practice exam
... a) only up and down b) only back and forth c) in circular orbits 38) The distance over which the wind blows to create waves is termed: a) fetch b) distortion c) convection d) defraction e) refraction 39) (True or False) The flood tide occurs as water flows out after high tide. 40) (True or False) St ...
... a) only up and down b) only back and forth c) in circular orbits 38) The distance over which the wind blows to create waves is termed: a) fetch b) distortion c) convection d) defraction e) refraction 39) (True or False) The flood tide occurs as water flows out after high tide. 40) (True or False) St ...
THE Neritic zone and open ocean
... deep floor. In 1977, scientists diving in Alvin to the Galapagos Rift discovered a new community of organisms. These organisms can withstand tremendous pressure, high temperatures, utter darkness, and toxic chemicals. They are called extremophiles because of their extreme living conditions. ...
... deep floor. In 1977, scientists diving in Alvin to the Galapagos Rift discovered a new community of organisms. These organisms can withstand tremendous pressure, high temperatures, utter darkness, and toxic chemicals. They are called extremophiles because of their extreme living conditions. ...
(LOW) variability
... modes and the South Atlantic response to El Niño-Southern Oscillation induced climate variability. 2. A regional ocean model is used to investigate variability in the south east Atlantic, especially in the Angola Benguela Frontal Zone. Results: 1. A Rotated Empirical Orthogonal Function analysis of ...
... modes and the South Atlantic response to El Niño-Southern Oscillation induced climate variability. 2. A regional ocean model is used to investigate variability in the south east Atlantic, especially in the Angola Benguela Frontal Zone. Results: 1. A Rotated Empirical Orthogonal Function analysis of ...
Geography Lesson Tectonics Tuesday * The largest earthquakes
... Geography Lesson Tectonics Tuesday ...
... Geography Lesson Tectonics Tuesday ...
Ocean Currents of the Eastern Gulf of Mexico Robert H. Weisberg
... 1. The eastern G of M deep-ocean circulation consists of the LC/FC/GS system, which is always present. Materials entrained in the LC can quickly flow through the Florida Straits in proximity to the Florida Keys and the east coast. 2. The WFS circulation is driven mainly by winds and surface heating. ...
... 1. The eastern G of M deep-ocean circulation consists of the LC/FC/GS system, which is always present. Materials entrained in the LC can quickly flow through the Florida Straits in proximity to the Florida Keys and the east coast. 2. The WFS circulation is driven mainly by winds and surface heating. ...
hydrosphere notes - drrossymathandscience
... A catchment area is an area which surrounds a waterway and all rainfall drain into the waterway. Ex: river, lake, or reservoir. ...
... A catchment area is an area which surrounds a waterway and all rainfall drain into the waterway. Ex: river, lake, or reservoir. ...
2014 Fellow, the American Geophysical Union
... (AGU). This year, 62 fellows representing less than 0.1 percent of overall membership were named for their scientific eminence, a major breakthrough, a major discovery, paradigm shifts and/or sustained scientific impact. Egbert is a geophysicist and oceanographer whose studies range from ocean tides ...
... (AGU). This year, 62 fellows representing less than 0.1 percent of overall membership were named for their scientific eminence, a major breakthrough, a major discovery, paradigm shifts and/or sustained scientific impact. Egbert is a geophysicist and oceanographer whose studies range from ocean tides ...
Oceans - Geophile.net
... up in the direction the wind is blowing – Water pressure is higher in the “piled up” area – Gravity pulls water down slope – Creates huge, slowly moving gyres ...
... up in the direction the wind is blowing – Water pressure is higher in the “piled up” area – Gravity pulls water down slope – Creates huge, slowly moving gyres ...
Oceans - Learn with Mrs. Schulz
... air expands creating a low pressure area. Cold air, which is high pressure, moves into these areas of low pressure creating wind. 2) Rotation of the Earth – causes the Earth to move beneath the currents (wind and water) causing them to turn. Causes equatorial winds to blow from the east thus pushing ...
... air expands creating a low pressure area. Cold air, which is high pressure, moves into these areas of low pressure creating wind. 2) Rotation of the Earth – causes the Earth to move beneath the currents (wind and water) causing them to turn. Causes equatorial winds to blow from the east thus pushing ...
Physical Oceanography
... o As waves reach the shallow water near a shoreline, energy is lost due to friction against the seafloor. This slows the wave. o Incoming wave crests catch up with slower crests, decreasing the wavelength. o Waves get higher, steeper, and unstable, causing the crests to collapse. o Collapsing wave c ...
... o As waves reach the shallow water near a shoreline, energy is lost due to friction against the seafloor. This slows the wave. o Incoming wave crests catch up with slower crests, decreasing the wavelength. o Waves get higher, steeper, and unstable, causing the crests to collapse. o Collapsing wave c ...
“I Can” Statement Template
... Higher temps, wilder weather, more droughts, changing precip, less snowpack, melting glaciers, shrinking sea ice, thawing permafrost, increased ocean acidity, warmer oceans, rising sea level ...
... Higher temps, wilder weather, more droughts, changing precip, less snowpack, melting glaciers, shrinking sea ice, thawing permafrost, increased ocean acidity, warmer oceans, rising sea level ...
Lecture 4:the observed mean circulation
... •In the south Pacific, isopycnals lean on the topography in the western part of the basin. •Isopycnal tilt would be associated with a northward flowing bottom intensified flow. •Enhanced oxygen concentration in these deep waters suggests that they were recently in contact with the surface and formed ...
... •In the south Pacific, isopycnals lean on the topography in the western part of the basin. •Isopycnal tilt would be associated with a northward flowing bottom intensified flow. •Enhanced oxygen concentration in these deep waters suggests that they were recently in contact with the surface and formed ...
Sea-Floor Spreading
... Resulting Question: Are all of the oceans getting bigger? • Suggested Answer: Ocean floors do not keep spreading. Parts of the oceanic crust get plunged into deep-ocean trenches due to the process of subduction. ...
... Resulting Question: Are all of the oceans getting bigger? • Suggested Answer: Ocean floors do not keep spreading. Parts of the oceanic crust get plunged into deep-ocean trenches due to the process of subduction. ...
ocean currents and weather
... WATER PILES UP IN THE DIRECTION THE WIND IS BLOWING. 3. GRAVITY - WATER WANTS TO FLOW DOWN HILL AGAINST THE PRESSURE GRADIENT. 4. CORIOLIS FORCE - THE CORIOLIS FORCE TURNS THE CURRENTS TO THE RIGHT IN THE NORTHERN HEMISPHERE AND TO THE LEFT IN THE SOUTHERN HEMISPHERE. ALL OF THESE FORCES COMBINE T ...
... WATER PILES UP IN THE DIRECTION THE WIND IS BLOWING. 3. GRAVITY - WATER WANTS TO FLOW DOWN HILL AGAINST THE PRESSURE GRADIENT. 4. CORIOLIS FORCE - THE CORIOLIS FORCE TURNS THE CURRENTS TO THE RIGHT IN THE NORTHERN HEMISPHERE AND TO THE LEFT IN THE SOUTHERN HEMISPHERE. ALL OF THESE FORCES COMBINE T ...
Role of large scale Ocean-Atmosphere interactions in the
... The surface warming due to +4Wm-2 (anthropogenic forcing) is not limited to the mixed layer. Heat exchanges between the mixed layer and deeper layers control the timescale of the surface warming. ...
... The surface warming due to +4Wm-2 (anthropogenic forcing) is not limited to the mixed layer. Heat exchanges between the mixed layer and deeper layers control the timescale of the surface warming. ...
Ocean Topography
... Plotting Data- D=VxT (divided by 2) Ocean Topography (labelling and identifying) -know how to draw both Atlantic and Pacific Ocean floor Continental shelf, slope and rise, trench, submarine canyon, seamount, guyot, mid-ocean ridge, rift valley, abyssal plain. Active Continental Margin vs Passive C ...
... Plotting Data- D=VxT (divided by 2) Ocean Topography (labelling and identifying) -know how to draw both Atlantic and Pacific Ocean floor Continental shelf, slope and rise, trench, submarine canyon, seamount, guyot, mid-ocean ridge, rift valley, abyssal plain. Active Continental Margin vs Passive C ...
MS1R_EXRT_ExamReviewMarine1RegularAnswers_V01
... disturbing force that produces capillary and wind waves is the wind. The disturbing force that generates a tsunami is a tectonic event, such as an earthquake or volcanic activity on the ocean floor. The disturbing force that produces a seiche is a change in atmospheric pressure over an enclosed body ...
... disturbing force that produces capillary and wind waves is the wind. The disturbing force that generates a tsunami is a tectonic event, such as an earthquake or volcanic activity on the ocean floor. The disturbing force that produces a seiche is a change in atmospheric pressure over an enclosed body ...
Lecture - Chapter 5 - Abiotic Components of Ecosystems
... Definition: periodic large scale warming of surface waters of tropical eastern Pacific Ocean ...
... Definition: periodic large scale warming of surface waters of tropical eastern Pacific Ocean ...
Properties of Ocean Water
... Water near the surface is warmer and less dense, so it doesn’t mix easily with deeper water. Deep ocean currents form when cold polar water sinks and moves below the warm water to the equator. ...
... Water near the surface is warmer and less dense, so it doesn’t mix easily with deeper water. Deep ocean currents form when cold polar water sinks and moves below the warm water to the equator. ...
Physical oceanography
Physical oceanography is the study of physical conditions and physical processes within the ocean, especially the motions and physical properties of ocean waters.Physical oceanography is one of several sub-domains into which oceanography is divided. Others include biological, chemical and geological oceanographies.