The last 600ky… LGM Last Glacial Maximum 18Ky. Paleoclimataology Lecture notes from Ellen Druffel.

Slides:



Advertisements
Similar presentations
Orbital Theory of Ice Ages
Advertisements

Climate Cycles and Cycles in Earth’s Orbit Cycles give predictability because they repeat at regular intervals. One of the major climate discoveries is.
Global Air temperature from 1850 The time series shows the combined global land and marine surface temperature record from 1850 to The year 2007.
Lecture 8: Orbital Variation and Insolation Change (Chapter 7)
EARTH’S PLACE IN THE UNIVERSE REVOLUTION, ROTATION, & LOCATION.
Seasonal & Diurnal Temp Variations ATS351 Lecture 3.
14.3 Climatic Changes.
Lecture 34: Orbital (Milankovitch) Theory of the Ice Ages
Lecture 7 Paleoclimate and the Ice Ages. Ruth Valley Glacier Alaska--The glacier occupying Yosemite Valley probably looked similar.
Bringing Astronomy Down to Earth What do we know about Earth – Moon – Sun interactions?
Sea-Tac. Glacial evidence In what way is a glacier like a water reservoir (other than they are both water)?
Myr ago Puzzle: Ice Ages! Occur with a period of ~ 250 million yr Cycles of glaciation within the ice age occur with a period of 40,000 yr Most recent.
Physics 218: Mechanics Instructor: Dr. Tatiana Erukhimova Lectures 35,36.
MET 112 Global Climate Change -
Natural and Human Influences on Climate Change
Physics 218: Mechanics Instructor: Dr. Tatiana Erukhimova Lectures Hw: Chapter 18 problems and exercises.
Gyroscope.
OC 450: Orbital Controls on Climate (Chaps 8 and 10) Main Points: Small cyclic variations in the earth’s orbital characteristics affect the distribution.
Physics 218: Mechanics Instructor: Dr. Tatiana Erukhimova Lectures 26, 27 Hw: Chapter 18 problems and exercises.
Earth Sun Geometry.
14.3 Climatic Changes SWBAT distinguish among different types of climatic changes; recognize why climatic changes occur.
Astronomical Control of Solar Radiation Earth's present-day orbit around the Sun Earth's present-day orbit around the Sun  Not permanent  Varies at cycles.
{ Natural Changes in Climate.  8.9 Long Term and Short Term Changes in Climate  8.10 Feedback Loops and Climate  8.11 Clues to Past Climates.
Long Term and Short Term Changes in Climate; The Albedo Effect
CE 401 Climate Change Science and Engineering orbital variations and climate, aerosols, carbon cycle 25 January 2011.
Ice Ages Effects on Climate, Weather, & Geography.
OC 450: Orbital Controls on Climate (Chaps 8 and 10) Main Points: Small cyclic variations in the earth’s orbital characteristics affect the distribution.
Quaternary Environments Climate and Climatic Variation.
Natural Climate Changes Processes Resulting in Changes in Climate Trends Over Time.
Chapter 8 Astronomical Control of Solar Radiation 1.Changes in Earth’s axial tilt through time 2.Changes in Earth’s Eccentric Orbit through time 3.Precession.
14.3 – CLIMATIC CHANGES. Ice Age  Periods of extensive glacial coverage  Lots of ice sheets  Average global temperature decreased by about 5°C  Most.
MILANK OVITCH cycles. What are the Milankovitch Cycles They are a series of theoretical cycles presented by Yugoslav Astronomer Milutin Milankovitch that.
Milankovitch Cycles and the Big Chill CGF3MI Sunday, June 5, 2016.
Honors 1360 Planet Earth Last time: Measuring Earth’s Hydrosphere Obs : Altimetric height changes on rivers & lakes (with strong seasonal cycle & dependence.
April , 2005 NOTE: Reviews will be handed back Thurs/Fri to
The Earth’s Orbit ES 2: I can explain that Earth is one of several planets to orbit (revolve and circle) the sun, and that the moon orbits Earth.
The Earth’s Tilt. The Earth is tilted on its axis at 23.5 degrees The Earth is tilted on its axis at 23.5 degrees For 6 months the Northern Hemisphere.
Natural Climate Changes Processes Resulting in Changes in Climate Trends Over Time.
History of Climate Change  During earth’s history, climate has generally been warmer than it is today, but is periodically interrupted by short cooler.
An Orbital Theory For Glacial Periods
Climate Change: Ice Ages Naturally Occuring, Long Term
Orbital Control of Climate The last 600,000 years.
Chapter 2- Activity 3 How Do Earth’s Orbital Variations Affect Climate?
Weather, Climate and Society ATMO 336 Seasons Orbital Variations and Ice Ages.
Our Current Seasons. seasons ence/terc/content/visualizations/es0408/es 0408page01.cfm?chapter_no=04http://
Climate and the Seasons
1 MET 112 Global Climate Change MET 112 Global Climate Change - Lecture 6 Natural Climate Forcing Dr. Eugene Cordero San Jose State University Outline.
Orbital Hypothesis of Climate Change & Pleistocene Ice Ages.
Milankovitch, 1937 Orbital Theory of Ice Ages
The Earth’s Orbit and Climate
Lecture 20: Orbital Variations in Ice Sheets (Milankovitch Cycles)
Climates of Geologic Time
Milankovitch cycles/ Chaotic obliquity variations
Long-term climate change & Short-term climate variability
14.3 Climatic Changes.
Climate and the Seasons
Eccentricity,Axial Tilt, Precession and Inclination
Lecture 18: Orbital Variations
The Earth’s Orbit and Climate
Past Climates - the mechanisms
Do Now Please take out your Milankovitch Cycles Packet.
Earths Movement.
Earth’s Season MOTIONS OF THE EARTH.
Earth Sun Geometry.
The Earth’s Orbit and Climate
“Being Milutin Milankovitch”
Natural climate change
Historical Climate Change
EARTHS MOVEMENT.
Oscillations – Resonance Glacial Cycle
Presentation transcript:

The last 600ky… LGM Last Glacial Maximum 18Ky

Paleoclimataology Lecture notes from Ellen Druffel

1. Eccentricity 3% range of variation of E-S distance due to eliptical orbit around Sun, Pull of large planets Now, perihelion occurs during northern Winter (3 January) 100ky and 413ky periods Now, e =.0167 (relatively circular)

2. Tilt - Reason for Seasons Now tilt is 23.5°, and is decreasing. Higher the tilt, higher the seasonal differences Has gone from 24.5° -22.2°, varied by pull of large planets 41 ky period

3. Precession - Wobble Varies E-S distance with season Variation of the direction in which the E axis leans. Caused by the pull of Sun and moon on Earth Now Earth’s axis points to Polaris 23 ky stronger period - combined wobble and slow turning of eliptical orbit. Now 11Kya

On the long term…the precessional index Eccentricity variations at 100Ky and 413Ky modulate the amplitude of the precession cycle. This is why we have the 100Ky ice age cycle!

How orbital theory, climate records (  18 O) and northern hemisphere insolation (i.e. melting in N. Atlantic) compare over the past 600ky. Cold warm now LGM 18ky

BLAG invokes chemical weathering

Molnar & England, 1990