Transcript Volcanoes and Igneous Activity Earth
Marine Hydrology
Topics:
1) Oceanography
a) Main oceans
2) Properties of seawater
1) Composition a) Salinity b) Sources of sea salt 2) Density 1) Factors that impact density 2) Temperature a) Cold water vs. warm water b) Layers of temperature
14.1
The Vast World Ocean
Oceanography
Nearly 71 percent of Earth’s surface is covered by the global ocean.
Oceanography
is a science that draws on the methods and knowledge of geology, chemistry, physics, and biology to study all aspects of world oceans.
14.1
The Vast World Ocean
Geography of the Oceans
The world ocean can be divided into four main ocean basins: • The
Pacific Ocean
is the largest and deepest • The
Atlantic Ocean
is about half the size of the Pacific and not quite as deep. • The
Indian Ocean
, largely a southern hemisphere body, is slightly smaller than the Atlantic. • The
Arctic Ocean
is the smallest and about 7% of the size of the Pacific.
15.1
The Composition of Seawater Salinity
Salinity
is the total amount of dissolved solid material in water.
Because the proportion of dissolved substances in seawater is so small, oceanographers express salinity as:
parts per thousand (ppt) Ex: 35g of salt per 1000 grams of water= 35 o / oo
Percentage of dissolved salts
Most of the salt in seawater is
sodium chloride
, NaCl
Average seawater salinity = 35 o / oo 30.6 % Sodium (Na) 55.0 % Chloride (Cl) 14.4% Other
15.1 The Composition of Seawater Salinity
Sources of Sea Salt
• 1) Chemical weathering and erosion
of rocks on the continents
• 2) Earth’s interior-
volcanic activity
15.1 The Composition of Seawater Salinity
Processes Affecting Salinity
• Processes that decrease salinity:
- Precipitation - Sea ice melting - Icebergs melting - Runoff from land
• Processes that increase salinity:
- Evaporation - Formation of sea ice
Processes that impact salinity
15.1 The Composition of Seawater
Ocean Temperature Variation
The ocean’s surface water temperature depends on the amount of solar radiation received, which is primarily a function of latitude.
Temperature Variation with Depth •
The
thermocline
is the layer of ocean water between about 300 meters and 1000 meters where there is a rapid change of temperature with depth.
Variations in Ocean Surface Temperature
Variations in Ocean Water Temperature
15.1
The Composition of Seawater Ocean Density Variation
Density is defined as mass per unit volume. It can be thought of as a measure of how heavy something is for its size.
Factors Affecting Seawater Density
•
Seawater density is influenced by two main factors: salinity and temperature.
15.1 The Composition of Seawater Ocean Density Variation
Density Variation with Depth
•
The
pycnocline
is the layer of ocean water between about 300 meters and 1000 meters where there is a rapid change of density with depth.
Variations in Ocean Water Density
Ocean Layering
Oceanographers generally recognize a three-layered structure in most parts of the open ocean: a shallow surface mixed zone, a transition zone, and a deep zone.
Surface Zone • Shallow (300 to 450 meters) • Zone of mixing • Sun-warmed zone
15.1
The Composition of Seawater Ocean Layering
Transition Zone • Between surface layer and deep zone • Thermocline and pycnocline Deep Zone • Sunlight never reaches this zone.
• Temperatures are just a few degrees above freezing. • Constant high-density water