Chapter 19 & 20 - Global Climate Change & Geology, Society, and the Future Flashcards
(60 cards)
- famous Earth scientist interested in the history of life on Earth, human impact on the environment, and the use of resources, proposed two central goals for Earth sciences:
- Understand how Earth works and how it has evolved from a landscape of barren rock to the complex landscape dominated by the life we see today.
- Apply that understanding to better manage our environment
Preston Cloud
studies how the Earth’s interconnected systems interact and influence life on a global scale.
Earth Systems Science
Tools for Studying Global Change
- The Geologic Record
- Real Time Monitoring
- Mathematical Models
● Organic material in sediment provides a timeline and insights into past climates, life, and environmental changes.
● Glacial ice, with trapped air bubbles, offers crucial data on past atmospheric CO2 and CH4 levels, making the geologic record essential for understanding Earth’s history and long-term environmental changes.
The Geologic Record
● Monitoring is the regular collection of data for a specific purpose.
● Real-time monitoring refers to collecting these data while a process is actually occurring.
● Gathering of real-time data is necessary for testing models and for calibrating the extended prehistoric record derived from geologic data
Real Time Monitoring
● use numerical methods to represent real-world phenomena and the interactions between processes
● They predict surface water and groundwater flow, sediment transport, ocean currents, and atmospheric circulation based on physical principles like energy and mass conservation.
- Mathematical Models
- refers to the long-term atmospheric conditions of a specific region, spanning seasons, years, or even decades.
- It involves more than just average temperature and precipitation-factors like humidity, wind patterns, and seasonal variations all contribute to the complexity of a region’s climate
Climate
The _____________ surrounds the Earth and holds the air we breathe; it protects us from outer space; and holds moisture (clouds), gases, and tiny particles
atmosphere
Atmosphere Consists mainly of:
Nitrogen - 78%, Oxygen - 21%, Argon - 0.9%, Carbon Dioxide - 0.03%, Trace Elements <0.07%
Also contains compunds (methane, ozone, etc.) and pollutants.
Water vapor varies between 0% and 4% in the lower atmosphere
- is a process that occurs when gases in Earth’s atmosphere trap the Sun’s heat.
- this process makes Earth much warmer than it would be without an atmosphere.
GREENHOUSE EFFECT
● About a third of the Sun’s energy is reflected into space, while the rest is absorbed by Earth’s surface, warming
it.
● The atmosphere transmits outgoing infrared radiation, with most emitted near its upper levels after scattering and absorption by greenhouse gases. A slight energy imbalance (about 1 W/m2) due to greenhouse gases warms the atmosphere and oceans while melting glaciers.
GREENHOUSE EFFECT
➔ Glacial events reshape landscapes during low temperatures, while high temperatures mark interglacial periods, which have varied over 150,000 and 18,000-year cycles.
The cold period that occurred about 11,500 years ago is known as the _________________, followed by rapid warming to the Holocene maximum, which preceded the Little Ice Age.
➔ Since around 1750, a warming trend began, followed by slight cooling in the 1940s. Over the past 100 years, global mean temperature has risen by about 0.8°C.
Global Temperature Change
Younger Dryas
Why Does Climate Change?
➔ Earth’s movement wobbles like a top, altering its position relative to the Sun and the solar radiation it
receives.
➔ Identified by Milutin Milankovitch in the 1920s, these cycles explain long-term climate trends but alone cannot account for large-scale changes.
➔ As natural climate forcing mechanisms, they contribute to global climate shifts when combined with other
processes
Milankovitch Cycles
- it is an imposed change of Earth’s energy balance. It can be positive if a particular forcing increases global mean temperature or negative if temperature is decreased.
Climate forcing
solar variation influences Earth’s climate, with increased radiation linked to the Medieval Warm Period (A.D. 1000-1300) and minimal activity marking the Little Ice Age. However, the effect is small, with only a 0.25% difference in solar forcing over the past 1,000 years.
Solar forcing
volcanic eruptions release aerosols into the atmosphere, which spread globally and reflect sunlight, causing cooling that can counteract some greenhouse warming.
Volcanic forcing
human-driven climate change includes recent warming of 0.2°C per decade, which
exceeds natural climate variability. Industrial-era forcing is primarily due to increased CO2 and other greenhouse gas emissions. Natural factors alone cannot explain the nearly 1°C rise in global temperature over the past century, but when combined with human influences, the observed changes become more consistent.
Anthropogenic forcing
● Unit for the forcing is W/m² (watts per square meter).
● It can be positive if a particular forcing increases global mean temperature or negative if temperature is
decreased.
Climate forcing (concept)
refers to the response of climate to a specific climate forcing after a new equilibrium has been established.
Climate Sensitivity
Unit for climate sensitivity is °C/(W/m²)
is the time required for the response to a forcing to occur
Climate response time
The ocean conveyor belt, also known as ___________________, is a system of ocean currents driven by differences in water density, which are caused by variations in temperature and salinity.
thermohaline circulation
Whirlpools of water trapping huge collections of trash in their currents
Gyres
Home of the Great Pacific Garbage Patch
Estimated 3.2 million tons of trash
Located Between Hawaii and California
North Pacific Gyre
POTENTIAL EFFECTS OF GLOBAL CLIMATE CHANGE
- Melting of Glacial Ice and Sea Ice and Thawing of Permafrost with Global Warming
- Climate Patterns Desertification
- Climate Patterns El Nino
- Sea Level Rise
- Adaptation of Species to Global Warming
- Changes in the Biosphere
- Strategies for Reducing the Impact of Global Warming