'Deep ocean' presentation slideshows

Learning Outcome G4

Learning Outcome G4. Phylum Mollusca , Echinodermata & Arthropoda. Learning Outcome G4. Analyse the increasing complexity of the Phylum Mollusca, the Phylum Echinodermata , and the Phylum Arthropoda. Student Achievement Indicators.

898 views • 75 slides

1/25 What is volume? How do you find the volume of an irregular solid

762 views • 60 slides

What caused Glacial-Interglacial CO 2 Change?

What caused Glacial-Interglacial CO 2 Change?. Douglas L. Love Meto 658A Spring 2006. Suggested papers:. Reviews: Archer et al., 2000 Newer ideas: Zeng 2003 Toggweiler et al. 2005 Paillard and Perenin 2005. Broecker and Henderson 1998. Broecker and Peng 1998.

695 views • 58 slides

Fate and Transport of Microbes in Water, Soils and Sediments

921 views • 47 slides

Carbon Capture and Storage

Carbon Capture and Storage . PRESENTATION TO THE PORTFOLIO COMMITTEE OF ENVIRONMENT, TUESDAY 21 AUGUST 2007. CCS: 210807. Carbon Sequestration.

559 views • 43 slides

CHAPTER 12 Marine Life and the Marine Environment

CHAPTER 12 Marine Life and the Marine Environment. Overview. More than 250,000 identified marine species Most live in sunlit surface seawater Species success depends on ability to Find food Avoid predation Reproduce Cope with physical barriers to movement.

868 views • 41 slides

Climate Change

593 views • 41 slides

Introduction to Primary Production, Respiration and Nutrient Cycling

Introduction to Primary Production, Respiration and Nutrient Cycling. Why we care? Coupling of atmosphere and ocean Ocean carbonate system & importance to chemistry in the of sea water Processes in controlling distribution of oxygen & dioxide in the ocean.

832 views • 33 slides

Renewable Energy

Renewable Energy. Section 1- Renewable Energy Today . Renewable Energy. Energy from sources constantly being formed Use needs to be increased. Solar Power. Sun Passive Solar Heating Uses heat from sun directly Large windows face directly into sun N. hemisphere- south windows.

473 views • 33 slides

459 views • 31 slides

Tracing the ocean overturning circulation

Tracing the ocean overturning circulation. Science Olympiad Resource Anand Gnanadesikan NOAA Geophysical Fluid Dynamics Lab. Welcome!- In this lesson you will learn. How we first learned about deep ocean currents.

385 views • 24 slides

Renewable / Alternative / Sustainable Energy : Analyzing the options

Carbon Sequestration By means of Ocean Iron Fertilization Igal Levine, Alon Henson and Yotam Asscher. Renewable / Alternative / Sustainable Energy : Analyzing the options. June 2010. What is Ocean Iron Fertilization?. Could this be a solution ?. Introduction.

332 views • 19 slides

Plankton

1.13k views • 19 slides

Chapter 2.5

Chapter 2.5 . Aquatic Ecosystems. Aquatic = water Ecosystem = environment. Freshwater Ecosystems include:. Streams and Rivers Ponds and Lakes It provides habitats (homes) for many organisms from algae to bears. . What is the difference between streams/rivers and ponds/lakes?.

357 views • 17 slides

Ocean Water and Ocean Life

453 views • 17 slides

Marine Ecosystems Vocabulary

Marine Ecosystems Vocabulary. 8 th Grade Science 2015- Hydrosphere. Estuaries. Marine Ecosystems.

680 views • 16 slides

Topic #1: Coastal Zones & Carbon Cycle

Topic #1: Coastal Zones & Carbon Cycle. Importance of study of coastal zones in the carbon cycle has been explicated by two major carbon science steering documents: The North American Carbon Plan (NACP) [ Wofsy et al ., 2002]

300 views • 16 slides

Unit 10 period 7

303 views • 16 slides

Tsunami Warning System

Tsunami Warning System. MIDN 1/C Carlin Song ES402 Systems Engineering Design 19 February 2008. Tsunami Phenomenon . large-scale, short-duration vertical displacement of water column. generated by subduction earthquakes principal source regions are earthquake zones in the Pacific Ocean.

529 views • 15 slides

Components of the Climate System

Components of the Climate System. Atmosphere Ocean. Biosphere Geosphere. Image from NASA. Atmosphere & Ocean Circulation. Atmospheric Circulation Depends on density Ocean Surface Circulation Depends on the wind Deep Ocean Circulation Depends on density.

388 views • 15 slides