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The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul [email protected] / X 7453 http://www.panoramas.dk/fullscree n2/full22.html
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The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul [email protected] / X 7453 .

Dec 22, 2015

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Page 1: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

The Whole Earth Course

Chapter 9

Hydrosphere 2

The Cryosphere

Instructor: Dr. George A. Maul

[email protected] / X 7453

http://www.panoramas.dk/fullscreen2/full22.html

Page 2: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Outline of the Class

• Earth’s Cover of Ice and Snow• Glaciers• Glaciated Landscapes• Sea Ice• Periglacial Landscapes and Permafrost• Summary

Page 3: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

What is the Cryosphere?

• Sea, lake, and river ice• Glaciers• Ice sheets• Ice caps• Ice shelves• Frozen ground such as permafrost

Page 4: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Last time we said that Earth’s Cryosphere is 43,400,000 km3

In-class Calculation:How tall would a 1 km x 1 km tower of 4.3x107 km3 stand?

What is the distance to the sun?

Volume = Height x Length x Width

4.3x107 ÷ 149.6x106 =

Page 5: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

HOW BIG IS THE CRYOSPHERE?

Approximately 3% of all the water in the hydrosphere is contained in the Cryosphere.

WHERE DO WE FIND THE CRYOSPHERE?

Glaciers cover about 10% of land area.

Permafrost is another 20% of land area.

HOW MUCH IS SEA ICE?

Two-thirds of Earth’s permanent ice cover;

one-thousandth of Earth’s total ice volume.

Page 6: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .
Page 7: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Past Glaciation

Ice cover changes Earth’s Albedo (A)

Who Cares?

Page 8: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Average snow cover in the northern hemisphere (%) during December 1992, based on data received (left) from a microwave sensor aboard a satellite.

Maximum 1979-1995What is a microwave

satellite sensor?

Today’s ice and snow coverage

Page 9: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

MICROWAVE SENSORSDefense Meteorological Satellite Program – DMSP

Scanning Multichannel Microwave Radiometer - SMMR

DMSP SMMR Image

Page 10: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Climate Change: Arctic Sea Ice

Page 12: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Antarctic Ice

“Facts matter” Stephen Breyer

Associate Justice, US Supreme Court

Page 13: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

How would Earth’s temperature change if the ice coverage changed?

414 EARTHSUN

GHE TAC

Q

QGHE: What is the greenhouse effect?

CSUN: What is the solar constant?

A: What is Earth’s albedo?

4: Where does the ¼ come from?

What is ?

Page 14: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Stefan-Boltzmann Law

Q=

Units?

Circa 1879

Plank’s LawIλ

λ

Page 15: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

What is QGHE ?

𝑄𝐺𝐻𝐸=𝜎 𝑆𝑡𝑒𝑓𝑎𝑛−𝐵𝑜𝑙𝑡𝑧𝑚𝑎𝑛𝑛×𝑇 4

Page 16: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

IN CLASS CALCULATION:

CSUN: What is the solar constant?

SUNSUNEarth

SUNSUN C

r

rT

2

24

4

4

where

4281067.5 KmWx

If TSUN = 5775 K, CSUN = ?

rsun= 696,000 kmrEarth-SUN=149,600,000 km

Page 18: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Why the ¼ in our equation?

Energy in: π r2

Energy out: 4π r2

By-the-way: Q is a flux, i.e. amount per unit area per unit time

𝐽𝑚2𝑠

=𝑊𝑚2

Units?

Page 19: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

IN CLASS CALCULATION:

How would Earth’s temperature change if the albedo changed from 30% to 29%?

4%)30(30.01

4 AEARTHSUN

GHE TC

Q

4%)29(29.01

4 AEARTHSUN

GHE TC

Q minus

)(30.029.04

4%)29(

4%)30( AEARTHAEARTH

SUN TTC

If TEARTH(A=30%) = 288K, TEARTH(A=29%) = ?

Page 20: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Contorted medial moraines of Susitna Glacier in Alaska.

Glaciers

Page 21: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Where do we find glaciers?

Page 22: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

28m

How thick can glaciers be?

How thick is 3000 m?

What is the height of the Crawford Building?

Page 23: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Main features of a valley glacier.

Page 24: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

An expanded view of the effects of glacial ice on the geosphere.

Page 25: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Pressure Melting Point of Ice

0

500000

1000000

1500000

2000000

2500000

-25-20-15-10-50

Temperature (Celsius)P

res

su

re (

mil

lib

ars

)

Ice movement over meltwater has less friction than over frozen surfaces.

What is the pressure (p) at the base of a 10,000 m thick glacier?

p = ρ∙g∙h

Page 26: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

IN CLASS CALCULATION:

What is the pressure (p) at the base of a 10,000 m thick glacier?

What are the units?

What is the pressure melting point at the base of the glacier?

-25-20-15-10-500

50000000

100000000

150000000

200000000

250000000

Pressure Melting Point of Ice

Temperature (Celsius)

Pre

ssu

re (p

asca

ls)

So the ice melts at -8°C

Page 27: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Changes in a Glacier

Page 28: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Evolution of glacial carved

landforms

Page 29: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Effects of glaciers on Earth’s surface are significant. Can you contrast the effects of streamflow and glaciers on sediment transport?

Hint: Which one sorts sediments during transport?

Page 30: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Major glacial landforms in USA

Page 31: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Periglacial Landforms, Permafrost, Tundra

Tundra Extent

TundraPeriglacial Landform

Permafrost

Page 32: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

FeedbackWhich is positive feedback and which is negative feedback?

http://www.atmosedu.com/Geol390/feedbacks.htm

Page 33: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Why do icebergs float? Who was Archimedes?

Sea Ice

Page 34: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

IN CLASS CALCULATION:

How high does an iceberg float?

We’ll need the hydrostatic equation again

p = ρ∙g∙hp – pressure, ρ – density, g – gravity, h – height

ρseawater=1025 kg·m-3 ρice=917 kg·m-3

(ρgh)water = (ρgh)ice so hice = ?

Page 35: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .
Page 36: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

What maritime disaster precipitated the formation of the International Ice Patrol?

Page 37: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Blowing up Icebergs?!?!

Page 38: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Pancake Ice – discovery of the Ekman Spiral.

Page 39: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Seasonal extent of sea ice in A. Southern hemisphere, and B. Northern hemisphere.

Page 40: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Florida Tech Student deploying FIT-built ROV under Arctic Ice

What is an ROV?

Page 41: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

How much frozen water is in sea ice?

Sea ice is 0.1% of the total volume of ice on Earth.

How much of Earth is covered with sea ice?

2/3 of Earth’s permanent ice cover is sea ice. This is approximately 5-6% of the surface area of Earth.

Of what significance is sea ice in the Earth System?

What happens if it all melts?

What happens if more forms?

Who cares?

Page 42: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Please note the size of the sheets of ice breaking off!!

Approximately 1000 km3 of glacial ice enters the sea each year as icebergs. (Can you put this number in perspective?)

How wide is Florida?

Page 43: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

http://oceanexplorer.noaa.gov/edu/learning/player/lesson12/l12la1.html

Towing Icebergs

Step 2: curtain icebergStep 1: circle iceberg Step 3: tow iceberg

Page 44: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

How much heat to melt sea ice?

What about the Cryosphere?Sea ice is 0.1% of Cryosphere

or

0.0434 x 106km3 or 39.4 x 1018 g of ice.

For ice at 00C to water at 00C 330J/g or 79 cal/g is required.

Total heat required to melt sea ice is 1.3 x 1022 J,

or

for the whole Cryosphere is 1.3 x 1025 J.

For perspective, world energy consumption is approximately

4 x 1020 J/year

One PB&J sandwich is about 1 million Joules!!

Page 45: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Transect along western Atlantic Ocean showing water masses and general circulation processes.

What happens if sea ice melts here?

What happens if sea ice forms here?

Page 46: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Post Script: Greenland Sea Deep Water Warming

http://www.sciencedaily.com/releases/2013/09/130925102833.htm

Page 47: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Summary

• Cover of Ice, Snow, and Permafrost is 30%• Glaciers: temperate and polar• Glacier mass = accumulation - ablation• Glaciated Landscapes: Plow, File, and Sled• Sea Ice: >60% of area, 0.1% of volume• Permafrost covers >20% of land surface

Page 48: The Whole Earth Course Chapter 9 Hydrosphere 2 The Cryosphere Instructor: Dr. George A. Maul gmaul@fit.edu / X 7453 .

Next TimeChapter 10 – the oceans

70.8% of the Whole Earth’s Surface