0
Term climate cycles refer to long-term variations in climate patterns that can last for decades to centuries. These cycles include phenomena such as the Milankovitch cycles, which are driven by changes in Earth's orbit and axial tilt, and can influence glacial and interglacial periods. Other examples include oceanic cycles like El Niño and La Niña, which can affect global weather patterns. Understanding these cycles helps scientists predict future climate behavior and assess the impacts of climate change.
What else can I help you with?
How does earth's orbit influence climate?
Earth's orbit influences climate primarily through variations in its shape (eccentricity), tilt (obliquity), and axial precession. These changes affect the distribution and intensity of sunlight received by different parts of the planet, leading to cycles of glacial and interglacial periods, known as Milankovitch cycles. For instance, increased tilt can enhance seasonal contrasts, while a more circular orbit can lead to milder climate variations. Together, these orbital changes significantly impact long-term climate patterns and trends.
Do scientist classify nitrogen carbon and water cycles as bio geochemical cycles?
Yes, scientists classify the nitrogen, carbon, and water cycles as biogeochemical cycles. These cycles involve the movement of essential elements and compounds between living organisms, the atmosphere, soil, and water in Earth's ecosystems. They play a vital role in sustaining life and regulating the Earth's climate.
What process is associated with long term cycle?
The process associated with long-term cycles is typically referred to as "cyclic succession" or "ecological succession." This involves gradual changes in ecosystems over extended periods, where communities of organisms evolve and replace one another in a specific sequence. Factors such as climate change, geological shifts, and human activities can influence these long-term cycles, leading to shifts in biodiversity and ecosystem structure. Examples include the carbon cycle and the water cycle, both of which operate over long timeframes and are crucial for sustaining life on Earth.
How does earths position cause climate change?
Earth's position in its orbit around the sun, as well as its tilt on its axis, determine the distribution of sunlight and thus the seasons. Climate change is mainly caused by human activities that release greenhouse gases into the atmosphere, trapping heat and leading to overall warming. Variations in Earth's orbit and tilt contribute to long-term climate cycles, but human influence is the primary driver of current rapid climate change.
Long-term variations in weather for a particular area make up the of an area?
climate
What can influence the climate of a continent?
Sun Cycles Ocean Cycles Cosmic Cycles
How long do business cycles last?
It varies, but there are short-term cycles that lasts probaly 36 moths or so. But there are long term cycles that some say swing in long about 50 year cycles, but these thing vary.
What is the scientific term for the rate at which waves oscillate in cycles?
The scientific term for the rate at which waves oscillate in cycles is frequency. It is measured in hertz (Hz), which represents the number of cycles per second.
Why don't global warming experts reference the Milankovitch cycles?
Because Milankovitch cycles cannot explain climate variability over the time scale that we're interested in predicting climate. Milankovitch cycles can explain large variations in climate over very long time scales, scales of thousands of years. Milankovitch cycles do not explain variability in climate on the scales of hundreds or tens of years. Variability at smaller time scales is driven by other factors, such as carbon dioxide (CO2) and other greenhouse gas concentrations.
How does earth's orbit influence climate?
Earth's orbit influences climate primarily through variations in its shape (eccentricity), tilt (obliquity), and axial precession. These changes affect the distribution and intensity of sunlight received by different parts of the planet, leading to cycles of glacial and interglacial periods, known as Milankovitch cycles. For instance, increased tilt can enhance seasonal contrasts, while a more circular orbit can lead to milder climate variations. Together, these orbital changes significantly impact long-term climate patterns and trends.
What are the driving forces of climate?
solar cycles and ocean currents are two of the main things
How do milankovitch cycles affect climate?
The Milankovitch cycles consist of the Procession or Wobble of the axis (24,000 years); the Eccentricity (100,000 years); and the Tilt (41,000 years). The Procession determines if the earth is closest or farthest away from the sun in winter; the Eccentricity determines how great the solar insolation will be when the earth is close to the sun; and the Tilt determines how extreme seasons will be. The larger, the tilt the more extreme. All these cycles in concert provide forcing that has led to periods of glaciation in the past. Feedback cycles are important also in allowing winter-time snow to last through the Northern Hemisphere summer above 65 N latitude. Bottom line - astronomical forcing was one of the primary drivers of creating past ice ages (which are large changes in climate).
What is the term for vibrates in cycles per second in music?
Pitch.
Who are responsible for climate change and how?
No one is responsible. It is just nature. Climate change has been happening for millions of years. The earth goes through cycles.
What is the medical term meaning gradual ending of menstruation?
You need to have a talk to your boyfriend/partner
How many years is climate measured?
Usually at least 30 and anywhere up from that, especially in terms of climate change. Climate is different to weather which is day to day change in temperature and rainfall etc but climate is an average of weathers over at least 30 years.
Which one doesn't have a shortterm biogeochemical cycle carbon nitrogen oxygen phosphorus?
Carbon has both short-term and long-term biogeochemical cycles, while nitrogen, oxygen, and phosphorus have primarily long-term biogeochemical cycles. These elements are cycled through various reservoirs in the environment, but the rates at which they move through these cycles differ.
