POLAR DETECTIVES
CAN YOU IMAGINE A YEAR
WITHOUT SUMMER?
In many places, the sky seemed permanently overcast.
In
1816…
CONDITIONS IN EUROPE…
Ireland—much rainier than normal and the potato crops failed.
Europe—wheat crops were dismal—bread shortages.
CONDITIONS IN ASIA…
A LITERARY CONNECTION…
NEWSPAPERS COVERED THE STORY OF THE YEAR WITHOUT SUMMER…
“We should be glad if proper pains were taken to ascertain, by regular journals of the weather from year to year, the state of the seasons in this country and Europe, as well as the general state of health in both quarters of the globe. We think the facts might be collected, and the comparison made, without much difficulty; and when once made, that it would be of great advantage to medical men, and medical science.”
Interesting that the Albany Advertiser proposed some theories and then called for the events to be studied to understand what was going on:
SO LET’S DO THAT STUDY…
AS SCIENTISTS, WE MUST START WITH A QUESTION:
What caused the extreme 1816 summer conditions, and how did that year’s climate compare to long term patterns?
HYPOTHESIS…
THERE MAY BE EVIDENCE IN THE ICE CORES AS TO WHAT CAUSED THE UNUSUAL CLIMATE IN 1816.
CHECK YOUR SUPPLIES:
BEFORE STUDYING ICE CORES, WE NEED TO UNDERSTAND SOME BASICS OF SNOW AND ICE.
POLAR DETECTIVES—
BACKGROUND
Snow forms differently under different
atmospheric conditions:
-under very cold, drier conditions, crystals are finer grained and needle-like—fine, smaller crystals indicate winter accumulation (appears ‘darker’ in snow pit)
SNOW TRANSITIONS TO ICE
EXAMINE THE SUGAR & SALT
DIRECTIONS:
Build an ice core model:
1. Build your base with summer snow to a thickness you can clearly see —sugar (representing coarser summer season snow)
2. Add winter snow on top to a layer you can clearly see from the outside of your cylinder. —salt (representing finer winter snow)
Together these 2 layers represent evidence of one year of precipitation at your site.
DIRECTIONS:
(Continued)
Build an ice core model:
4. Continue to alternate layers of summer and winter snow.
5. At several different times, put in evidence of a volcano —pepper (representing an ash layer). This should be a thin layer, but thick enough to see.
6. Examine your “ice core” with your hand lens. What do you observe?
Ice Core Layers
Prepare to become
Polar Detectives!
Dr. Osterberg is going to lead us through an exploration of data from the time period around “The Year Without Summer.”
POLAR DETECTIVES—WHAT ELSE WE NEED TO KNOW
Snow contains chemical properties we can’t see:
GRAPHING
Using the graph paper, plot the concentration of sulfur in parts per billion (ppb) on the Y-axis against the year on the X-axis for each core. Use different colored pencils for the Summit (Greenland) and Antarctic data sets.
NOTE: the half added to each year indicates it was half-way through the calendar year, or summer, when the ice core data was recorded.
The ppb represents an average for the year (i.e. summer 1780-summer 1781)
Data courtesy of Dr. Joe McConnell.
CHECK YOUR WORK
DRAWING CONCLUSIONS
CLEAN UP
DIRECTIONS:
Contents of bags:
Hand lens
Black paper
White paper
Photo of snowflakes
Spoon
Graduated cylinder and black base
3 bags: salt, sugar and pepper
CLEAN UP
DIRECTIONS:
Contents of bags:
Hand lens
Black paper
White paper
Photo of snowflakes
Spoon
Graduated cylinder and black base
3 bags: salt, sugar and pepper