19
Seawater Chemistry & Ocean Stratification 1

Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Embed Size (px)

Citation preview

Page 1: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Seawater Chemistry & Ocean Stratification

1

Page 2: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Key Points

• The salt in seawater is due in part to water’s unique properties.

• Seawater density is influenced by temperature and salinity.

• The ocean has layers as a result of different densities.

Page 3: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

How did the Ocean get so salty?• Through a combination of water’s properties

(universal solvent, adhesion) water “picks up” minerals via erosional and weathering processes

• In other words, water physically and

chemically picks up salts

• Make way to the ocean

Page 4: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Hydrological Cycle (Water Cycle)

4

Page 5: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

What types of elements are found in the ocean’s salts?

Page 6: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

6

Page 7: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

How do we measure the amount of salt in the Ocean?

• Salinity vs. Conductivity

• CTD Rosette– Conductivity– Temperature– Density

7

Page 8: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Key Points

• The salt in seawater is due in part to water’s unique properties.

• Seawater density is influenced by temperature and salinity.

• The ocean has layers as a result of different densities.

Page 9: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

How is the Ocean Like a Red Velvet

Cake?

Page 10: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Ocean ModelTemperature

De

pth

Surface

Deeper

WarmerColder

10

Page 11: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Ocean Model

11

Page 12: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

“Warm” shallow surface layer

Cold deep layer

Transition Zone

Ocean Model

12How do the layers form?

Page 13: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

SurfaceLayer

DeepWater

TransitionZone

13

Homogeneous Ocean

Page 14: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Ocean Temperature

Deep Water

• 90% of the total volume of ocean is this cold, deep water. •At depths greater than 1000m, temperature is approximately 4ºC (even in the tropics!!).

windows.ucar.edu

Why do layers form?

Thermocline = Temperature Change

Surface Layer

Transition Zone

14

Page 15: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Mass per unit volume

Lighter1.000 g/cm 3

Denser1.022 to 1.030 g/cm3

hawaiianphotos.net

Because of Density

Lighter100 kg/m3

Denser19,300 kg/m3

Slashfood.com

http://www.youtube.com/watch?v=w_8mw-1HYFg

Page 16: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Ocean Density

Surface Layer

Deep Water

• Seawater density is controlled by Temperature and Salinity

•In the ocean, Temperature has a greater effect on density

windows.ucar.edu

Pycnocline = Density ChangePycnocline

Transition Zone

16

Page 17: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

SurfaceLayer

DeepWater

BoundaryTransitionZone

Thermocline & Pycnocline

17

Page 18: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

SurfaceLayer

DeepWater

Boundary

18

Mixed

Warmed and lit by sun

Photosynthesis

Cold, Dark, No Photosynthesis

Less Nutrients

, More Nutrients

Page 19: Seawater Chemistry & Ocean Stratification 1. Key Points The salt in seawater is due in part to water’s unique properties. Seawater density is influenced

Surface Ocean

• Warm• Lit by the sun• Has photosynthesis• Less nutrients

Deep Ocean

• Cold• Dark• No photosynthesis• More Nutrients• LOTS AND LOTS OF

PRESSURE

19

Main Differences…