Solar System Astronomy Earth Lecture 2

Solar System AstronomyEarth Lecture 2

Earth’s Interior, Plate tectonics, Climate, Atmosphere, Global

warming

Overview of Earth’s Interior

Interior Temperature Increases with Depth

Earth’s Magnetic Field

Current position of N magnetic pole

Motion of Magnetic poles

North magnetic pole is now moving N about 15 km/yr

1000 km

Daily Magnetic pole motion

100 km

Sir John Ross (1831) first discovered N magnetic pole while exploring the Arctic. He was trapped in the polar ice for 4 years (!) and made magnetic observations to

pass the time.

Aurora

Solar wind electrons precipitate into polar regions, ionizing nitrogen and oxygen atoms

University of Iowa VIS Auroral Imager Instrument

Auroral Imaging movie from Polar VIS Instrument

Plate Tectonics

Continental DriftNorth American plate moves 50 cm per year

Continental drift:

Historical Maps

Movie of Continental Drift

Time (Myr)

Alfred Wegener and Continental Drift: Embattled Scientist

A. Wegener (1880-1930)

Wegener first proposed continental drift theory in 1915. It was soundly rejected, and only became accepted after his death

Earthquake zones vs. Tectonic Plates

Principle of the Seismograph

San Andreas Fault

The San Andreas Fault is a transform fault margin that separates the Pacific plate from the North American plate. Directions of motion are shown by the arrows. Los Angeles, on the Pacific plate, is moving north, while San Francisco is moving south, bringing the two cities closer together at a speed of 5.5 cm/y; they will be adjacent about 10 million years in the future.

Locating an earthquake epicenter using seismic waves

Seismic Risk Map of U.S.

Note: This map does not indicate frequency of earthquakes

Earth’s atmospheric gases

Earth at early epochs had 500-1000x (15%-30%) CO2 than current levels (0.03%)

Transmission of atmosphere versus wavelength

Ozone blocks harmful UV: skin cancersCO2 blocks

IR: global warming

Infrared Visible Ultraviolet

UV Protection from

Atmospheric Oxygen Isotopes

Greenhouse effect

Comparison of Greenhouse effect on terrestrial planets

Atmospheric carbon dioxide concentration 1950-2000

Atmospheric C02 versus CO2 emission from fossil fuels

Global land temperature 1860-1997

From the late 1860s to the early 1940s, the annual mean temperature rose about 0.6 degrees C. From the early 1940s to 1965 the temperature declined about 0.2 degrees C and since 1965 the trend has been upward. The overall rise during the century and a quarter of record is ca. 0.85 degrees C. The decade of the 1990’s has been the warmest on record

Future Effects of global warming by CO2

Predicted global temperature increase for doubling CO2

Northern hemisphere Winter (C)Northern hemisphere Summer (C)

Model of Precipitation Changes caused by doubling CO2 concentration

Long-term global temperature variations

Variations in the oxygen-isotope ratio through the Greenland Ice Sheet. The zone of strongly negative values beginning about 70,000 years ago and ending about 10,000 years represents the last glaciation. The pronounced shift in values about 10,000 years ago marks an abrupt change from glacial to interglacial climate at the end of the glaciation.

Glaciation Cycles Measured by

Oxygen Isotope ratios

Curve of average oxygen-isotope variations during the last 2 million years based on analyses of deep-sea sediment cores. The curve illustrates changing global ice volume during successive glacial-interglacial cycles of the Quaternary Period

North America during last glaciation (10,000 BCE)

Des Moines lobe

Europe during last glaciation(20000 BCE -10000 BCE)

Affect of glaciation on trees species

Simplified pollen diagram prepared from data collected at Rogers Lake, Connecticut. Variations in pollen influx are plotted as a function of time, and show progressive changes in forest composition.

Greenland ice core acidity records of Volcanic eruptions

Acidity record from a Greenland ice core showing peaks in sulphuric-acid precipitation attributable to major volcanic eruptions. The largest acid peak dates to 1815-1816, the time of the huge Tambora eruption in the East Indies, which produced "the year without a summer" (1816). The volcanic dust and gases in the stratosphere reduced northern hemisphere temperatures at least 0.7 degrees C.

Effects of volcanic eruptions on global temperature

My. Pinatubo eruption June, 1991 (Phillipines)