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Energy Pathways and Principles: |
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Shortwave energy from the Sun enters Earth’s atmosphere – Longwave energy is radiated from Earth |
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Passage of shortwave and longwave energy through atmosphere or water |
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the equator, lower at poles |
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– Energy that bounces off surface and is returned – Earth and its atmosphere reflects an average of 31% of all insolation |
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– Reflective quality of a surface – Percentage of insolation that is reflected – Darker colors have lower albedos (less reflective) – Lighter colors have higher albedos (more reflective) |
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Cloud-albedo forcing occurs when |
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clouds cause an increase in albedo: |
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Cloud-albedo forcing occurs when clouds cause an increase in albedo: |
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– Incoming shortwave radiation from Sun is reflected back towards space by clouds – Industrial aerosols can also reflect insolation |
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Cloud-greenhouse forcing occurs when |
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clouds act to increase greenhouse warming: |
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Cloud-greenhouse forcing occurs when clouds act to increase greenhouse warming: |
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Traps longwave radiation emitted from Earth |
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But greater surface cooling since |
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not as much solar radiation reaches Earth |
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the assimilation of radiation and its conversion from one form to anothe |
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Insolation that is not reflected is |
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absorbed and converted into longwave radiation |
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Temperature of absorbing surface |
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Absorption also occurs in |
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atmospheric gases, dust, clouds and stratospheric ozone |
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Some insolation also absorbed by |
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– Molecule-to-molecule transfer |
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– Energy transferred by movement |
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– Horizontally dominant movement |
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– Energy traveling through air or space |
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Radiation,Advection,Convection,Conduction |
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greenhouse in that it delays the transfer of heat from Earth into space |
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Outgoing shortwave flux is |
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lower over equatorial waters where more shortwave radiation is absorbed |
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Water and continents near equator return |
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higher flux of longwave energy to space |
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– Heat that we can feel – Determined by heat capacity (cal/gm/ oC) of a substance |
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– Heat that is absorbed or released due to phase changes – Ice to water (80 cal/gm absorbed) – Water to vapor (540 cal/gm absorbed) |
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When you heat a substance, |
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it stores heat by getting hotter |
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Different substances have different heat capacities |
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Some substances can store more heat than others |
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Substance and heat capacity (cal/gm/oC) |
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– Water 1.0 – Wet mud 0.60 – Ice 0.50 – Sandy clay 0.33 – Dry air 0.24 – Quartz sand 0.19 – Granite 0.19 |
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Example: – Water has a heat capacity of 1.0 cal/gm/oC – Land has a heat capacity of 0.2 cal/gm/ oC – Question? If I put one calorie (cal) of heat into 1 gram (gm) of water or land, how does the temperature of each change? |
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the balance between incoming and outgoing radiation |
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There is a ______ imbalance in net radiation: |
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There is a latitudinal energy imbalance in net radiation: |
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– Positive values at low latitudes (energy surplus) – Negative values poleward of 36o north and south latitudes (energy deficits) |
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low latitudes is transported poleward via air and ocean currents |
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Net radiation at Earth’s surface is a balance between |
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incoming and outgoing radiation: |
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Net radiation at Earth’s surface is a balance between incoming and outgoing radiation: |
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– Surface receives visible shortwave (+SW) and longwave (+LW) radiation – Surface also reflects visible (-SW) and radiates longwave (-LW) radiation |
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After heating of a non-vegetated surface (land and water), NET R at the surface gradually |
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decreases via three pathways of heat removal: |
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After heating of a non-vegetated surface (land and water), NET R at the surface gradually decreases via three pathways of heat removal |
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Sensible heat within bedrock and soil is transferred to the ground surface by conduction – Atmospheric convection removes sensible heat from the surface via rising air masses to higher altitudes – Latent heat of evaporation absorbs heat energy at the surface during phase change from liquid to vapor |
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Global Sensible Heat at Surface Level |
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Global Latent Heat of Evaporation |
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Greater over water & wetter land areas |
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Variations in the expenditure of NET R |
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among sensible heat, latent heat, and ground heating and cooling produces the variety of environments in nature: |
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High sensible, low latent heat |
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Moist, vegetated environments |
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High latent, low sensible heat |
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Urban areas have on average both maximum and minimum temperatures higher than nearby rural settings |
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Why urban areas are warmer |
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Surfaces typically metal, glass, asphalt, etc. – Irregular geometric shapes cause incoming insolation to be caught in maze-like reflection and radiation ‘canyons’ – Human activity such as electricity production, burning of fossil fuels, and heating during winter – Sealed so that water does not reach soil; more runoff, less long-term moisture and fewer vegetation – Urban air pollution absorbs more infrared radiation |
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– Melting point of ice 32o F – 180 divisions to the boiling point water at 212o F |
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– Melting point of ice 0o C – Boiling temperature water at sea level 100o C |
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Proportional to actual kinetic energy in material – Starts at absolute zero temperature – Melting point for ice 273 K – Boiling point of water 373 K |
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Mercury thermometer or alcohol thermometer |
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– Fluid stored in sealed glass tube – Fluid expands when heated, contracts when cooled – Calibrations measure amount of expansion or contraction |
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– Measures temperature by sensing electrical resistance of a semiconducting material – Resistance changes 4% per oC – Temperatures reported electronically to a weather station |
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– Affects insolation (more diffuse at higher latitudes) |
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– High altitude has greater daily range – High altitude has lower annual average |
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– High albedo – Moderate temperatures – cooler days, warmer nights |
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An estimated ____ of all evaporation on Earth is from the _____ |
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heat energy is absorbed as latent heat |
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This evaporative heat loss causes |
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temperatures at marine locations |
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Solid ground is opaque Water is transparent: |
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Water has a higher specific heat Land has a lower specific heat |
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Water has a higher specific heat |
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Land has a lower specific heat |
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Holds less heat than water |
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Land is rigid and solid, whereas water is fluid and capable of movement – Oceans thus are able to mix cooler and warmer regions effectively |
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Oceans moderate atmospheric |
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temperatures through negative feedback: |
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Higher ocean temperatures produce greater |
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water vapor in overlying air mass |
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air to absorb longwave radiation increases |
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However, greater cloud formation reflects |
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more insolation, producing lower temperatures |
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of air reduces evaporation rates and the ability of the air mass to absorb water vapor |
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temperature conditions more moderate--water warms and cools slowly |
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temperature conditions more extreme---and land warms and cools rapidly |
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Correlates cold and wind speed |
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Correlates heat and humidity |
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Holding actual air temperature constant, |
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higher wind speed results in higher wind chill |
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Holding actual air temperature constant |
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higher humidity results in higher heat index |
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Changing direction of light's movement within the atmosphere without altering its wavelengths is known as ________. |
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Insolation at Earth's surface is higher near the poles than along the equator. |
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which of the following has the highest albedo? |
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Which of the following can result in the cooling of Earth's surface? |
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Cloud-albedo forcing where increasing cloud cover causes an increase in atmospheric albedo |
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How do greenhouse gases like carbon dioxide and water vapor warm the atmosphere? |
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Greenhouse gases delay the transfer of longwave radiation from Earth into space |
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How is latent heat transferred from surface water to the atmosphere? |
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Conduction is the principle way of transferring sensible heat... |
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Which of the following statements more likely applies to land than water? |
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heats up faster during the day and cools down faster at night |
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Which of the following correlates the effects of air temperature on the human body with wind speed? |
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On land, the highest annual values for latent heat of evaporation occur in ________ and the highest values for sensible heat occur in ________. |
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Tropical rain forests/subtropical deserts |
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On a sunny summer afternoon, at which of the following locations would temperatures be highest? |
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