/research/blog/graphrag-unlocking-llm-discovery-on-narrative-private-data/
1. CLIMATE
Climate refers to the sum total of weather conditions and variations over a large
area for a long period of time.
WEATHER:
It refers to state of atmosphere over an area at any point of time.
The elements of weather and climate are temperature, atmospheric pressure,
wind, humidity and precipitation.
INDIAN CLIMATE•
The climate of India is monsoon type.
•Monsoon is derived from „mausim‟which means season and it refers to the
seasonal reversal in the wind direction during a year.
•In Asia, this type of climate is found mainly in south and south-east.
DIFFERENCES IN INDIAN CLIMATE
In summer the temperature of Rajasthan is about 50‟C but in Jammu & Kashmir
it‟s 20‟c.
In winter at J&K the temperature is -45‟C but in Thiruvanantapuram its 22‟C.
While precipitation is in the form of snowfall in upper parts of Himalyas, it rains
over the rest of country.
Most parts receive rainfall from June to July but some like Tamil Nadu receive it
even in the season of October and November.
CLIMATIC CONTROLS
The major controls of climate are:
1.Latitude : Due to curvature the amount of solar energy received varies according
to it.
2.Altitude: As we go higher there is a decrease in temperature of 16‟
3.Pressure and Wind system: As per latitude and altitude temperature and rainfall
also influences the climate.
4.Distance from sea: The sea exerts moderating influence on climate, regions near
2. sea experiences moderate climate.
5.Ocean Currents: It leads continentality which means very hot during summers
and very cold during winters.
FACTORS AFFECTING INDIAN CLIMATE
1.Latitude:
Tropic of cancer almost divides the country in two equal parts running from Rann
of Kuchh to Mizoram.
The region lying in the south of tropic of cancer is tropical whereas the region in
north is in sub tropical.
Therefore India receives both tropical as well as sub-tropical climate.
2.Altitude:
India has mountains in north with average height of 6000m and coast line of about
30m.
The Himalyas act as a barrier to enter winds in India from Centeral Asia.
That‟s why it experiences mild winters as compare to Centeral Asia.
3.PRESSURE and WINDS
It is further devided in three parts.
•Pressure and surface winds
•Upper air circulation
•Western disturbances
Pressure and surface winds: India lies in the region of north-easterly winds which
originate from northern hemispher and blow towards south but
deflected to right due to corollis force.These winds carry small silts that‟s why
don‟t affect India‟s rain.
4.Upper air circulation: Winds travel from a low pressure area to high
pressure area. Air moves from indian ocean to south-east direction crossing
equator and turns right towards indian subcountinent giving rain to it. The upper
air circulation over warm oceans is called jet stream.
3. 5.Western disturbances: During the time of winters in India cyclone formation
takes place in „mediterranean sea‟whose winds are very powerful that after
crossing Pakistan, Afghanistan they finally reach jammu and kashmir leads to
rainfall in winters there.
The unifying influence of the monsoon on the Indian subcontinent is quite
perceptible.
The seasonal alteration of the wind systems and the associated weather conditions
provide a rhythmic cycle of seasons.
Even the uncertainties of rain and uneven distribution are very much typical of the
monsoon.
The Indian landscape, its animal and plant life, the people, including their
festivities, revolve around this phenomenon.
Year after year, people of India from north to south and from east to west, eagerly
await the arrival of the monsoon.
These monsoon winds bind the whole country by providing water to set the
agricultural activities in motion. The river valleys which carry this water also unite
as a single river valley unit.
Early in the season, the windward side of the Western Ghats receives very heavy
rainfall, more than 250cm.
The Deccan Plateau and parts of Madhya Pradesh also receive some amount of
rain in spite of lying in the rain shadow area.
The maximum rainfall of this season is received in the north-eastern part of the
country.
Rainfall in the Ganga valley decreases from the east to the west. Rajasthan and
parts of Gujarat get scanty rainfall.
The breaks in the monsoon are related to the movement of the monsoon tough.
The trough and its axis keep on moving northward or southward. When the axis of
the monsoon trough lies over the plains and widespread rain occur in the
Himalayan Rivers.
Mawsynram in the southern ranges of the Khasi Hills receives the highest average
rainfall in the world.
Ques. Why is monsoon known for its “uncertainties”?
4. While it causes heavy floods in one part, it may be responsible for droughts in the
other.
It is often irregular in its arrival and its retreat. Hence, it sometimes disturbs the
farming schedule of millions of farmers all over the country.
During October-November, the monsoon trough or the low pressure trough over
the northern plains becomes weaker. This is gradually replaced by a high-pressure
system.
The south-east monsoon winds weaken and start withdrawing gradually. By the
beginning of the October, the monsoon withdraws from the Northern Plains.
The months of October-November form a period of transition from hot rainy
season to dry winter conditions. The retreat of the monsoon is marked by clear
skies and rise in temperature.
While day temperatures are high, nights are cool and pleasant.
Owing to the conditions of high temperature and humidity, the weather becomes
rather oppressive during the day. This is known as “OCTOBER HEAT”.
The low-pressure conditions, over north-western India, get transferred to the Bay
of Bengal by early November.
This shift is associated with the occurrence of cyclonic depressions, which
originates over the Andaman Sea.
These cyclones generally cross the eastern coasts of India cause heavy and
widesprad rain.
These tropical cyclones are often very destructive.
The thickly populated deltas of the Godavari, the Krishna and the Kaveri are
frequently struck by cyclones, which cause great damage to life and property.
THE SEASONS
The monsoon type of climate is characterised by a distinct seasonal pattern.
The weather conditions greatly change from one season to the other. The coastal
areas do not experience much variation in temperature though there is variation
in rainfall pattern. Four main seasons can be identified in India- the cold weather
season, hot weather season, the advancing monsoon and the retreating monsoon
with some regional variations.
5. THE COLD WEATHER SEASON (WINTER)
1. The cold weather season begins from mid- November in northern India and
stays
till February.
2. December and January are the coldest months in the northern part of India.
3. The temperature decreases from south to the north.
4. Days are warm and nights are cold.
5. Frost is common in the north and the higher slopes of Himalayas experience
snowfall.
6. The northeast trade winds blow from land to sea and hence, for most part of the
country, it is a dry season.
7. Some amount of rainfall occurs on the Tamil Nadu coast from these winds as,
here they blow from sea to land.
8. The weather is normally marked by clear sky, low temperatures and low
humidity
and feeble variable winds.
9. A characteristic feature of the cold weather season over the northern plains is a
the inflow of cyclonic disturbances from the west and the northwest.
10.They cause the much- needed winter rains over the plains and snowfall in the
mountains.
11.Total amount of winter rainfall locally known as „mahawat‟ is small; they are
of . immense importance for the cultivation of „rabi‟ crops.
12. The peninsular region does not have well- defined cold season.
THE HOT WEATHER SEASON (SUMMER)
1. From March to May, it is hot weather season in India.
2. The influence of shifting of the heat belt can be seen clearly from temperature
recordings taken during March- May at different latitudes.
3. In peninsular India, temperature remain lower due to the moderating influence
of the
oceans.
4.The summer months experience rising temperature and falling air pressure in
the
6. northern part of the country.
5. Towards the end of May, an elongated low pressure area develops in the region
extending from the Thar Desert in the northwest to Patna and Chotanagpur
plateau
and southeast.
6. The striking feature of the hot weather season is the „loo‟. These are strong,
gusty, hot, dry winds blowing during the day over the north and northwestern
India.
7. Dust storms are very common during the month of May in northern India. These
storms bring temporary relief as they lower the temperature and may bring light
rain
and cool breeze.
8. In West Bengal, these storms are known as „Kaal Baisakhi‟.
9. Towards the close of the summer season, pre- monsoon showers are common
especially, in Kerala and Karnataka.
DISTRIBUTION OF RAINFALL
There are three types of rainfall :-Low rainfall (Less than 50 cm.)
- Average rainfall (Between 50 to 250 cm.)
- High rainfall (More than 250 cm.)
1. Parts of western coast and northern India receive over about 400 cm of rainfall
annually.
2. It is less than 60cm in western Rajasthan and adjoining parts of Gujarat,
Haryana and
Punjab.
3. Rainfall is equally low in the interior of Deccan plateau, and east of the
Sahyadris.
4. The rest of the country receives moderate rainfall. Snowfall is restricted to the
Himalayan region.
Because of the nature of monsoons, the annual rainfall is highly variable from year
to year. Variability is high in the regions of low rainfall such as parts of Rajasthan,
Gujarat and leeward (rain shadow area) side of the Western Ghats. While the
areas of high rainfall are responsible to be affected by the floods and the areas of
7. low rainfall are drought- prone.
SOME IMPORTANT TERMS
1. Frost- A state in freezing, frozen dew.
2. Loo- Strong, gusty, hot, dry winds blowing during the day over the north and
northwestern India.
3. Mango showers- Pre-monsoon showers in Kerala and Karnataka help in
ripening of
mangoes earlier, known as monsoon showers.
4. Trough- large vacuum in between of the Himalayas and the peninsular plateau,
the
plains.
5. Leeward- Rain shadow area.
Apara Sanwaria