Climate change Flashcards
Medieval Warming Period case stidy
Period in history when temperatures were warmer and thus European cultures flourished
Earth systems science
To recognize and perhaps modify the changes we have initiated, we need to understand how the entire Earth works as a system. The discipline, called Earth systems science, seeks to further this understanding by learning how the various components of the system—the atmosphere, oceans, land, and biosphere—are linked on a global scale and interact to affect life on Earth.
Monitoring
the regular collection of data for a specific purpose; real-time monitoring refers to collecting these data while a process is actually occurring.
Earth’s climate system,
defined as the system consisting of the atmosphere, hydrosphere, land surface, biosphere, and cryosphere (i.e., ice, snow, and frozen ground), which are linked and often interact with each other in complex ways
Climate
The characteristic atmospheric condition (weather) at a particular place or region over time periods of seasons, years, or decades.
Hadley cells
There are three cells of circulation (called Hadley cells, named after George Hadley, who first described them) in each hemisphere. Simplified, warm air rises at the equator and moves toward the poles, where it sinks after going through cell 2 (see Figure 18.6), and return flow is along the surface toward the equator.
troposphere
The lower, active part of the atmosphere, where weather occurs
The instrumental record
Starting about 1860, measurements of temperatures have been made at various locations on land and in the oceans
The historical record.
A variety of historical records go back several hundred years. Included are people’s written recollections (e.g., books, newspapers, journal articles, personal journals) of the Medieval Warm Period and the Little Ice Age, as well as ships’ logs, travelers’ diaries, and farmers’ crop records.
proxy data
refers to data that are not strictly climatic but that can be correlated with climate, such as temperature of the land or sea. Some of the information gathered as proxy data includes natural records of climate variability, as indicated by tree rings, ocean sediments, ice cores, fossil pollen, corals, and carbon-14
dendrochronology
Tree ring chronology
Coral reefs
consists of corals (and other organisms) that have hard skeletons composed of calcium carbonate (CaCO3) extracted by the corals from the seawater. The calcium carbonate contains isotopes of oxygen, as well as a variety of trace metals, that can be used to estimate the temperature of the water that the coral grew in. Thus, corals are a source of paleo-proxy data that can help us to interpret climate change. Corals may be dated by using several dating techniques, and a chronology of change over time may be constructed.
cosmic rays
come from outer space and are a product of the energy from the sun
Global warming
Refers to the hypothesis that the mean annual temperature of the lower atmosphere is increasing as a result of burning fossil fuels and emitting greenhouse gases into the atmosphere.
Milankovitch cycles
The question that begs to be answered is: Why does climate change? Examination of Figure 18.18 suggests that there are cycles of change lasting 100,000 years, separated by shorter cycles of 20,000 to 40,000 years