Temporary behavior of atmosphere (what's going on at any certain time)
Small geographic area
Can change rapidly
Climate
More than "the average state of the atmosphere" because a complete climate description should also include variations and extremes to accurately portray the total character of an area
The most important elements are temperature and precipitation since they have the greatest influence on people and their activities and also have as important impact on the distribution of vegetation and the development of soils
"Warming of the climate system is unequivocal, human influence on the climate system is clear ..."
Global warming
The increase of the Earth's average surface temperature due to a build-up of greenhouse gases in the atmosphere
Climate change
A broader term that refers to long-term changes in climate, including average temperature and precipitation
September 2023 ranked as the warmest September in NOAA's 174-year global climate record
2020 2nd warmest
17 of the top 18 warmest years on record have all been since 2001 (except 1998)
Average global temperatures have increased by about 1.09°C (1.9°F) since 1880
Climate trends
The diurnal temperature range decreased. (Tmin (=night) increasingtwice as fast as Tmax (=day))
Precipitation trend = + 5–10% for 30–85°N since 1900
Sea level rise = +18.5cm since 1900
Snow cover extent has generally decreased
Sea level rise
Global average sea level has risen 8–9 inches (21–24 centimeters) since 1880
Glacier retreat
Muir Glacier retreated more than 7 miles and thinned more than 2600 feet from 1941 to 2004
Arctic sea ice
September extent has decreased
If all permafrost thaws: 3–10 cm (1–4 in) sea level rise
If all the (freshwater) seaice would melt: 4 cm (1.5 in) sea level rise
If all of Greenland's ice sheet melted: 6.5 m (21 ft) sea level rise
If all of the Antarctic ice sheet melted: ~60 m (197 ft) sea level rise
If the entire cryosphere thawed/melted: 67 m (220 ft) sea level rise
Substantial areas of coastal plains would be flooded worldwide
Causes of climate change
Natural mechanisms: solaroutput, earth-sunrelationships, movement of continents, atmosphere/oceanvariability, volcanic activity
Human mechanisms: land use/land cover change, changing atmospheric chemistry
Radiative forcing
Measure of the climatic impact of a greenhouse gas or other forcing agent
Major types of radiative forcings
Changes in greenhouse gases
Changes in aerosols (particles)
Changes in surface albedo
Changes in contrails
Changes in solar variability
Changes in volcanic activity
Radiative forcing gives a first-order estimate of the relative climatic forcing of anthropogenic gases, aerosols, land-use change
Feedbacks
Ice-albedo feedback: positive
Cloud feedbacks: positive or negative
Land surface feedback: positive (deforestation and hydrological cycle)
Water vapor feedback: positive
General Circulation Models (GCMs)
Numerical climate model that simulates Earth's circulation, physical processes in the atmosphere, ocean, cryosphere and on land surface, to project future climate, understand past climate, and identify causes and effects
Data for climate models comes from weather balloons, satellites, airplanes, radar and other ground-based instruments measuring wind, precipitation, temperature, humidity, etc. Reliable records have been kept since the 1800s.
Climate scenario
A coherent, internally consistent and plausible description of a possible future state of the world, not a forecast
Climate models can correctly replicate recent warming only if they include human influences
Projected changes
Maximum warming in high northern latitudes
Warming is largest in cold season
Precipitation will likely increase (decrease) in some regions 10 to 20%
Decrease in snow cover, and sea-ice thickness + extent
More frequent and intense heat waves, droughts, and heavy precipitation
Tropical cyclones may be more intense
Projected temperature rise: 1.0–3.7°C by 2100
How climate change will affect people
Sea-level rise
Ecosystem change, effect on species and farming
Melting of polar ice, effect on shipping and wildlife