Heat Transfer in Earth’s Oceans WOW!, 3 meters of ocean water can hold as much energy as all other Earth Systems combined!

Slides:



Advertisements
Similar presentations
Making water move How it is mixed & transported
Advertisements

Weather.
Introduction to Oceanography
Ocean Currents – PART 2. Surface Currents Are Driven by the Winds  Winds that drive the ocean’s surface currents:  The westerlies  The trade winds.
Earth Science 16.1 Ocean Circulation
Global Wind Patterns and Weather & Weather Basic
Earth’s Climate System (part 2) revisiting the radiation budget heat capacity heat transfer circulation of atmosphere (winds) Coriolis Effect circulation.
Atmosphere 78% nitrogen, 21% oxygen. Water Vapor up to 4% by volume leaves atmosphere as dew, rain or snow.
Review - Precipitation is caused by the uplift of moist air Air rising along the ITCZ or weather fronts (convergence) Convection caused by intense surface.
Earth Systems Science Chapter 5 OCEAN CIRCULATION I: SURFACE Winds, surface currents Flow within gyres: convergence, divergence, upwelling, downwelling,
General Circulation and Climate Zones Martin Visbeck DEES, Lamont-Doherty Earth Observatory
Oceans, Currents, and Weather Dynamics
Atmosphere 78% nitrogen, 21% oxygen. Water Vapor up to 4% by volume leaves atmosphere as dew, rain or snow.
Ocean Currents.
More Climatic Interactions
General Atmospheric Circulation
Unit 2: Climate Winds and Climate
The direction of the winds The Coriolis effect
“ What Causes Our Weather” n I. Factors that cause weather : A. Weather-Is the present state of our atmosphere. B. What causes our weather? 1. The interaction.
ATMOSPHERE Air Circulation
“ I. What Causes Our Weather” 1. Weather-Is the present state of our atmosphere. 2. The interaction between the earth’s air, water, land and the sun causes.
Video Field Trip 1. How are waves created? 2. Describe the way in which the moon influences the tides.
Lecture 5– Climate. Meteorology: Study of climate and weather Weather: daily variations in precipitation, winds, temperature, etc. Climate: overall combination.
Global Circulation and El Nino
Ocean Circulation Winds and Currents. The __________________ and the ___________________ interact The ocean and atmosphere transport heat from the ______________________________.
Earth's Atmosphere Troposphere- the layer closest to Earth's surface extending roughly 16 km (10 miles) above Earth. Densest – N, O, & water vapor Stratosphere-
Global and Local Winds.
Ocean Currents.
Surface Currents Movement of water that flow in the upper part of the ocean’s surface.
Welcome to Class Define radiation, convection, and conduction.
Latitude structure of the circulation Figure 2.12 Neelin, Climate Change and Climate Modeling, Cambridge UP.
The General Circulation of the Atmosphere and Oceans ATS 351 Lecture 9 November 2, 2009.
Ocean Currents.
Global Climates and Biomes
Lecture #2 Weather. Convection and Atmospheric Pressure Much of solar energy absorbed by the Earth is used to evaporate water. – Energy stored in water.
Ocean Currents Ocean Density. Energy in = energy out Half of solar radiation reaches Earth The atmosphere is transparent to shortwave but absorbs longwave.
19.2 Pressure Centers & Wind
Atmospheric movements We learned that energy is transferred from the Sun to the Earth creating convection currents. But, what type of currents???
Climate Climate is the average weather over a long period of time – Weather is the current condition of the atmosphere – Factors affecting weather/climate.
© 2011 Pearson Education, Inc. CHAPTER 6 Air-Sea Interaction.
Do Now: Analyze the following images
Introduction to Meteorology UNIT 10 STANDARDS: NCES 2.5.1, 2.5.2, 2.5.3, 2.5.4, 2.5.5, LESSON 1.
Solar Energy & The Greenhouse Effect The driving energy source for heating of Earth and circulation in Earth’s atmosphere is solar energy (AKA the Sun).
Ocean Currents.
Wind and the Ocean. Wind Currents of air Develop when two adjacent bodies of air have different densities. Denser air sinks, pushing less dense air upward.
Ocean Currents p. 36 Ocean waters are constantly on the move. How they move influences climate and living conditions for plants and animals, even on land.
Section 1.2 The Causes of Weather
Welcome to Class Define radiation, convection, and conduction.
Art or Science?. Explain the thermal transfers of energy within oceans and the importance of oceanic conveyor belts.
1 0º Equator90º Pole LP HP  At the Equator the atmosphere is heated  Air becomes less dense and rises.  Rising air creates low pressure at the equator.
Ocean Currents. The water in the ocean is constantly moving The water in the ocean is constantly moving Broad bands of ocean water that flow in one direction.
Ocean Circulation. Ocean Currents Ocean currents Surface currents –Affect surface water within and above the pycnocline (10% of ocean water) –Driven.
GCM’s Heating of the Earth Uneven Solar Energy Inputs: Earth is heated unevenly by the sun due to different angles of incidence between the horizon and.
Chapter 4 Global Climates and Biomes. Global Processes Determine Weather and Climate Weather- the short term conditions of the atmosphere in a local area.
Fact Statements.  Surface currents are mainly caused by prevailing winds.  Their flow is controlled by the winds, Earth’s rotation and location of the.
Latitudinal effects Intensity of insolation is not the same at all latitudes Earth is roughly spherical, so insolation passing through 1 m 2 screen –Illuminates.
Chapter 4 Global Climates and Biomes. Global Processes Determine Weather and Climate Weather- the short term conditions of the atmosphere in a local area.
Ocean Circulation Winds and Currents. The atmosphere and the oceans interact The ocean and atmosphere transport heat from the equatorial regions to the.
Wind and Ocean Circulation currents.swf
Ocean Currents What causes them?
Chapter 16.1 Ocean Circulation.
Ocean-Air Interaction
Currents and Climate.
Ocean Currents: 4 causes
Currents and Climate.
Ocean Currents.
“ What Causes Our Weather”
Currents and Climate.
“ What Causes Our Weather”
Presentation transcript:

Heat Transfer in Earth’s Oceans WOW!, 3 meters of ocean water can hold as much energy as all other Earth Systems combined!

Tropical air rising Warming air = lower density+increasing volume Rising air = lower pressure, lower temperature Condensation = warming Result: tremendous rainfall along the equator

Surface Ocean – Temp. is variable -2 to 30°C Deep ocean – Temp. is stable -1 to 4°C Average Temp. of the world ocean is 3.8°C 200 m

Sinking air Hadley Cell 0° Latitude Hot, humid 30° latitude Hot, dry (desert belt)

Surface ocean circulation Solar radiation Large heat capacity Heat variations lead to changes in pressures Air circulation (wind) –Gyres

Tropical Gyre Driven by wind –Trade winds –Westerly movement –Counter clockwise (CCW) direction (northern hemisphere)

Subtropical Gyre Very active evaporation –A product of warm/dry air moving over the oceans and land masses Results in a warm and salty Gulf Stream The gyre moves in a clockwise (CW) direction in this region.

Sub Polar Gyre Tremendous transfer of heat from the ocean to the atmosphere. –This warms the rising air that travels northeast and through northern Europe. –The Erbinger Current (Norwegian/Greenland Sea)

General surface current movements Winds mix and transport warm waters through the Earth’s oceans –Depth of 100 m –Average depth of 4000 m Warm water is circulated from the tropics towards the poles Coriolis force

Movement beneath the surface Coriolis force –Pushes the underlying water –Through a depth of 100 m –Friction drives the downward spiralling water further to the right (Nh) or left (Sh)

Subpolar sink Water becomes cold and salty (increase in density) to the north of Greenland. This cold dense water sinks creating vertical movement –Supplies the deep ocean with circulating water

Northern sub polar gyre

Southern Hemisphere This vertical movement also occurs in the southern hemisphere –Weddell Sea –Both movements (north and south) occur in the Atlantic ocean

Polar water/ice Ice is fresh water Circum-Antarctic Current: Flows around Antarctica –Circulates from west to east –4000 cubic meters of water –Insulates Antarctica (keeps it cold) This circulation pattern has a huge effect on global climate.

Deep Water Circulation Deep water goes from the North Atlantic to the North Pacific. Surface water flows opposite of the deep water pattern The deep cycle is about 800 to 1000 years. Surface water cycles occur on the order of decades.

Water and The Global Water Cycle Largest bulk chemical transfer on Earth Important to heat transfer from the Equator (evaporation) Patterns control regional distribution rainfall in terrestrial environments Movement of water is a function of evaporation and precipitation of two pumps. –Biologic –Physical

The Biological Pump Operates on feedback Nutrients + H20 +CO2 → organic matter + O2 Photosynthesis, CO2 Evapotranspiration O2 + H2O Nutrients, soil

Biologic Pump, negative feedback When there is ample water the inner cell is enlarged and promotes evapotranspiration When water is short the inner cell is closed allowing for the absence of evapotranspiration

Water budget Ocean (1,350,000) = 97% of the total water 425, ,000 40,000 Ice Ground water 8,200,000 27,500,000 Rivers, 40,000 Atmosphere = 13,000 Units Km 3 : 1m water = metric tons, 50 * 1000 Km 3 = 10 18

Longer residence time for the land system Stock / flux – Residence time of water in the atmosphere –13,000 (atmosphere) / 425,000 (evaporation) = 0.3 years × 52 weeks Residence time in the oceans –1,350,000,000/425,000 = 3176 years

Calculate the residence time of land. Add the stocks and divide by the flux 357,040,000/425,000 = 840 years There are more stocks than listed here so the value of 840 years will be an underestimate.

Calculating the average evaporation and precipitation Ocean: –100 cm/yr, evaporation –70 cm/yr, precipitation Tropics –4mm/day (precipitation is skewed to the tropics because this zone account for 50% of the runoff on Earth Poles –X≤1mm/day, Desert belt 0% rain leads to little to no runoff.

The Jungle effect (Tropics) Trade winds The Amazon Basin Bio-enhanced cloud formation, This is a water trap set up by biologic activity Ocean Amazon River The Amazon and Oronoco flow systems are responsible for 20% of Earth’s runoff

Physical Pump Summer –Rainy season –Drives major rivers –Monsoons in India Winter –The ocean surface circulation follows wind patterns moving away from land