Definition: Weather refers to the state of the atmosphere at a given time, and can change minute by minute, hour by hour, or day by day.
Common inquiries: People often ask things like 'What is the weather like today?' or 'Will it rain tomorrow?', showing a focus on short-term conditions.
Components of Weather:
Temperature
Humidity
Precipitation
Cloudiness
Visibility
Wind
Importance of Weather Measurement: Countries worldwide gather data to:
Predict upcoming weather phenomena.
Identify weather patterns.
Assess historical weather data over time.
Prepare for severe weather events like snowstorms or heat waves.
Definition of Climate: climate is the average state of weather over a longer period, typically more than 30 years.
Key Differences:
Weather can alter rapidly (minutes to days); climate tends to change slowly (over decades).
Climate includes statistical averages and extreme weather ranges based on historical data.
Fields of Study:
Weather: Meteorology
Climate: Climatology
Climate Zones:
Climate zones on Earth include polar, temperate, arid, tropical, Mediterranean, and mountains/tundra/taiga, each having distinct climatic characteristics.
Historical Context: Ice sheets existed significantly across the Earth 25,000 years ago compared to today’s distributions.
Activity: Group activities to locate current ice-covered areas using an atlas for comparison with past locations.
Periods:
Ice Age: A prolonged period marked by widespread glaciers.
Glacial period: time when ice advances beyond normal polar limits.
Interglacial period: warmer periods with ice retreat.
Pattern: The Earth alternates between glacial and interglacial periods over the last 450,000 years.
The timeline of various ice ages includes significant fluctuations in Earth's climate.
Glacial Evidence: Boulders and rock formations indicate historical glacier activity through glacial deposits and scratches.
Pollen Analysis: Peat bogs serve as climate recorders; scientists analyze pollen layers to reconstruct historical climates and conditions over the millennia.
Early Atmosphere: Initially rich in carbon dioxide, with virtually no oxygen, composed mainly of water vapor, methane, and ammonia.
Evolution: Changes over millions of years led to the oxygen-rich atmosphere we have today due to photosynthesis by early microorganisms and plants.
Current Issues: Industrial activities have increased atmospheric carbon dioxide levels, contributing to climate change. Trees and plants serve as critical carbon sinks, but deforestation reduces their capacity to mitigate CO2.
Types:
Wind: Wind turbines generate electricity, but depend on consistent wind.
Tidal: Utilizing tidal movements to drive generators, limited to specific times.
Solar: Solar panels converted solar energy to electricity; restricted to daylight.
Bioplastics: Environmentally friendly alternatives to traditional plastics, made from renewable sources, help reduce fossil fuel use and environmental pollution from single-use plastics.
Greenhouse Effect: Increased levels of greenhouse gases (CO2, methane) trap heat and contribute to global warming, characterized by changes in climate patterns.
Mitigation: Emphasis on transitioning to renewable energy to reduce carbon emissions and enhance sustainability.