Geog 1900: ExtremeWeather and Climate. Review of last lecture The modern climatology (meteorology) was born in the 1940s (a very young science!), but.

Slides:



Advertisements
Similar presentations
Feedback effects When the Earth warms up, a large number of changes take place in the atmosphere, the oceans, and the land surface. Some of these changes.
Advertisements

The syllabus says: Atmosphere and change  Describe the functioning of the atmospheric system in terms of the energy balance between solar and long- wave.
Evolution of the Atmosphere. Review of last lecture The modern climatology (meteorology) was born in the 1940s (a very young science!), but has been growing.
Deep Tropical Convection contribution to climate change.
KYLE PETROSKY PHYSICS MAJOR Effect of Deep Convection on the Regulation of Tropical Sea Surface Temperature By John M. Wallace (1992) Formation and Limiting.
DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 16: 05/20/2010 ATM S 111, Global Warming: Understanding the Forecast.
DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 9: 04/27/2010 ATM S 111, Global Warming: Understanding the Forecast.
Extratropical climate. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the Walker circulation?
Climate and Weather Pages Climate and Weather Weather refers to the conditions in the atmosphere of a certain place at a certain time. (ex: The.
Arctic summers ice-free by 2013 predict scientists European heat waves kill 35, – the UK’s warmest year on record Rising sea levels threaten Pacific.
Severe Weather! © The GlobalEd 2 Project Photo credit: Tyrone Turner, National Geographic Homes destroyed by Hurricane Katrina.
Modern Global Climate Change by Thomas R. Karl and Kevin E. Trenberth Summary: Ken Hu Critique: Roy Chen.
Ocean Response to Global Warming William Curry Woods Hole Oceanographic Institution Wallace Stegner Center March 3, 2006.
Gary Lagerloef, PhD Science on Tap, 7 April Apollo 17 December 1972 Climate Science in the Space Age Gary Lagerloef Oceanographer & Climate Scientist.
Present Climate Change – Inquiry Labs Lesson Global Precipitation Measurement Mission Developed by the GPM Education Team NASA Goddard Space Flight Center.
Climate Variability and Change: Introduction Image from NASA’s Terra satellite Temperature anomalies for July 2010.
UNDERSTANDING TYPHOONS
Weather: The state of the atmosphere at a given time and place, with respect to variables such as temperature, moisture, wind velocity and direction,
Overview II: Importance of the atmospheric boundary layer.
1 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt 10 pt 15 pt 20 pt 25 pt 5 pt Surface.
Importance of the atmospheric boundary layer. Life cycle of the Sun and the Earth The earth will be inhabitable for another 0.5 billion years, if we protect.
Climate and Climate Change
Earth Science Sec. 1.1 Introduction to Earth Science and Systems.
Geog 1900: Extreme Weather and Climate. Review of last lecture Atmosphere: A mixture of gas molecules, microscopically small particles of solid and liquid,
In the winter time in Virginia, the air mass that brings us the cold dry air that makes your skin dry is the:
Geog 5900: Climatology. Atmospheric Sciences at a Glance (1)
OCEAN INTERACTIONS WITH THE ATMOSPHERE Niki Henzel & Ron Gabbay.
How do we predict weather and climate?. Review of last lecture Well-defined pattern of heating, temperature, pressure and winds around the globe. Well-defined.
Climate Change UNIT 3 Chapter 7: Earth’s Climate System
Feedbacks and Abrupt Climate Change. Review of last lecture Global climate models: Earth system models (5 components) Global climate models can reproduce.
Geog 1900: Extreme Weather and Climate. Overview I: Extreme weather and climate.
21.3 Climate Change. Natural Processes That Change Climate Volcanic eruptions The presence of volcanic ash, dust, & aerosols in the air increases the.
@earthscience92. What is a System? Systems – a group of interacting parts that work to together to do a job or to form a whole. Open Systems Closed Systems.
Lecture 5 The Climate System and the Biosphere. One significant way the ocean can influence climate is through formation of sea ice. Sea ice is much more.
Return to Home Page Return to Home Page January 23, 2014 Introduction to GEOG 495: The Geographies of Climate Change.
Understanding the Science of Climate Change Susquehanna University January 9, 2015
Importance of the atmospheric boundary layer (1).
Meteorology What is it? How does it work? Meteorology in action!!
Overview I: Atmospheric Sciences at a Glance. The mission of the atmospheric sciences is to understand and predict weather, climate, and related disasters.
Warm Up 4/15 Where are dry-summer tropical climates found in the United States? a. Utah c. Texas b. Arizona d. California Another name for a semi-arid.
Climate feedbacks for global warming. Review of last lecture Mean state: The two basic regions of SST? Which region has stronger rainfall? What is the.
DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 3: 10/08/2015 ATM S 111, Global Warming: Understanding the Forecast.
EARTH’S CLIMATE PAST and FUTURE SECOND EDITION CHAPTER 17 Climatic Changes Since the 1800s WILLIAM F. RUDDIMAN © 2008 W. H. Freeman and Company.
Geog 1900N: Extreme Weather and Climate. Overview I: Extreme weather and climate.
GEOGRAPHY 120: EARTH SYSTEM II. Atmospheric Sciences at a Glance.
Are Humans Causing Global Warming? How do we know? What is the Evidence?
CE 401 Climate Change Science and Engineering modeling of climate change predictions from models 10 February 2011 team selection and project topic proposal.
Unit 4 Weather Lesson 2 How Do the Oceans and the Water Cycle Affect Weather?
What causes the wind to blow?
Surface Energy Balance (1). Review of last lecture The mission of meteorology is to understand and predict weather- and climate-related disasters (e.g.
Lecture 9: Air-Sea Interactions EarthsClimate_Web_Chapter.pdfEarthsClimate_Web_Chapter.pdf, p ; Ch. 16, p ; Ch. 17, p
Geog 1900N: ExtremeWeather and Climate. Review of last lecture The modern climatology (meteorology) was born in the 1940s (a very young science!), but.
Importance of the atmospheric boundary layer (2).
Geog 5900: Climatology. Review of last lecture Atmosphere: A mixture of gas molecules, microscopically small particles of solid and liquid, and falling.
Weather Patterns Environmental Science 2.2. Weather Predictions Meteorology – study of the physics and chemistry of the atmosphere Weather – atmospheric.
NEW CHAPTER the BIG idea Some features of weather have predictable patterns. Weather Patterns Air pressure varies in the atmosphere. The atmosphere has.
9/9/16 WHAT IS EARTH SCIENCE?
Global Weather Patterns
Air-Sea Interactions The atmosphere and ocean form a coupled system, exchanging heat, momentum and water at the interface. Emmanuel, K. A. 1986: An air-sea.
Q2 What kinds of information can you get from a weather map?
Warm Water Currents & Climate Cold Water Currents & Climate
Weather, Weather Maps and Forecasting
Impacts of climate change
Atmosphere & Weather Review
Weather, Weather Maps and Forecasting
Climate and Climate Change
El Niño-Southern Oscillation
Weather, Weather Maps and Forecasting
Understanding and forecasting seasonal-to-decadal climate variations
Intro to Earth Science-Part 1
Presentation transcript:

Geog 1900: ExtremeWeather and Climate

Review of last lecture The modern climatology (meteorology) was born in the 1940s (a very young science!), but has been growing very fast! Now we have a global observational network with many satellites, ships, radars and surface stations, as well as very comprehensive prediction models running on the world ’ s fastest supercomputers. The current status of weather and climate predictions: (1) weather prediction good to 10 days, (2) tropical cyclone prediction good in track but not in intensity, (3) climate prediction good to two seasons, (4) climate change projections have a 3-fold difference in magnitude.

Overview III: Why is it so difficult to predict weather and climate?

Problem I: Different parts of the world are strongly connected to each other (The “Teleconnection Problem”) Global atmospheric flow

Satellite image: Flow of water vapor in the atmosphere

Example 1: Global impacts of El Nino

The “Pineapple Express” connecting Hawaii and California

Example 2: Global impacts of the mini El Nino (Madden-Julian Oscillation)

Factors affecting US weather and climate El NinoMadden-Julian Oscillation Amazon Arctic N. Atlantic Atlantic/ Sahel

Any location is affected by all the other locations, and in turn is affecting all the other locations

Problem II: Different components of the earth system (atmosphere, land, ocean, ice, clouds, etc) are strongly interacting with each other (The “Feedback Problem”)

Example: Melting of Arctic sea ice

Video: Ice Albedo feedback

Problem III: The global climate models divide the earth into many small pixels (called grids), but the earth system composes of both very big objects (such as the whole Pacific Ocean) and very small objects (such as the cloud droplets), making it very difficult to draw them on the same page (The “Subgrid-Scale Problem”)

The limitation of concept/theory/model: Only approximation of real world Concepts cut reality into smaller pieces

Some Great Weather/Climate Scientists

Prof. Lonnie Thompson – OSU Father of Tropical Glaciology Spent an enormous amount of time above 5500 m Discovered solid record for Earth’s climate history Grown up in West Virginia Did three part-time jobs in high school to make a living Worked for many years with low salary Went back to the Himalayas after heart transplant

Prof. Robert Cess SUNY at Stony Brook World’s leading expert on climate change and Earth’s energy budget Organized the first international team for supercomputer prediction of global climate change, and many NASA and DOE projects Was not even an AMS Fellow when received the Charney Award Finished his Ph.D. in 3 years while doing a full-time job and taking care of his first child Hobby: Collectible cars

The young generation Video: Prof Dargan Frierson and Elizabeth Maroon sing The World of Daisies (lyrics by Prof Mike Wallace) in ATM S 111: Global Warming TtFcQlUhttps:// TtFcQlU

Summary The main reasons of the difficulties in weather and climate predictions: (1) Teleconnection problem, (2) Feedback problem, and (3) Subgrid-scale problem Some great weather/climate scientists