Why Does Climate Change
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Climate change occurs over long, medium, and short terms. Long term climate cycles, like variations in Earth's orbit and axial tilt that occur over tens of thousands of years, influence how much sunlight reaches Earth. Medium term changes over hundreds of years may be linked to solar output variations from sunspot activity levels. Short term volcanic eruptions can temporarily block sunlight with ash particles, lowering temperatures for months or years, like the 1815 Tambora eruption caused a "year without a summer" and famine.
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![LONG TERM: The Earth’s orbit around the sun changes from circular to elliptical and back over about 100,000 years. ,[object Object],[object Object]](data:image/gif;base64,R0lGODlhAQABAIAAAAAAAP///yH5BAEAAAAALAAAAAABAAEAAAIBRAA7)
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The natural causes of climate change
Large volcanic eruptions can cool the global climate by ejecting ash and sulfur dioxide into the stratosphere, where they reflect sunlight back into space. The 1991 eruption of Mount Pinatubo cooled the planet by 0.5°C for about a year by reducing sunlight by 10%. Even larger eruptions like Tambora in 1815 and Krakatoa in 1883 lowered global temperatures more significantly for multiple years.
Solar variation and climatic changes
This document discusses the relationship between solar variation and climatic changes. It introduces that the sun provides the energy that drives Earth's climate and any changes in the sun's output can affect the climate. It then covers topics like how solar variation is measured, records of past solar activity, the relationship between solar activity and historical climate changes like the Little Ice Age, and conclusions that the climate appears to be highly sensitive even to small changes in solar irradiance.
Long term & short term effects of climate
This document discusses both long-term and short-term causes of climate change. Long-term causes occurring over millions of years include continental drift, changes in Earth's orbit and tilt, which affect ocean currents and temperatures. Short-term causes operating over decades to thousands of years include volcanic eruptions, which eject particles that block sunlight, and shifts in ocean and air currents driven by wind and temperature changes. Together, these natural factors have triggered shifts between ice ages and warmer periods throughout Earth's history.
Climate: Climatic Change - Evidence, Cycles and The Future
A PowerPoint used in class to cover the key forms of evidence you need to know for the Exam. Key Questions are likely to be focused on how we can gain information of past climatic change, and how it can be used to predict future, and I would expect you to be able to comment on the usefulness of the different types. For instance, Ice cores are highly accurate and quantifiable evidence, but gaining them is expensive, and only gives a climatic record for the site at which the snow formed. However, they do provide the longest record of change.
Natural causes of climate change
The Earth’s climate is dynamic and characterised by trends, aberrations and quasi-periodic oscillations varying over a broad range of time-scales [1], which are governed by external (extraterrestrial systems) and/or internal(ocean, atmosphere and land system). Trends are largely controlled by plate tectonics, and thus to change gradually on million year time scale. Aberrations occur when the certain thresholds are passed and are manifested in the geological record as the unusual rapid (less than a few thousands of years) or extreme change in climate. The quasi-periodic oscillations are mostly astronomically paced; they are driven by astronomical perturbations that affect the earth’s orbit around the sun and the orientation of earth’s rotation axis with respect to its orbital plane. These perturbations are described by the three main astronomical cycles: eccentricity, precession and obliquity, which together determine the spatial and seasonal pattern of insolation received by the earth [2], eventually resulting in climatic oscillations of ten to hundreds of thousands of year [3].Sun being the main source of energy for the earth system controls the climate of it. Variation in solar activity and cosmic ray intensity has direct influence over climatic features such as cloudiness, temperature and rainfall [4]. Volcanic eruptions also force all elements of the climatic systems up to a varying degree but producing long term climatic signals in the ocean. The cumulative volcanic cooling effect at present offsets about one third of anthropogenic warming [5].Other than these causes paleoclimatologists also relates the past climate changes with movement of solar system[6], interplanetary dusts and influence of asteroids[7].However the recent variability in climate what earth is experiencing is unlikely due to any of the individual above factors rather it is due to the compound effect of complex interactions of all the natural as well as anthropogenic forcings.
References:
1. J. C. Zachos, M. Pagani, L. Sloan, E. Thomas, K. Billups, Science 292 (2001) 686-693.
2. G. Kukla, Nature (London) 253, 600 (1975).
3. J. D. Hays, J. Imbrie, N. J. Shackleton, Science 194 (1876) 1121-1132.
4. N. Marsh, H. Swensmark, Space Sci. Rev. 94 (2000) 215-230.
5. T. L. Delworth, V. Ramaswamy, G. L. Stenchikov, Geophys. Res. Lett. 32 (2005) L24709.
6. K. Fuhrer, E. W. Wolf, S. J. Johnsen, J. Geophys. Res. 104(D24) (1999) 31043-31052
7. P. Hut, W. Alvarez, W. P. Elder, T. Hansen, E. G. Kauffman, G. Keller, E. M. Shoemaker & P. R. Weissman, Nature Vol. 329, 10 September, 1987
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CCAFS workshop titled "Using Climate Scenarios and Analogues for Designing Adaptation Strategies in Agriculture," 19-23 September in Kathmandu, Nepal. Causes Of Climate Change
The document discusses several potential causes of climate change, including both natural and human factors that can lead to cooling or warming. It describes how the Milankovitch cycles have coincided with ice ages in the past. El Nino and La Nina events involve changes in ocean circulation patterns in the Pacific that impact global weather. The albedo effect describes how ice and snow reflect solar radiation and cool the climate. Deforestation reduces carbon absorption and lowers albedo, while fossil fuel burning increases the greenhouse effect. Volcanic eruptions can cool the climate temporarily by reflecting sunlight.
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The document discusses both long-term and short-term effects of climate change. Over millions of years, continental drift and changes in Earth's orbit have triggered changes by altering ocean currents, wind patterns, and the distribution of land masses. In the short-term, volcanic eruptions and shifts in air and ocean currents can temporarily cool the climate by blocking sunlight. The Milankovitch cycles of Earth's orbit and axial tilt occurring over tens of thousands of years are linked to recurring ice ages and interglacial periods.
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Large volcanic eruptions can cool the global climate by ejecting ash and sulfur dioxide into the stratosphere, where they reflect sunlight back into space. The 1991 eruption of Mount Pinatubo cooled the planet by 0.5°C for about a year by reducing sunlight by 10%. Even larger eruptions like Tambora in 1815 and Krakatoa in 1883 lowered global temperatures more significantly for multiple years.
Solar variation and climatic changes
This document discusses the relationship between solar variation and climatic changes. It introduces that the sun provides the energy that drives Earth's climate and any changes in the sun's output can affect the climate. It then covers topics like how solar variation is measured, records of past solar activity, the relationship between solar activity and historical climate changes like the Little Ice Age, and conclusions that the climate appears to be highly sensitive even to small changes in solar irradiance.
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This document discusses both long-term and short-term causes of climate change. Long-term causes occurring over millions of years include continental drift, changes in Earth's orbit and tilt, which affect ocean currents and temperatures. Short-term causes operating over decades to thousands of years include volcanic eruptions, which eject particles that block sunlight, and shifts in ocean and air currents driven by wind and temperature changes. Together, these natural factors have triggered shifts between ice ages and warmer periods throughout Earth's history.
Climate: Climatic Change - Evidence, Cycles and The Future
A PowerPoint used in class to cover the key forms of evidence you need to know for the Exam. Key Questions are likely to be focused on how we can gain information of past climatic change, and how it can be used to predict future, and I would expect you to be able to comment on the usefulness of the different types. For instance, Ice cores are highly accurate and quantifiable evidence, but gaining them is expensive, and only gives a climatic record for the site at which the snow formed. However, they do provide the longest record of change.
Natural causes of climate change
The Earth’s climate is dynamic and characterised by trends, aberrations and quasi-periodic oscillations varying over a broad range of time-scales [1], which are governed by external (extraterrestrial systems) and/or internal(ocean, atmosphere and land system). Trends are largely controlled by plate tectonics, and thus to change gradually on million year time scale. Aberrations occur when the certain thresholds are passed and are manifested in the geological record as the unusual rapid (less than a few thousands of years) or extreme change in climate. The quasi-periodic oscillations are mostly astronomically paced; they are driven by astronomical perturbations that affect the earth’s orbit around the sun and the orientation of earth’s rotation axis with respect to its orbital plane. These perturbations are described by the three main astronomical cycles: eccentricity, precession and obliquity, which together determine the spatial and seasonal pattern of insolation received by the earth [2], eventually resulting in climatic oscillations of ten to hundreds of thousands of year [3].Sun being the main source of energy for the earth system controls the climate of it. Variation in solar activity and cosmic ray intensity has direct influence over climatic features such as cloudiness, temperature and rainfall [4]. Volcanic eruptions also force all elements of the climatic systems up to a varying degree but producing long term climatic signals in the ocean. The cumulative volcanic cooling effect at present offsets about one third of anthropogenic warming [5].Other than these causes paleoclimatologists also relates the past climate changes with movement of solar system[6], interplanetary dusts and influence of asteroids[7].However the recent variability in climate what earth is experiencing is unlikely due to any of the individual above factors rather it is due to the compound effect of complex interactions of all the natural as well as anthropogenic forcings.
References:
1. J. C. Zachos, M. Pagani, L. Sloan, E. Thomas, K. Billups, Science 292 (2001) 686-693.
2. G. Kukla, Nature (London) 253, 600 (1975).
3. J. D. Hays, J. Imbrie, N. J. Shackleton, Science 194 (1876) 1121-1132.
4. N. Marsh, H. Swensmark, Space Sci. Rev. 94 (2000) 215-230.
5. T. L. Delworth, V. Ramaswamy, G. L. Stenchikov, Geophys. Res. Lett. 32 (2005) L24709.
6. K. Fuhrer, E. W. Wolf, S. J. Johnsen, J. Geophys. Res. 104(D24) (1999) 31043-31052
7. P. Hut, W. Alvarez, W. P. Elder, T. Hansen, E. G. Kauffman, G. Keller, E. M. Shoemaker & P. R. Weissman, Nature Vol. 329, 10 September, 1987
An Overview of the Climate System
An Overview of the Climate SystemCCAFS | CGIAR Research Program on Climate Change, Agriculture and Food Security
CCAFS workshop titled "Using Climate Scenarios and Analogues for Designing Adaptation Strategies in Agriculture," 19-23 September in Kathmandu, Nepal. Causes Of Climate Change
The document discusses several potential causes of climate change, including both natural and human factors that can lead to cooling or warming. It describes how the Milankovitch cycles have coincided with ice ages in the past. El Nino and La Nina events involve changes in ocean circulation patterns in the Pacific that impact global weather. The albedo effect describes how ice and snow reflect solar radiation and cool the climate. Deforestation reduces carbon absorption and lowers albedo, while fossil fuel burning increases the greenhouse effect. Volcanic eruptions can cool the climate temporarily by reflecting sunlight.
Long term & short term effects of climate 2
The document discusses both long-term and short-term effects of climate change. Over millions of years, continental drift and changes in Earth's orbit have triggered changes by altering ocean currents, wind patterns, and the distribution of land masses. In the short-term, volcanic eruptions and shifts in air and ocean currents can temporarily cool the climate by blocking sunlight. The Milankovitch cycles of Earth's orbit and axial tilt occurring over tens of thousands of years are linked to recurring ice ages and interglacial periods.
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The document discusses evidence that climate change has occurred in the past due to non-anthropogenic or natural causes. It provides examples from geology of past periods of glaciation and warming from factors like variations in the Earth's orbit and volcanic eruptions. While acknowledging natural climate variability, it also notes that the current pace of warming seems to be increasing due to human activity like greenhouse gas emissions. The document concludes by arguing for a comprehensive strategy to mitigate risks from climate change through renewable energy, international agreements, carbon markets and efficiency improvements.
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The document discusses long and short term changes in climate. Long term changes occurring over millions of years are influenced by continental drift and changes in Earth's orbit. Short term changes occurring over decades to thousands of years can be caused by volcanic eruptions, fluctuations in the sun's radiation, and shifts in ocean and air currents. Major long term climate shifts are also linked to variations in Earth's axial tilt, orbital shape, and the wobbling direction of its axis.
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The document discusses long and short term changes in climate. Long term changes over millions of years are caused by continental drift and changes in Earth's orbit, which affect ocean currents and heat transfer. Short term changes over decades to thousands of years can be caused by volcanic eruptions, which block sunlight, or changes in ocean currents and air currents driven by uneven heating of the Earth. The cycles of ice ages and interglacial periods that occur every 100,000 years are explained by changes in the Earth's orbit, tilt, and wobble over long time scales.
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2) The climate system includes interactions between the atmosphere, oceans, ice, land, and life. Feedback loops can amplify or reduce the effects of initial climate changes.
3) Factors that influence the climate on long timescales include variations in solar activity, volcanic eruptions, greenhouse gases, and plate tectonics. Climate has fluctuated in the past between ice ages and warmer periods.
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- Evidence from geology and fossils shows past climate changes, including intervals warmer than today and ice ages. The last ice age peaked around 20,000 years ago and glaciers have since retreated.
- Future climate is uncertain but computer models predict global warming and changing precipitation patterns if CO2 doubles from current levels due to feedbacks like ice-albedo and water vapor effects. Careful study of past and present helps understand complex climate system.
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2) Orbital cycles known as Milankovitch cycles, which cause ice ages and warm interglacial periods over 100,000 year cycles.
3) Large volcanic eruptions, which eject aerosols that reflect sunlight and cause short-term global cooling lasting several years.
4) Ocean circulation patterns, with changes potentially causing Europe to be 6-8°C cooler during glacial periods due to reductions in the
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2) Evidence of past climate changes is seen in temperature and carbon dioxide variations from ice cores, glacial activity, sea levels, and vegetation changes.
3) The author argues that climate change is a natural phenomenon and that the role of human-caused carbon dioxide emissions in current warming is limited and uncertain.
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The document discusses several factors that influence Earth's climate:
1) Solar energy is the main driver of climate, affecting global temperatures as it is absorbed by the atmosphere, oceans, and land.
2) Other factors like Earth's orbit, axial tilt, and rotation influence the distribution of solar radiation and cause seasonal changes.
3) Large bodies of water like oceans influence climate by slowly storing and transferring heat around the world.
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The document discusses long and short term changes in climate. Long term changes over millions of years are caused by continental drift and changes in Earth's orbit, which affect ocean currents and heat transfer. Short term changes over decades to thousands of years can be caused by volcanic eruptions, which block sunlight, or changes in ocean currents and air currents driven by uneven heating of the Earth. The cycles of ice ages and interglacial periods that occur every 100,000 years are explained by changes in the Earth's orbit, tilt, and wobble over long time scales.
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The document discusses key concepts about the Earth's climate system:
1) Climate is the long-term average weather conditions in an area, while weather describes short-term conditions. Various mechanisms can cause climate change over different timescales.
2) The climate system includes interactions between the atmosphere, oceans, ice, land, and life. Feedback loops can amplify or reduce the effects of initial climate changes.
3) Factors that influence the climate on long timescales include variations in solar activity, volcanic eruptions, greenhouse gases, and plate tectonics. Climate has fluctuated in the past between ice ages and warmer periods.
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- Climate change occurs on various timescales and is influenced by factors like solar activity, Earth's orbit, atmospheric composition and greenhouse gases, volcanic eruptions, and human activities like fossil fuel burning.
- Evidence from geology and fossils shows past climate changes, including intervals warmer than today and ice ages. The last ice age peaked around 20,000 years ago and glaciers have since retreated.
- Future climate is uncertain but computer models predict global warming and changing precipitation patterns if CO2 doubles from current levels due to feedbacks like ice-albedo and water vapor effects. Careful study of past and present helps understand complex climate system.
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The document discusses several natural causes of past climate change:
1) Solar activity, with periods of lower sunspot activity corresponding to "Little Ice Ages" and higher activity to warm periods like the Medieval Warm Period. However, solar activity does not correlate with warming since 1975.
2) Orbital cycles known as Milankovitch cycles, which cause ice ages and warm interglacial periods over 100,000 year cycles.
3) Large volcanic eruptions, which eject aerosols that reflect sunlight and cause short-term global cooling lasting several years.
4) Ocean circulation patterns, with changes potentially causing Europe to be 6-8°C cooler during glacial periods due to reductions in the
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Methane is produced through methanogenesis by archaea in anaerobic conditions and some diffuses into the atmosphere. Peatlands contain large amounts of sequestered carbon as peat forms from partially decomposed organic matter in waterlogged soils. Over geological eras, partially decomposed organic matter was converted into fossil fuels like oil and gas or coal. Combustion of fossil fuels releases carbon dioxide and water. Corals and mollusks incorporate carbonate into their shells, acting as an aquatic carbon sink. There is a strong correlation between increases in greenhouse gases like carbon dioxide and global temperature increases.
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Climate change is a significant and lasting change in the statistical distribution of weather patterns over periods ranging from decades to millions of years. It may be a change in average weather conditions, or in the distribution of weather around the average conditions (i.e., more or fewer extreme weather events). Climate change is caused by factors such as biotic processes, variations in solar radiation received by Earth, plate tectonics, and volcanic eruptions. Certain human activities have also been identified as significant causes of recent climate change, often referred to as "global warming"
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Climate_Change_ppt.ppt
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Intro to Meteorology: Our Atmosphere
Here are the answers to your questions:
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Climate ChangeInvestigation ManualENVIRONMENTAL SCIENC
Climate Change
Investigation
Manual
ENVIRONMENTAL SCIENCE
CLIMATE CHANGE
Overview
In this lab, students will carry out several activities aimed at
demonstrating consequences of anthropogenic carbon emissions,
climate change, and sea level rise. To do this, students will model
how certain gases in Earth’s atmosphere trap heat and then how
different colors and textures of surfaces reflect differing amounts
of sunlight back into space. They will create models of sea level
rise resulting from melting of sea ice and glacial ice and examine
the effects of this potential consequence of climate change.
Students will critically examine the model systems they used in
the experiments.
Outcomes
• Explain the causes of increased carbon emissions and their likely
effect on global climate.
• Discuss positive and negative climate feedback.
• Distinguish between glacial ice melt and oceanic ice melt.
Time Requirements
Preparation ..................................................................... 15 minutes
Activity 1: Modeling the Greenhouse Effect ................... 30 minutes
Activity 2: Modeling Albedo ........................................... 40 minutes
Activity 3: Sea Ice, Glacial Ice, and Sea Level Rise ....... 30 minutes
2 Carolina Distance Learning
Key
Personal protective
equipment
(PPE)
goggles gloves apron
follow
link to
video
photograph
results and
submit
stopwatch
required
warning corrosion flammable toxic environment health hazard
Made ADA compliant by
NetCentric Technologies using
the CommonLook® software
Table of Contents
2 Overview
2 Outcomes
2 Time Requirements
3 Background
9 Materials
9 Safety
9 Preparation
10 Activity 1
11 Activity 2
12 Activity 3
13 Graphing
13 Submission
13 Disposal and Cleanup
14 Lab Worksheet
Background
For the last 30 years, controversy has
surrounded the ideas of global warming/climate
change. However, the scientific concepts behind
the theory are not new. In the 1820s, Joseph
Fourier was the first to recognize that, given
the earth’s size and distance from the sun,
the planet’s surface temperature should be
considerably cooler than it was. He proposed
several mechanisms to explain why the earth
was warmer than his calculations predicted,
one of which was that the earth’s atmosphere
might act as an insulator. Forty years later,
John Tyndall demonstrated that different
gases have different capacities to absorb
infrared radiation, most notably methane (CH4),
carbon dioxide (CO2), and water vapor (H2O),
all of which are present in the atmosphere. In
1896, Svante Arrhenius developed the first
mathematical model of the effect of increased
CO2 levels on temperature. His model predicted
that a doubling of the amount of CO2 in the
atmosphere would produce a 5–6 °C increase
in temperature globally. Based on the level of
CO2 production in the late 19th century, he
predicted that this change would take place
over thousands of years, if at ...
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The document discusses how Milankovitch cycles have driven climate changes on Earth throughout geological history. It explains that Milankovitch cycles are variations in Earth's eccentricity, axial tilt, and precession that influence the amount of solar radiation received in different locations over long time periods. Specifically, it notes that periods of low eccentricity and tilt are linked to glacial periods, while high eccentricity and tilt encourage interglacial phases. When all three factors are aligned to point towards a warmer or colder Earth, peak glacial or interglacial periods are reached. The combined effects of these orbital variations are thought to be responsible for the cyclical glacial and interglacial periods seen in Earth's climate
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Climate change occurs over short, medium, and long timescales. Short-term climate change involves global warming over decades, while medium-term changes occurred over thousands of years according to ice core and fossil records. Long-term changes shaped climate over hundreds of thousands to millions of years. Recent climate change has led to 0.5°C warming globally since 1970 due to increased greenhouse gas emissions from human activities like burning fossil fuels. This enhanced greenhouse effect from carbon dioxide and methane emissions is trapping more heat in the atmosphere and causing unprecedented global warming according to temperature and Arctic sea ice records.
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Columbus Data & Analytics Wednesdays - June 2024
Columbus Data & Analytics Wednesdays, June 2024 with Maria Copot 20
Digital Marketing Trends in 2024 | Guide for Staying Ahead
https://www.wask.co/ebooks/digital-marketing-trends-in-2024
Feeling lost in the digital marketing whirlwind of 2024? Technology is changing, consumer habits are evolving, and staying ahead of the curve feels like a never-ending pursuit. This e-book is your compass. Dive into actionable insights to handle the complexities of modern marketing. From hyper-personalization to the power of user-generated content, learn how to build long-term relationships with your audience and unlock the secrets to success in the ever-shifting digital landscape.
June Patch Tuesday
Ivanti’s Patch Tuesday breakdown goes beyond patching your applications and brings you the intelligence and guidance needed to prioritize where to focus your attention first. Catch early analysis on our Ivanti blog, then join industry expert Chris Goettl for the Patch Tuesday Webinar Event. There we’ll do a deep dive into each of the bulletins and give guidance on the risks associated with the newly-identified vulnerabilities.
Finale of the Year: Apply for Next One!
Presentation for the event called "Finale of the Year: Apply for Next One!" organized by GDSC PJATK
Your One-Stop Shop for Python Success: Top 10 US Python Development Providers
Simplify your search for a reliable Python development partner! This list presents the top 10 trusted US providers offering comprehensive Python development services, ensuring your project's success from conception to completion.
Best 20 SEO Techniques To Improve Website Visibility In SERP
Boost your website's visibility with proven SEO techniques! Our latest blog dives into essential strategies to enhance your online presence, increase traffic, and rank higher on search engines. From keyword optimization to quality content creation, learn how to make your site stand out in the crowded digital landscape. Discover actionable tips and expert insights to elevate your SEO game.
AWS Cloud Cost Optimization Presentation.pptx
This presentation provides valuable insights into effective cost-saving techniques on AWS. Learn how to optimize your AWS resources by rightsizing, increasing elasticity, picking the right storage class, and choosing the best pricing model. Additionally, discover essential governance mechanisms to ensure continuous cost efficiency. Whether you are new to AWS or an experienced user, this presentation provides clear and practical tips to help you reduce your cloud costs and get the most out of your budget.
System Design Case Study: Building a Scalable E-Commerce Platform - Hiike
This case study explores designing a scalable e-commerce platform, covering key requirements, system components, and best practices.
Skybuffer AI: Advanced Conversational and Generative AI Solution on SAP Busin...
Skybuffer AI, built on the robust SAP Business Technology Platform (SAP BTP), is the latest and most advanced version of our AI development, reaffirming our commitment to delivering top-tier AI solutions. Skybuffer AI harnesses all the innovative capabilities of the SAP BTP in the AI domain, from Conversational AI to cutting-edge Generative AI and Retrieval-Augmented Generation (RAG). It also helps SAP customers safeguard their investments into SAP Conversational AI and ensure a seamless, one-click transition to SAP Business AI.
With Skybuffer AI, various AI models can be integrated into a single communication channel such as Microsoft Teams. This integration empowers business users with insights drawn from SAP backend systems, enterprise documents, and the expansive knowledge of Generative AI. And the best part of it is that it is all managed through our intuitive no-code Action Server interface, requiring no extensive coding knowledge and making the advanced AI accessible to more users.
HCL Notes and Domino License Cost Reduction in the World of DLAU
Webinar Recording: https://www.panagenda.com/webinars/hcl-notes-and-domino-license-cost-reduction-in-the-world-of-dlau/
The introduction of DLAU and the CCB & CCX licensing model caused quite a stir in the HCL community. As a Notes and Domino customer, you may have faced challenges with unexpected user counts and license costs. You probably have questions on how this new licensing approach works and how to benefit from it. Most importantly, you likely have budget constraints and want to save money where possible. Don’t worry, we can help with all of this!
We’ll show you how to fix common misconfigurations that cause higher-than-expected user counts, and how to identify accounts which you can deactivate to save money. There are also frequent patterns that can cause unnecessary cost, like using a person document instead of a mail-in for shared mailboxes. We’ll provide examples and solutions for those as well. And naturally we’ll explain the new licensing model.
Join HCL Ambassador Marc Thomas in this webinar with a special guest appearance from Franz Walder. It will give you the tools and know-how to stay on top of what is going on with Domino licensing. You will be able lower your cost through an optimized configuration and keep it low going forward.
These topics will be covered
- Reducing license cost by finding and fixing misconfigurations and superfluous accounts
- How do CCB and CCX licenses really work?
- Understanding the DLAU tool and how to best utilize it
- Tips for common problem areas, like team mailboxes, functional/test users, etc
- Practical examples and best practices to implement right away
Main news related to the CCS TSI 2023 (2023/1695)
An English 🇬🇧 translation of a presentation to the speech I gave about the main changes brought by CCS TSI 2023 at the biggest Czech conference on Communications and signalling systems on Railways, which was held in Clarion Hotel Olomouc from 7th to 9th November 2023 (konferenceszt.cz). Attended by around 500 participants and 200 on-line followers.
The original Czech 🇨🇿 version of the presentation can be found here: https://www.slideshare.net/slideshow/hlavni-novinky-souvisejici-s-ccs-tsi-2023-2023-1695/269688092 .
The videorecording (in Czech) from the presentation is available here: https://youtu.be/WzjJWm4IyPk?si=SImb06tuXGb30BEH .
A Comprehensive Guide to DeFi Development Services in 2024
DeFi represents a paradigm shift in the financial industry. Instead of relying on traditional, centralized institutions like banks, DeFi leverages blockchain technology to create a decentralized network of financial services. This means that financial transactions can occur directly between parties, without intermediaries, using smart contracts on platforms like Ethereum.
In 2024, we are witnessing an explosion of new DeFi projects and protocols, each pushing the boundaries of what’s possible in finance.
In summary, DeFi in 2024 is not just a trend; it’s a revolution that democratizes finance, enhances security and transparency, and fosters continuous innovation. As we proceed through this presentation, we'll explore the various components and services of DeFi in detail, shedding light on how they are transforming the financial landscape.
At Intelisync, we specialize in providing comprehensive DeFi development services tailored to meet the unique needs of our clients. From smart contract development to dApp creation and security audits, we ensure that your DeFi project is built with innovation, security, and scalability in mind. Trust Intelisync to guide you through the intricate landscape of decentralized finance and unlock the full potential of blockchain technology.
Ready to take your DeFi project to the next level? Partner with Intelisync for expert DeFi development services today!
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Why Does Climate Change
- 1. Why does climate change?
- 5. This graph suggests that sunspot activity might be a factor in temperature change (– but be careful – graph only covers a short period of time)
- 8. Since the 1850s, there has been a rapid rise in temperatures – and human activities are being blamed for this… but that’s the next instalment!