Greenhouse to Icehouse: The Last 50 Million Years.

Slides:



Advertisements
Similar presentations
Factors that Affect Climate
Advertisements

It all begins with the sun……
Climate Cooling Proxy evidence indicates an erratic cooling Proxy evidence indicates an erratic cooling  Over both poles and mid latitudes  Roughly equal.
1 Back into the Icehouse GEOL 3100 Christina Gallup.
Lecture 7: Back into the Icehouse: Last 55 Myr (Chapter 6)
Climate over the long term (Ch highlights)
GEOS 112 Lecture Topics 4/28/03 Read Chapter 12 (Glaciers) Final Exam – Monday, May 5 1:00pm 1.Types of Glaciers; 2.Glacier Formation, Mass Balance, and.
FACTORS INFLUENCING CLIMATE
Section 3: The Changing Continents
Lecture 17 Tectonic-scale Climate Change Text book: Ch. 4, p64-67, 71-80, Four Main Processes: –Land-ocean spatial configuration: control where.
FACTORS INFLUENCING CLIMATE
By John B.. Plate tectonics The movement of the plates caused by convection in the mantle. Moves the continents and widens/compresses the oceans. –affects.
Overview of the Past and Present Earth System Observations of the Earth OSHR 1609 Climate 101 September 20, 2013 Scott Denning, CSU.
The Factors that Affect Climate Grade Nine Socials.
Back into the Icehouse: The Last 55 Million Years Global Climate Change Since 55 Myr Ago.
Climate.
Goals for this section 1.EXPLAIN the feedback mechanism believed to have maintained Earth's average temperature within the range of liquid water over 100s.
Greenhouse Earth: 100 Ma GEOL Paleoclimate Research Two components –Observations i.e. fossils, sediments, chemical proxies –Modeling using observations.
Plate Tectonics.
Lecture 4 Outline: Plate Tectonics – Mechanisms and Margins Learning Objectives: What are the types of plate boundaries? What processes occur at different.
How it happens and how it affects us.
Factors That Affect Climate
Back into the Icehouse: The Last 55 Million Years Chi-jung Wu.
Unit 1: Physical Geography
Global distribution of heat text. Spectra of incoming vs. outgoing radiation text.
The Physical Regions of Western Canada
Climate & Climate Change Objectives: 1. What factors affect climate? 2. What is El Nino & how does it work? 3. What causes ice ages? 4. How can scientists.
Plate Tectonics and Global Glaciation Tectonic plate motions move the continents and determine the form of the ocean basins. Paleoclimatologists have suggested.
Overview of Climate Change Throughout Earth History Overview of Climate Change Throughout Earth History During the Phanerozoic (600 Ma), climate fluctuated.
Ch : Climate & Climate Change Objectives: 1
S6E2.c. relate the tilt of earth to the distribution of sunlight through the year and its effect on climate.
Class #35: Friday, November 201 Past Climates: Proxy Data and Mechanisms of Change.
1 Plate Tectonics and Climate 陳奕穎 Chapter 5 of EARTH’S CLIMATE Institute of Hydrological Sciences.
The Climate Chapter 25.
Climate Long term weather patterns
Greenhouse Climate September 11, Earth 100 Mya -Global sea level 100m higher than today -No permanent ice -Middle Cretaceous -Dinosaurs, turtles,
The Last Glacial Maximum. What was it like during the last glacial max? About 21K yrs ago ice sheets were at a max and CO2 was at a min. The ice.
FACTORS INFLUENCING CLIMATE The factors that influence climate can be identified by using the following anagram: J. BLOWER J. = Jet Stream B = Bodies of.
Lesson #8 Climate & Weather Patterns Earth & Space Science.
Climate and Ecosystems
Global Climate Change The Evidence and Human Influence Principle Evidence CO 2 and Temperature.
Climate and Climate Change Chapter 21
What are the factors that control air temperature? What are the factors that control precipitation? What drives the annual temperature regime. What effect.
What is it?.  Climate is the name for the general conditions of temperature and precipitation for an area over a long period of time.
The Greenhouse Climate. We Know the Last 100 Myr Pretty Well… Why? Know –Continental Positon –Shape of the Ocean Basins –Temperature –Sea Levels.
Factors Affecting Climate
Class #39: Friday, April 171 Mechanisms of Climate Change Natural and Anthropogenic.
L- Latitude O- Ocean Currents W- Wind and Air Masses E- Elevation R- Relief N- Nearness to Water.
Chapter: Climate Section 3: Climatic Changes.
Art or Science?. Explain the thermal transfers of energy within oceans and the importance of oceanic conveyor belts.
The Current Location of Continents on the Earth Today If these were pieces to a puzzle, can you see how they would fit together?
Climate Change Ch. 12 Study Guide. 1. Identify 2 physical features and explain how they influence the climate. Latitude Elevation.
Climate. Climate Climate – the pattern of temperature and precipitation typical of an area over a long period of time. –Temperature –Precipitation There.
Climate Climate. Introduction Introduction Climate is a generalized pattern for weather over a period of time Climate is a generalized pattern for weather.
$200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $300 $400 $500 $100 $200 $ 300 $400 $500 $100 $200 $300 $400 $500 $100 Plate Tectonics More Plate.
Factors That Affect Climate. Identify five factors that affect climate and explain how each affects climate.
Climate, Weather and Vegetation Zones
Location of Large Igneous Provinces:
The Great Cooling.
What is Climate Change? Long term changes in the Earth’s heat budget resulting from radiative inbalance can result in a colder or warmer climate.
FACTORS INFLUENCING CLIMATE
Section 1: Ocean Currents
Plate Tectonics California Standard 3a. & b.
Chapter 3: Plate Tectonics
Climate Changes.
Ocean Currents Chapter 25 section 1.
Chapter: Climate Section 3: Climatic Changes.
Climate.
Topic 4: The Moving Crust
Presentation transcript:

Greenhouse to Icehouse: The Last 50 Million Years

Since the Cretaceous the Climate has Grown Colder….Why?

60 Myr Ago

50 Myr Ago

40 Myr Ago

30 Myr Ago

20 Myr Ago

Evidence of Cooling Prior to 50 Myr ago we had palm trees and crocodiles north of the artic circle 35 Myr ago the palms gave way to broadleaf evergreens Cooling was first intense in the southern hemisphere

Evidence of Cooling Until about 30 Myr ago Antarctica looked like this… Now Antarctica looks like this…

Arctic Conditions Breadfruit trees north of the arctic circle ~60 myr ago Now tundra…

Oddly there is a relationship between leaf edges and temperature

Just from leaf shape it is clear that the climate is changing

Deep-Water O-18 Shows Strong Cooling O-18 from deepwater forams. Current temperatures are around 2  C 50 Myr ago temperatures were ~16  C

More Evidence of Cooling Turns out that the ratio of Mg to Ca in Foram shells depends on temperature. Again, for deep water forams there is a very strong cooling signal

So what caused the cooling? Geography? –Distribution of heat by ocean circulation –Gateway Hypothesis Changes in seafloor spreading rates? Uplift and Weathering? –Changes in uplift

The opening of the Mar de Hoces (Drake Passage) Before the separation of South America and Antarctica warm currents would push heat south. The development of the circum-polar current occurred about the same time as onset of major glaciation. Climate models don’t support this idea. I don’t really buy modeling as evidence…. modeling is not always a good guide to reality.

Mar de Hoces

The closing of the Panama Seaway Closed about 4-10 Myr ago. This redirects warm water north (gulf stream). Suppresses sea ice and provides more moisture at high latitudes for snow buildup. BUT, it is the gyres that drive the circulation. The seaway is too far south to strongly affect the North Atlantic gyre.

Spreading Rates? The simplest idea about causes of cooling is that CO2 dropped because of slower seafloor spreading. But….over the last 15 Myr spreading has been pretty constant while the climate became very cold.

Spreading Rates? BUT….not all subducted material is created equal –Remember it is subduction that actually delivers the carbon to volcanoes. –If the plate being subducted is carbon-poor, then there is less CO2 available for eruption. But….that recycling process is VERY slow, so the current CO2 is probably coming from plate subducted 10’s Myr ago. Most current subduction may be on the carbon-poor side, but that would have no effect on CO2 output for a long time. I really doubt that changing spreading rates have anything to do with the current cooling.

Uplift and Weathering The hypothesis is that we are currently experiencing unusually high rates of uplift and weathering –Unusually large amounts of high terrain –Unusual amounts of rock fragmentation –Unusually high rates of chemical weathering

Are today’s continental elevations normal? Well….no. “Normal” is Andean style mountain building associated with subduction. Continent to continent collision has been pretty sparse since the assembly of Pangaea (~200 Myr ago) The Tibetan Plateau is a pretty unusual feature –2.5 million Km 2 an average of 5 km elevation The Rocky Mountains are also pretty unusual

Is today’s physical weathering normal? Well….no. Most of the suspended sediment load is associated with mountains (duh…) But by far the largest loads are off of the Tibetan Plateau

Is today’s physical weathering normal? And the sediments coming off the Himalayas have increased 10X in the last 40 Myr.

Is today’s physical weathering normal? Part of the reason for enhanced weathering comes from an enhanced Indian Monsoon The higher the Himalayas rise, the more it pushes moist air into cool altitudes, creating more rainfall….creating more weathering….

Is today’s physical weathering normal? Probably not…. But what is normal? It is very hard to estimate CO2 removal rates for past epochs. It does seem that the rise of Tibet and other major uplifts do have a strong effect on climate.

Feedbacks Changes in uplift could generate a negative feedback that moderates cooling. The decrease in temperatures would decrease weathering in the rest of the world

Feedbacks But, the overall effect of the feedback is not clear. Uplift could produce a positive feedback. Glaciation could increase fragmentation and create much more weathering More weathering enhances cooling, creating more glaciers…..

Feedbacks Remember, what glaciers do is pulverize rock and push it around. Just the thing to enhance weathering and make things colder.

Feedbacks But this sort of weathering feedback would tend to moderate any increase in warming. Weathering would rapidly increase as ice retreats. That would reduce CO2 and then reduce warming …..not happening now.

Tectonics Tectonic-scale processes operate very slowly. Doesn’t really explain why we got four major ice advances in the last 500,000 years. Or how we got warm intervals (like now…).