Enviar pesquisa
Carregar
Climate System
•
Transferir como PPT, PDF
•
12 gostaram
•
11,768 visualizações
E
Ed Stermer
Seguir
Vista de apresentação de diapositivos
Denunciar
Compartilhar
Vista de apresentação de diapositivos
Denunciar
Compartilhar
1 de 51
Baixar agora
Recomendados
Atmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology Chapter
Kaium Chowdhury
Earth's Climate
Earth's Climate
OhMiss
Air Circulation models, three model cells, planetary & local wind are shown here with flexible example.
General Circulation of the Atmosphere
General Circulation of the Atmosphere
Khalilur Rahman
GEOGRAPHY
Insolation and heat budget
Insolation and heat budget
pavithrasenthilkumar5
Meteorology
Meteorology
lorizimmerman
Presentation made at GWP-C's Disaster Mitigation Workshop held in Guyana in December 2009.
Impact of Climate Change and Variability
Impact of Climate Change and Variability
Global Water Partnership-Caribbean (GWP-C)
Atmospheric circulation
3. Atmospheric circulation
3. Atmospheric circulation
Mr Blackwell
Milancovitch Cycles explains variations in eccentricity, axial tilt, and precession of Earth. The climate changes caused by changes in the position of the Earth in comparison to the Sun. This explains the formation of ice ages.
Milancovitch cycles
Milancovitch cycles
Lakshmi Sravani Chilukuri
Recomendados
Atmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology Chapter
Kaium Chowdhury
Earth's Climate
Earth's Climate
OhMiss
Air Circulation models, three model cells, planetary & local wind are shown here with flexible example.
General Circulation of the Atmosphere
General Circulation of the Atmosphere
Khalilur Rahman
GEOGRAPHY
Insolation and heat budget
Insolation and heat budget
pavithrasenthilkumar5
Meteorology
Meteorology
lorizimmerman
Presentation made at GWP-C's Disaster Mitigation Workshop held in Guyana in December 2009.
Impact of Climate Change and Variability
Impact of Climate Change and Variability
Global Water Partnership-Caribbean (GWP-C)
Atmospheric circulation
3. Atmospheric circulation
3. Atmospheric circulation
Mr Blackwell
Milancovitch Cycles explains variations in eccentricity, axial tilt, and precession of Earth. The climate changes caused by changes in the position of the Earth in comparison to the Sun. This explains the formation of ice ages.
Milancovitch cycles
Milancovitch cycles
Lakshmi Sravani Chilukuri
This Presentation covers the following topics:- -Radiation -Albedo -Factors affecting albedo -Albedo-ice feedback -Impacts of Albedo On Environment -Heat island effect -Innovative ways to reduce albedo -Insolation effects -Black body -Kirchhoff's perfect black bodies Credits - Aditi Shah
Albedo and Radiation
Albedo and Radiation
Mokshya Priyadarshee
A short lecture on how the ocean and atmosphere interact and contribute to the global climate system
Ocean atmosphere interactions
Ocean atmosphere interactions
Janine Samelo
Geologist Indonesia
Ocean circulation
Ocean circulation
Dedy Aslam
Fronts- types and frontal zones
Fronts
Fronts
SimranSehrawat3
Circulation of the Atmosphere
Circulation of the Atmosphere
ZBTHS
Horizontal Distribution & Differences of Temperature If the Earth was a homogeneous body without the present land/ocean distribution, its temperature distribution would be strictly latitudinal. However, the Earth is more complex than this, being composed of a mosaic of land and water. This mosaic causes latitudinal (horizontal) zonation of temperature to be disrupted spatially.
Presentation on horizontal differences of Temperature
Presentation on horizontal differences of Temperature
Islamic University of Bangladesh
General circulation model
General circulation model
General circulation model
Absar Ahmed
Atmospheric circulation
Atmospheric circulation
Sarah Zurcaled
A presentation "Impact of human activities on weather and climate" or "changing climate".
A presentation on impact of human activities on weather and climate
A presentation on impact of human activities on weather and climate
Vasu Malhotra
Climatic systems major components and implications in agricultural planning
Climatic systems major components and implications in agricultural planning
Jack Onyisi Abebe
ANAKHA MOHAN ACADEMY OF CLIMATE CHANGE EDUCATION AND RESEARCH KAU
NATURAL AND ANTHAOPOGENIC RADIATIVE FORCING BASED ON IPCC AR5
NATURAL AND ANTHAOPOGENIC RADIATIVE FORCING BASED ON IPCC AR5
Anakha Mohan
Earth's energy budget refers to the tracking of how much energy is flowing into and out of the Earth's climate, where the energy is going, and if the energy coming in balances with the energy going out. The Earth receives energy from the Sun, and it also reflects and radiates energy back into space. All of the energy that warms the atmosphere, oceans and land must be radiated back into space in order to maintain our current climate. If the amount of energy radiating back into space is decreased by even a very small amount, it can lead to warming. It is believed that increasing levels of carbon dioxide in the atmosphere has a 'greenhouse effect' of reducing the amount of energy radiated into space.
Energy budget of earth
Energy budget of earth
DCRUST University
Climate modeling lecture for upper level undergraduates.
Climate Models
Climate Models
Andreas Schmittner
Paleoclimatology
Paleoclimatology
Anurag Bhatu
Air Masses
Air Masses
David Genis
HOW DOES JET-STREAMS WORK
Jet streams
Jet streams
Abdul mannan Karim
Energy Balance
Energy Balance
Stuart Kirkham
Earth Radiation Balance Project
Earth Radiation Balance Project
Suryaveer Singh
An explication of what the Bergeron Process is about.
The Bergeron Process
The Bergeron Process
Jean_Diaz
Elements of weather and climate,Measuring the weather.
Elements of weather and climate
Elements of weather and climate
Abdul Rab
elements of climate for Animal climatology
Animal climatology
Animal climatology
nea killuae
elements of climate for Animal climatology 101
Animal climatology
Animal climatology
nea killuae
Mais conteúdo relacionado
Mais procurados
This Presentation covers the following topics:- -Radiation -Albedo -Factors affecting albedo -Albedo-ice feedback -Impacts of Albedo On Environment -Heat island effect -Innovative ways to reduce albedo -Insolation effects -Black body -Kirchhoff's perfect black bodies Credits - Aditi Shah
Albedo and Radiation
Albedo and Radiation
Mokshya Priyadarshee
A short lecture on how the ocean and atmosphere interact and contribute to the global climate system
Ocean atmosphere interactions
Ocean atmosphere interactions
Janine Samelo
Geologist Indonesia
Ocean circulation
Ocean circulation
Dedy Aslam
Fronts- types and frontal zones
Fronts
Fronts
SimranSehrawat3
Circulation of the Atmosphere
Circulation of the Atmosphere
ZBTHS
Horizontal Distribution & Differences of Temperature If the Earth was a homogeneous body without the present land/ocean distribution, its temperature distribution would be strictly latitudinal. However, the Earth is more complex than this, being composed of a mosaic of land and water. This mosaic causes latitudinal (horizontal) zonation of temperature to be disrupted spatially.
Presentation on horizontal differences of Temperature
Presentation on horizontal differences of Temperature
Islamic University of Bangladesh
General circulation model
General circulation model
General circulation model
Absar Ahmed
Atmospheric circulation
Atmospheric circulation
Sarah Zurcaled
A presentation "Impact of human activities on weather and climate" or "changing climate".
A presentation on impact of human activities on weather and climate
A presentation on impact of human activities on weather and climate
Vasu Malhotra
Climatic systems major components and implications in agricultural planning
Climatic systems major components and implications in agricultural planning
Jack Onyisi Abebe
ANAKHA MOHAN ACADEMY OF CLIMATE CHANGE EDUCATION AND RESEARCH KAU
NATURAL AND ANTHAOPOGENIC RADIATIVE FORCING BASED ON IPCC AR5
NATURAL AND ANTHAOPOGENIC RADIATIVE FORCING BASED ON IPCC AR5
Anakha Mohan
Earth's energy budget refers to the tracking of how much energy is flowing into and out of the Earth's climate, where the energy is going, and if the energy coming in balances with the energy going out. The Earth receives energy from the Sun, and it also reflects and radiates energy back into space. All of the energy that warms the atmosphere, oceans and land must be radiated back into space in order to maintain our current climate. If the amount of energy radiating back into space is decreased by even a very small amount, it can lead to warming. It is believed that increasing levels of carbon dioxide in the atmosphere has a 'greenhouse effect' of reducing the amount of energy radiated into space.
Energy budget of earth
Energy budget of earth
DCRUST University
Climate modeling lecture for upper level undergraduates.
Climate Models
Climate Models
Andreas Schmittner
Paleoclimatology
Paleoclimatology
Anurag Bhatu
Air Masses
Air Masses
David Genis
HOW DOES JET-STREAMS WORK
Jet streams
Jet streams
Abdul mannan Karim
Energy Balance
Energy Balance
Stuart Kirkham
Earth Radiation Balance Project
Earth Radiation Balance Project
Suryaveer Singh
An explication of what the Bergeron Process is about.
The Bergeron Process
The Bergeron Process
Jean_Diaz
Elements of weather and climate,Measuring the weather.
Elements of weather and climate
Elements of weather and climate
Abdul Rab
Mais procurados
(20)
Albedo and Radiation
Albedo and Radiation
Ocean atmosphere interactions
Ocean atmosphere interactions
Ocean circulation
Ocean circulation
Fronts
Fronts
Circulation of the Atmosphere
Circulation of the Atmosphere
Presentation on horizontal differences of Temperature
Presentation on horizontal differences of Temperature
General circulation model
General circulation model
Atmospheric circulation
Atmospheric circulation
A presentation on impact of human activities on weather and climate
A presentation on impact of human activities on weather and climate
Climatic systems major components and implications in agricultural planning
Climatic systems major components and implications in agricultural planning
NATURAL AND ANTHAOPOGENIC RADIATIVE FORCING BASED ON IPCC AR5
NATURAL AND ANTHAOPOGENIC RADIATIVE FORCING BASED ON IPCC AR5
Energy budget of earth
Energy budget of earth
Climate Models
Climate Models
Paleoclimatology
Paleoclimatology
Air Masses
Air Masses
Jet streams
Jet streams
Energy Balance
Energy Balance
Earth Radiation Balance Project
Earth Radiation Balance Project
The Bergeron Process
The Bergeron Process
Elements of weather and climate
Elements of weather and climate
Semelhante a Climate System
elements of climate for Animal climatology
Animal climatology
Animal climatology
nea killuae
elements of climate for Animal climatology 101
Animal climatology
Animal climatology
nea killuae
Environmental studies
Clamate change introduction class 1.pptx
Clamate change introduction class 1.pptx
Lavanya943804
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" Scientists actively work to understand past and future climate by using observations and theoretical models. A climate record — extending deep into the Earth's past — has been assembled, and continues to be built up, based on geological evidence from borehole temperature profiles, cores removed from deep accumulations of ice, floral and faunal records, glacial and periglacial processes, stable-isotope and other analyses of sediment layers, and records of past sea levels. More recent data are provided by the instrumental record. General circulation models, based on the physical sciences, are often used in theoretical approaches to match past climate data, make future projections, and link causes and effects in climate change.
Climate change and its effects
Climate change and its effects
Sakil Ahmed
Science climate project
Science climate project
nashmiya
Science climate project
Science climate project
nashmiya
Hansen
Hansen
guest0517b7
Geo pro
Geo pro
joremy
Global warming and greenhouse effect
Global warming and greenhouse effect
Vinayak Verma
Climate change
Climate change (1)
Climate change (1)
Rositsa Dimova
4202: Climate change-1
4202: Climate change-1
4202: Climate change-1
Md. Abdullah-Al-Mahbub
Climate presentation
Climate presentation
YCIS Beijing
Global warming ppt
Global_warming_presentation.pptx
Global_warming_presentation.pptx
viveksingh20861
The largest association of meteorologists and climate scientists issued a fresh statement on the scientific evidence for human-driven climate change and possible impacts. This is an update from the 2007 statement that can be found here: http://www.ametsoc.org/policy/2007climatechange.html More on climate change on Dot Earth: http://j.mp/dotBasic http://j.mp/dotBasics
New Climate Change Statement from the American Meteorological Society
New Climate Change Statement from the American Meteorological Society
Earth Institute of Columbia University
climate change
Climate change scenario_new
Climate change scenario_new
Lallu Prathapan
Ecopals - Spain
Climate change (1)
Climate change (1)
Soares Jose Soares
Over millions of years, species become adapted to survive in the conditions in which they live. A stable climate supports this process and allows living things to thrive. If the climate changes quickly, organisms don’t have enough time to adapt to new conditions and may no longer be able to survive.
Climate Change Anthropogenic or Beyond
Climate Change Anthropogenic or Beyond
Arifur Rahman
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 ...
Climate ChangeInvestigation ManualENVIRONMENTAL SCIENC
Climate ChangeInvestigation ManualENVIRONMENTAL SCIENC
VannaJoy20
Global Warming - A Global Warning.... today Global warming is Rapidly increasingh it is the need of the hour to control it...... for more details about the presentation contact anishrajgoyal09rockstar@gmail.com
GLoBal WaRmiNg..
GLoBal WaRmiNg..
Anish Raj Goyal
climate change
Causes of Climate Change and environment.pptx
Causes of Climate Change and environment.pptx
AnamikaShikha2
Semelhante a Climate System
(20)
Animal climatology
Animal climatology
Animal climatology
Animal climatology
Clamate change introduction class 1.pptx
Clamate change introduction class 1.pptx
Climate change and its effects
Climate change and its effects
Science climate project
Science climate project
Science climate project
Science climate project
Hansen
Hansen
Geo pro
Geo pro
Global warming and greenhouse effect
Global warming and greenhouse effect
Climate change (1)
Climate change (1)
4202: Climate change-1
4202: Climate change-1
Climate presentation
Climate presentation
Global_warming_presentation.pptx
Global_warming_presentation.pptx
New Climate Change Statement from the American Meteorological Society
New Climate Change Statement from the American Meteorological Society
Climate change scenario_new
Climate change scenario_new
Climate change (1)
Climate change (1)
Climate Change Anthropogenic or Beyond
Climate Change Anthropogenic or Beyond
Climate ChangeInvestigation ManualENVIRONMENTAL SCIENC
Climate ChangeInvestigation ManualENVIRONMENTAL SCIENC
GLoBal WaRmiNg..
GLoBal WaRmiNg..
Causes of Climate Change and environment.pptx
Causes of Climate Change and environment.pptx
Mais de Ed Stermer
Nuclear power
Nuclear power
Ed Stermer
Climate change part 1
Climate change part 1
Ed Stermer
Climate change part 2
Climate change part 2
Ed Stermer
Alternative fuels
Alternative fuels
Ed Stermer
Alternative fuels
Alternative fuels
Ed Stermer
Mobile Air Pollution
Mobile Air Pollution
Ed Stermer
Stationary Air Pollution
Stationary Air Pollution
Ed Stermer
Gasoline
Gasoline
Ed Stermer
Gasoline
Gasoline
Ed Stermer
Illinois Petroleum
Illinois Petroleum
Ed Stermer
Coal
Coal
Ed Stermer
Carbon Cycle
Carbon Cycle
Ed Stermer
Carbon cycle
Carbon cycle
Ed Stermer
Generation Of Electricity
Generation Of Electricity
Ed Stermer
Solar Electricity
Solar Electricity
Ed Stermer
Sedimentary Rock Slides
Sedimentary Rock Slides
Ed Stermer
Volcanic Hazards Slides
Volcanic Hazards Slides
Ed Stermer
Igneous Activity
Igneous Activity
Ed Stermer
Weathering
Weathering
Ed Stermer
Electricity
Electricity
Ed Stermer
Mais de Ed Stermer
(20)
Nuclear power
Nuclear power
Climate change part 1
Climate change part 1
Climate change part 2
Climate change part 2
Alternative fuels
Alternative fuels
Alternative fuels
Alternative fuels
Mobile Air Pollution
Mobile Air Pollution
Stationary Air Pollution
Stationary Air Pollution
Gasoline
Gasoline
Gasoline
Gasoline
Illinois Petroleum
Illinois Petroleum
Coal
Coal
Carbon Cycle
Carbon Cycle
Carbon cycle
Carbon cycle
Generation Of Electricity
Generation Of Electricity
Solar Electricity
Solar Electricity
Sedimentary Rock Slides
Sedimentary Rock Slides
Volcanic Hazards Slides
Volcanic Hazards Slides
Igneous Activity
Igneous Activity
Weathering
Weathering
Electricity
Electricity
Climate System
1.
The Earth’s Climate
System
2.
3.
4.
5.
6.
7.
Recall the evidence
for the last glacial period during our hike
8.
Ice Ages Glacial
Glacial Glacial Glacial Today’s Interglacial Period
9.
10.
11.
12.
Plate Tectonics
13.
14.
15.
16.
17.
18.
19.
20.
21.
22.
23.
24.
25.
26.
27.
28.
29.
30.
31.
32.
33.
34.
35.
36.
37.
38.
Ocean – Carbon
Dioxide Feedback Note the positive correlation between atmospheric CO 2 and global temperature over the past 450,000 years.
39.
40.
41.
42.
43.
44.
45.
46.
47.
Ocean Circulation Feedback
48.
49.
50.
51.
Baixar agora