PDF-UK Ocean Acidificatio

Author : jane-oiler | Published Date : 2016-02-28

Research Programme wwwoceanacidicationorg ocb Ocean Carbon Biogeochemistry September 15 2012

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UK Ocean Acidificatio: Transcript


Research Programme wwwoceanacidicationorg ocb Ocean Carbon Biogeochemistry September 15 2012. K South Georgia Island UK National boundary National capital LEGEND 250 500 250 500 mi km An oceanliterate person understands the ssential Principles and Fundamental oncepts about the ocean can communicate about the ocean in a meaningful way and is able to make informed and responsible decisions regarding the ocean and its resources This While written to incorporate computer technology the lesson can be easily adapted to paper and pen Lesson Objective Students will compose a series of slides based on the exhibits at OC The teacher may select one type of exhibit such as those that co Ocean Zones. Which Zone?. 1. Each . group. . will be given a set of words that relate to the different zones of the ocean.. 2. At your table you will . try and place . your words in the correct zone.. Key understanding. Due to the use of unsustainable energy, ocean acidification is a rising problem for marine ecosystems. The high levels of pH (acidity) in the water alters the natural chemical bonding process in regards to the building of shells and exoskeletons of marine wildlife. The rising level of . Alexandria Boehm . Professor of Civil & Environmental Engineering. Senior Fellow Woods Institute of the Environment. Stanford University. Bruce Steele, commercial sea urchin fisherman on ocean acidification:. Chapter 14 . pg. 393. A. The Vast World Ocean. The blue planet. 71% of earth is covered by ocean. Oceanography – study of the ocean. Geography of oceans. 4 main ocean basins. Pacific Ocean. Largest ocean. MEDITERRANEAN SEA. NILE RIVER. CONGO RIVER. ZAMBEZI RIVER. NIGER RIVER. ATLAS MOUNTAINS. SAHARA DESERT. DRAKENSBURG MOUNTAINS. GREAT RIFT VALLEY. ETHIOPIAN HIGHLANDS. KALAHARI DESERT. MT. KILAMANJARO. From 100-200 m (600 ft) to the deepest part. Mesopelagic (to depth of 3300 ft -1000 m). Twilight. THE DEEP - Bathypelagic, Abyssopelagic & Hadopelagic. No sunlight at all. THE MESOPELAGIC. From 100-200 m to depth of 3300 ft (1000 m). 1 WOCE was conceived in late-1970snot so easy to re-capture thinking of the time: Submersibles, satellites, and other technology allow scientists to study the structure and composition of the ocean floor.. a. system that uses transmitted and reflected sound waves to measure distances to the ocean floor; SONAR. A: Sunlight – Producers require sunlight for photosynthesis. Ocean life is determined by many factors:. B: Temperature – most animals live near the surface where it is warmer. Ocean life is determined by many factors:. Section 2: Life in the Oceans. Section 3: Ocean Resources. Salinit. y. - measure of the mount of dissolved salts and other solids in a given liquid. Thermocline. - marks the distinct separation between the warm surface water and the deep, cold water. Sam Coakley. Advisor: Travis Miles, Ph.D.. Tropical cyclone impact on US. https://. www.ncdc.noaa.gov. /billions/summary-stats. Total cost 1980-2019: $954.4B. Total deaths 1980-2019: 6,507. Tropical cyclone impact on US.

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