SlideShare uma empresa Scribd logo
1 de 38
Long Term & Short Term Effects of Climate Change By: Sarah Ramanathan  Keiran Alam Chantal Liu Manal Rahim
For the past millions of years, our climate has had many significant changes.  Changes in Earth's climate are triggered by changes in Earth's energy balance.  Long term changes: - continental drift - changes in Earth's orbit Short term changes: - Volcanic eruptions - Air and Ocean Currents 
Long Term Changes in climate(millions of years- hundreds of thousands of years) Chantal & Manal
Plate Tectonics = Theory of explaining slow movement of large plates of Earth's crust Continental Drift - Theory that Earth's continents used to be one supercontinent named Pangaea. 225 Million years ago: Pangaea (Permian period) Changes Due to Continental Drift
200 Million years ago: Laragia and Gondwanaland (Triassic period) 135 Million years ago: Jurassic period 65 Million years ago: Creations period.
Continents move = ocean currents and wind patterns change 	- Affects heat transfer Affects distribution of land mass 	- Nothern Hemisphere (includes Canada) has most land mass.
	- Fewer large bodies of water = coldest winters & warmest summers 	- More large bodies of water in Southern hemisphere = more moderate climate 	- Temperatures weren't like this in Permian period
More mountains (caused by movement of Earth's plates) affects Local & regional climates Wearing of mountains over time can also cause regional climate change 	- These changes have occurred in Canada because we have new and old mountain 	regions such as the Rockies and Appalachians.
Scientists have found that over time the energy the Sun produces over time can also change Changes of area cause complications in production of CO2 	- CO2 porduced in volcanoes & mid-ocean trenches. 		-> Lost by slowly being absorbed into oceans 		-> Areas w/ high overall temperature most likely had greenhouse warming due to 		volcanic CO2
Long-Term Cycles in Climate 20 000 years ago, Earth had last ice age. 	- Temp was 10 degrees lower than today 	- Canada covered in ice sheet 3 km thick 	- Sea levels dropped as oceans froze over 		-> Land under oceans were exposed, revealing hidden bridges to continents
		-> Animals crossed over to new habitats Major changes in temp happen in regular cycles (page 349 of textbook) 	-warm interglacial periods occur every 100 000 years Interglacial Period - Time between ice ages when Earth warms up
Changes That Occur Over Hundreds Of Thousands Of Years: The Recurrence of Interglacial Periods and Ice Ages every 100,000 years, interglacial periods and ice ages occur Ice age (glacial period): long term reduction of Earth’s temperature = glaciers and ice sheets covering Earth
Interglacial periods: period of warmer temperature that separates periods of time in an ice age Interglacial periods involve movements of glaciers Causes temperatures to keep rising and falling depending on whether glaciers are advancing or retreating
Why these Interglacial Periods &Ice Ages Keep Happening?  Engineer/astronomer Milutin Milankovitch developed theory on reason for these climate changes  Earth’s orbit around sun changes on three main ways/cycles: Eccentricity (changing shape) of Earth’s orbit Earth’s  Tilt Direction (wobble) of tilt
Eccentricity of the Earth’s orbit Shape of Earth’s orbit around sun changes  Goes from almost circular to more elliptical (flattened circle/oval-like)
Caused by Jupiter and Saturn’s gravities Occurs approximately every 100,000 years Earth’s current cycle is more elliptical (oval-like)
Earth’s Tilt Earth’s current tilt = 23.5 degrees Earth’s tilt is responsible for its changes in seasons
Scientists believe that changes in Earth’s tilt are cause for glacial cycles occurring When Earth’s tilt is larger (closer to its 24.5 degrees max): Glaciations end Causes warmer summers Earth’s tilt currently decreasing
In a cycle close to 42,000 years, Earth tilts back and forth on its axis from 22.1 degrees to 24.5 degrees
Direction (wobble) of tilt (Axial Precession) In order to grasp the idea, think of a spinning top
As it spins, it wobbles around/changes direction while spinning on same point Earth’s tilt is similar As Earth’s spins on its axis, it slowly wobbles The angle of its tilt remains approximately the same but its directions changes Cycle of roughly 26,000 years
Short Term Changes in climate (decades-thousands of years) Sarah & Keiran
Volcanic Eruptions Volcanic eruptions can cause Earth’s climate to change temporarily rocks, dust, and gases are sent out high into atmosphere.
Suns energy reflects back out to space (from sulfur dioxide particles)  Earth’s surface shaded. Amount of cooling depends on amount of dust put in air, and time of cooling-on size of particles.
Ocean Currents Uneven heating of Earth causes convection currents that create prevailing winds and ocean currents.  Ocean currents have a strong effect on climates of nearby land Ocean currents can be caused by winds Cold ocean currents cool air above  Warm ocean currents heat air above
The global conveyor belt begins around the North Pole and then works its way down, traveling through all of the oceans before circling back Ocean currents can have a major effect on the weather
Air Currents Air on Earth's surface is in constant motion called air currents Air currents affect air quality and ocean currents, and weather conditions Air currents caused by three main processes:  ,[object Object]
Impurities
pressure. ,[object Object]
Changes in Sun’s Radiation suns radiation amount drops, Earth gets less energy (less heat =Earth cools down) suns radiation higher=more energy No scientific reason yet why radiation     and     over shorter time scales.
Thank You
Bibliography Nelson Science Perspectives 10 Nelson Education Ltd. 2010 Pages 348-353 <http://ircamera.as.arizona.edu/NatSci102/NatSci102/lectures/climate.htm>. Windows to the Universe 2010 National Earth Science Teachers Association  200-2011 http://www.windows2universe.org/earth/climate/cli_seasons.html Woods Hole Oceanographic Institution Shelley Dawicki March 28, 2005 http://www.whoi.edu/page.do?pid=9779&tid=282&cid=3638&ct=162 Long term climate hypertext   G. H. Rieke http://ircamera.as.arizona.edu/NatSci102/NatSci102/lectures/climate.htm

Mais conteúdo relacionado

Mais procurados

Global climate change
Global climate changeGlobal climate change
Global climate change
jparker9
 
El nino & la nina tam 2013-22
El nino & la nina tam 2013-22El nino & la nina tam 2013-22
El nino & la nina tam 2013-22
Vijay Kumar
 
Greenhouse Effect Power Point
Greenhouse Effect Power PointGreenhouse Effect Power Point
Greenhouse Effect Power Point
hilli1sm
 
Structure and Composition of the Atmosphere
Structure and Composition of the AtmosphereStructure and Composition of the Atmosphere
Structure and Composition of the Atmosphere
beaudry2011
 
Greenhouse Gases
Greenhouse GasesGreenhouse Gases
Greenhouse Gases
OhMiss
 

Mais procurados (20)

Global climate change
Global climate changeGlobal climate change
Global climate change
 
Final the albedo effect
Final  the albedo effectFinal  the albedo effect
Final the albedo effect
 
Weather and climate: basic concepts
Weather and climate: basic conceptsWeather and climate: basic concepts
Weather and climate: basic concepts
 
Climate Change 2016
Climate Change 2016Climate Change 2016
Climate Change 2016
 
Energy resources
Energy resourcesEnergy resources
Energy resources
 
General circulation model
General circulation modelGeneral circulation model
General circulation model
 
Climate change
Climate changeClimate change
Climate change
 
El nino & la nina tam 2013-22
El nino & la nina tam 2013-22El nino & la nina tam 2013-22
El nino & la nina tam 2013-22
 
Air Pressure
Air PressureAir Pressure
Air Pressure
 
Winds and Wind System
Winds and Wind SystemWinds and Wind System
Winds and Wind System
 
Greenhouse Effect Power Point
Greenhouse Effect Power PointGreenhouse Effect Power Point
Greenhouse Effect Power Point
 
Structure and Composition of the Atmosphere
Structure and Composition of the AtmosphereStructure and Composition of the Atmosphere
Structure and Composition of the Atmosphere
 
Climate change
Climate changeClimate change
Climate change
 
Solar radiation
Solar radiationSolar radiation
Solar radiation
 
Global air circulation
Global air circulationGlobal air circulation
Global air circulation
 
Greenhouse gases and their effect
Greenhouse gases and their effectGreenhouse gases and their effect
Greenhouse gases and their effect
 
THE ATMOSPHERE. WEATHER AND CLIMATE
THE ATMOSPHERE. WEATHER AND CLIMATETHE ATMOSPHERE. WEATHER AND CLIMATE
THE ATMOSPHERE. WEATHER AND CLIMATE
 
Types of erosion
Types of erosionTypes of erosion
Types of erosion
 
Greenhouse Gases
Greenhouse GasesGreenhouse Gases
Greenhouse Gases
 
Seasons
Seasons Seasons
Seasons
 

Semelhante a Long term & short term effects of climate

Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
Sarah Ramanathan
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
Sarah Ramanathan
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
Sarah Ramanathan
 
Climate changes past and future
Climate changes  past and futureClimate changes  past and future
Climate changes past and future
DocumentStory
 
Natural causes of climate change
Natural causes of climate changeNatural causes of climate change
Natural causes of climate change
debasishagri
 
Earth's Climate
Earth's ClimateEarth's Climate
Earth's Climate
OhMiss
 
Science climate project
Science climate projectScience climate project
Science climate project
nashmiya
 
Science climate project
Science climate projectScience climate project
Science climate project
nashmiya
 
Climatesystem 100427220733-phpapp02
Climatesystem 100427220733-phpapp02Climatesystem 100427220733-phpapp02
Climatesystem 100427220733-phpapp02
mjasdan
 
Climate System
Climate SystemClimate System
Climate System
Ed Stermer
 

Semelhante a Long term & short term effects of climate (20)

Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
 
Long term & short term effects of climate 2
Long term & short term effects of climate 2Long term & short term effects of climate 2
Long term & short term effects of climate 2
 
Climate_Change_ppt.ppt
Climate_Change_ppt.pptClimate_Change_ppt.ppt
Climate_Change_ppt.ppt
 
Climate changes past and future
Climate changes  past and futureClimate changes  past and future
Climate changes past and future
 
Natural causes of climate change
Natural causes of climate changeNatural causes of climate change
Natural causes of climate change
 
Earth's Climate
Earth's ClimateEarth's Climate
Earth's Climate
 
Science climate project
Science climate projectScience climate project
Science climate project
 
Science climate project
Science climate projectScience climate project
Science climate project
 
Weather.climate edited
Weather.climate editedWeather.climate edited
Weather.climate edited
 
Climate Notes PowerPoint
Climate Notes PowerPointClimate Notes PowerPoint
Climate Notes PowerPoint
 
Chapt15 lecture
Chapt15 lectureChapt15 lecture
Chapt15 lecture
 
Climatesystem 100427220733-phpapp02
Climatesystem 100427220733-phpapp02Climatesystem 100427220733-phpapp02
Climatesystem 100427220733-phpapp02
 
Climate System
Climate SystemClimate System
Climate System
 
SALDIVAR_CLIMATE- AND ITS FACTORS. .pptx
SALDIVAR_CLIMATE- AND ITS FACTORS. .pptxSALDIVAR_CLIMATE- AND ITS FACTORS. .pptx
SALDIVAR_CLIMATE- AND ITS FACTORS. .pptx
 
Animal climatology
Animal climatologyAnimal climatology
Animal climatology
 
Animal climatology
Animal climatologyAnimal climatology
Animal climatology
 
Theory of climate change (kiran thorat)
Theory of climate change (kiran thorat)Theory of climate change (kiran thorat)
Theory of climate change (kiran thorat)
 
Orbital variations
Orbital variationsOrbital variations
Orbital variations
 
Ch 15 ed
Ch 15 edCh 15 ed
Ch 15 ed
 

Último

IAC 2024 - IA Fast Track to Search Focused AI Solutions
IAC 2024 - IA Fast Track to Search Focused AI SolutionsIAC 2024 - IA Fast Track to Search Focused AI Solutions
IAC 2024 - IA Fast Track to Search Focused AI Solutions
Enterprise Knowledge
 

Último (20)

[2024]Digital Global Overview Report 2024 Meltwater.pdf
[2024]Digital Global Overview Report 2024 Meltwater.pdf[2024]Digital Global Overview Report 2024 Meltwater.pdf
[2024]Digital Global Overview Report 2024 Meltwater.pdf
 
04-2024-HHUG-Sales-and-Marketing-Alignment.pptx
04-2024-HHUG-Sales-and-Marketing-Alignment.pptx04-2024-HHUG-Sales-and-Marketing-Alignment.pptx
04-2024-HHUG-Sales-and-Marketing-Alignment.pptx
 
Handwritten Text Recognition for manuscripts and early printed texts
Handwritten Text Recognition for manuscripts and early printed textsHandwritten Text Recognition for manuscripts and early printed texts
Handwritten Text Recognition for manuscripts and early printed texts
 
Powerful Google developer tools for immediate impact! (2023-24 C)
Powerful Google developer tools for immediate impact! (2023-24 C)Powerful Google developer tools for immediate impact! (2023-24 C)
Powerful Google developer tools for immediate impact! (2023-24 C)
 
TrustArc Webinar - Stay Ahead of US State Data Privacy Law Developments
TrustArc Webinar - Stay Ahead of US State Data Privacy Law DevelopmentsTrustArc Webinar - Stay Ahead of US State Data Privacy Law Developments
TrustArc Webinar - Stay Ahead of US State Data Privacy Law Developments
 
Raspberry Pi 5: Challenges and Solutions in Bringing up an OpenGL/Vulkan Driv...
Raspberry Pi 5: Challenges and Solutions in Bringing up an OpenGL/Vulkan Driv...Raspberry Pi 5: Challenges and Solutions in Bringing up an OpenGL/Vulkan Driv...
Raspberry Pi 5: Challenges and Solutions in Bringing up an OpenGL/Vulkan Driv...
 
From Event to Action: Accelerate Your Decision Making with Real-Time Automation
From Event to Action: Accelerate Your Decision Making with Real-Time AutomationFrom Event to Action: Accelerate Your Decision Making with Real-Time Automation
From Event to Action: Accelerate Your Decision Making with Real-Time Automation
 
Advantages of Hiring UIUX Design Service Providers for Your Business
Advantages of Hiring UIUX Design Service Providers for Your BusinessAdvantages of Hiring UIUX Design Service Providers for Your Business
Advantages of Hiring UIUX Design Service Providers for Your Business
 
The Codex of Business Writing Software for Real-World Solutions 2.pptx
The Codex of Business Writing Software for Real-World Solutions 2.pptxThe Codex of Business Writing Software for Real-World Solutions 2.pptx
The Codex of Business Writing Software for Real-World Solutions 2.pptx
 
IAC 2024 - IA Fast Track to Search Focused AI Solutions
IAC 2024 - IA Fast Track to Search Focused AI SolutionsIAC 2024 - IA Fast Track to Search Focused AI Solutions
IAC 2024 - IA Fast Track to Search Focused AI Solutions
 
Factors to Consider When Choosing Accounts Payable Services Providers.pptx
Factors to Consider When Choosing Accounts Payable Services Providers.pptxFactors to Consider When Choosing Accounts Payable Services Providers.pptx
Factors to Consider When Choosing Accounts Payable Services Providers.pptx
 
GenCyber Cyber Security Day Presentation
GenCyber Cyber Security Day PresentationGenCyber Cyber Security Day Presentation
GenCyber Cyber Security Day Presentation
 
What Are The Drone Anti-jamming Systems Technology?
What Are The Drone Anti-jamming Systems Technology?What Are The Drone Anti-jamming Systems Technology?
What Are The Drone Anti-jamming Systems Technology?
 
Tata AIG General Insurance Company - Insurer Innovation Award 2024
Tata AIG General Insurance Company - Insurer Innovation Award 2024Tata AIG General Insurance Company - Insurer Innovation Award 2024
Tata AIG General Insurance Company - Insurer Innovation Award 2024
 
Mastering MySQL Database Architecture: Deep Dive into MySQL Shell and MySQL R...
Mastering MySQL Database Architecture: Deep Dive into MySQL Shell and MySQL R...Mastering MySQL Database Architecture: Deep Dive into MySQL Shell and MySQL R...
Mastering MySQL Database Architecture: Deep Dive into MySQL Shell and MySQL R...
 
08448380779 Call Girls In Greater Kailash - I Women Seeking Men
08448380779 Call Girls In Greater Kailash - I Women Seeking Men08448380779 Call Girls In Greater Kailash - I Women Seeking Men
08448380779 Call Girls In Greater Kailash - I Women Seeking Men
 
Strategies for Unlocking Knowledge Management in Microsoft 365 in the Copilot...
Strategies for Unlocking Knowledge Management in Microsoft 365 in the Copilot...Strategies for Unlocking Knowledge Management in Microsoft 365 in the Copilot...
Strategies for Unlocking Knowledge Management in Microsoft 365 in the Copilot...
 
Bajaj Allianz Life Insurance Company - Insurer Innovation Award 2024
Bajaj Allianz Life Insurance Company - Insurer Innovation Award 2024Bajaj Allianz Life Insurance Company - Insurer Innovation Award 2024
Bajaj Allianz Life Insurance Company - Insurer Innovation Award 2024
 
Data Cloud, More than a CDP by Matt Robison
Data Cloud, More than a CDP by Matt RobisonData Cloud, More than a CDP by Matt Robison
Data Cloud, More than a CDP by Matt Robison
 
Boost Fertility New Invention Ups Success Rates.pdf
Boost Fertility New Invention Ups Success Rates.pdfBoost Fertility New Invention Ups Success Rates.pdf
Boost Fertility New Invention Ups Success Rates.pdf
 

Long term & short term effects of climate

  • 1. Long Term & Short Term Effects of Climate Change By: Sarah Ramanathan Keiran Alam Chantal Liu Manal Rahim
  • 2. For the past millions of years, our climate has had many significant changes.  Changes in Earth's climate are triggered by changes in Earth's energy balance.  Long term changes: - continental drift - changes in Earth's orbit Short term changes: - Volcanic eruptions - Air and Ocean Currents 
  • 3. Long Term Changes in climate(millions of years- hundreds of thousands of years) Chantal & Manal
  • 4. Plate Tectonics = Theory of explaining slow movement of large plates of Earth's crust Continental Drift - Theory that Earth's continents used to be one supercontinent named Pangaea. 225 Million years ago: Pangaea (Permian period) Changes Due to Continental Drift
  • 5. 200 Million years ago: Laragia and Gondwanaland (Triassic period) 135 Million years ago: Jurassic period 65 Million years ago: Creations period.
  • 6.
  • 7.
  • 8. Continents move = ocean currents and wind patterns change - Affects heat transfer Affects distribution of land mass - Nothern Hemisphere (includes Canada) has most land mass.
  • 9. - Fewer large bodies of water = coldest winters & warmest summers - More large bodies of water in Southern hemisphere = more moderate climate - Temperatures weren't like this in Permian period
  • 10. More mountains (caused by movement of Earth's plates) affects Local & regional climates Wearing of mountains over time can also cause regional climate change - These changes have occurred in Canada because we have new and old mountain regions such as the Rockies and Appalachians.
  • 11. Scientists have found that over time the energy the Sun produces over time can also change Changes of area cause complications in production of CO2 - CO2 porduced in volcanoes & mid-ocean trenches. -> Lost by slowly being absorbed into oceans -> Areas w/ high overall temperature most likely had greenhouse warming due to volcanic CO2
  • 12. Long-Term Cycles in Climate 20 000 years ago, Earth had last ice age. - Temp was 10 degrees lower than today - Canada covered in ice sheet 3 km thick - Sea levels dropped as oceans froze over -> Land under oceans were exposed, revealing hidden bridges to continents
  • 13. -> Animals crossed over to new habitats Major changes in temp happen in regular cycles (page 349 of textbook) -warm interglacial periods occur every 100 000 years Interglacial Period - Time between ice ages when Earth warms up
  • 14. Changes That Occur Over Hundreds Of Thousands Of Years: The Recurrence of Interglacial Periods and Ice Ages every 100,000 years, interglacial periods and ice ages occur Ice age (glacial period): long term reduction of Earth’s temperature = glaciers and ice sheets covering Earth
  • 15. Interglacial periods: period of warmer temperature that separates periods of time in an ice age Interglacial periods involve movements of glaciers Causes temperatures to keep rising and falling depending on whether glaciers are advancing or retreating
  • 16.
  • 17. Why these Interglacial Periods &Ice Ages Keep Happening?  Engineer/astronomer Milutin Milankovitch developed theory on reason for these climate changes Earth’s orbit around sun changes on three main ways/cycles: Eccentricity (changing shape) of Earth’s orbit Earth’s Tilt Direction (wobble) of tilt
  • 18. Eccentricity of the Earth’s orbit Shape of Earth’s orbit around sun changes Goes from almost circular to more elliptical (flattened circle/oval-like)
  • 19. Caused by Jupiter and Saturn’s gravities Occurs approximately every 100,000 years Earth’s current cycle is more elliptical (oval-like)
  • 20. Earth’s Tilt Earth’s current tilt = 23.5 degrees Earth’s tilt is responsible for its changes in seasons
  • 21. Scientists believe that changes in Earth’s tilt are cause for glacial cycles occurring When Earth’s tilt is larger (closer to its 24.5 degrees max): Glaciations end Causes warmer summers Earth’s tilt currently decreasing
  • 22. In a cycle close to 42,000 years, Earth tilts back and forth on its axis from 22.1 degrees to 24.5 degrees
  • 23. Direction (wobble) of tilt (Axial Precession) In order to grasp the idea, think of a spinning top
  • 24. As it spins, it wobbles around/changes direction while spinning on same point Earth’s tilt is similar As Earth’s spins on its axis, it slowly wobbles The angle of its tilt remains approximately the same but its directions changes Cycle of roughly 26,000 years
  • 25.
  • 26. Short Term Changes in climate (decades-thousands of years) Sarah & Keiran
  • 27. Volcanic Eruptions Volcanic eruptions can cause Earth’s climate to change temporarily rocks, dust, and gases are sent out high into atmosphere.
  • 28.
  • 29.
  • 30. Suns energy reflects back out to space (from sulfur dioxide particles) Earth’s surface shaded. Amount of cooling depends on amount of dust put in air, and time of cooling-on size of particles.
  • 31. Ocean Currents Uneven heating of Earth causes convection currents that create prevailing winds and ocean currents. Ocean currents have a strong effect on climates of nearby land Ocean currents can be caused by winds Cold ocean currents cool air above Warm ocean currents heat air above
  • 32. The global conveyor belt begins around the North Pole and then works its way down, traveling through all of the oceans before circling back Ocean currents can have a major effect on the weather
  • 33.
  • 35.
  • 36. Changes in Sun’s Radiation suns radiation amount drops, Earth gets less energy (less heat =Earth cools down) suns radiation higher=more energy No scientific reason yet why radiation and over shorter time scales.
  • 38. Bibliography Nelson Science Perspectives 10 Nelson Education Ltd. 2010 Pages 348-353 <http://ircamera.as.arizona.edu/NatSci102/NatSci102/lectures/climate.htm>. Windows to the Universe 2010 National Earth Science Teachers Association 200-2011 http://www.windows2universe.org/earth/climate/cli_seasons.html Woods Hole Oceanographic Institution Shelley Dawicki March 28, 2005 http://www.whoi.edu/page.do?pid=9779&tid=282&cid=3638&ct=162 Long term climate hypertext   G. H. Rieke http://ircamera.as.arizona.edu/NatSci102/NatSci102/lectures/climate.htm
  • 39. Pictures: Long term climate hypertext   G. H. Rieke http://ircamera.as.arizona.edu/NatSci102/NatSi102/lectures/climate.htm http://www.phy6.org/stargcc/Sconcat2.htm http://room106vjh2.blogspot.com/2010_09_01_archive.html Black, Ken. "How does Ocean Temperature affect Air Temperature?" WiseGeek. Web. 10 Jan 2011. Capital Regional District. "Global Ocean Currents.". Web. 10 Jan 2011. Hayhoe, Christy, Douglas and Katharine. Energy Transfer within the Climate System: Air and Ocean Circulation. Perspectives 10. Canada: Nelson Eduacation Ltd, 2010. 344-348. Print. Exploring the environment Wheeling Jesuit University/NASA-supported Classroom of the Future September 30, 2010 http://www.cotf.edu/ete/modules/volcanoes/vclimate.html