12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Schmidt Gertraud M. 1, Wall M. 1, Jantzen C. 1, Bürger P. 1, Khokiattiwong.

Slides:



Advertisements
Similar presentations
Global Average Barometric Pressure: January
Advertisements

A case study in the Western Indian Ocean
R Bhagooli & N Taleb-Hossenkhan
Predicting Coral Bleaching from Satellite Sea Surface Temperature Tyler Christensen NOAA Coral Reef Watch Tyler Christensen NOAA Coral Reef Watch.
Somali Current TYLER JANOSKI. First, let’s talk about the South-Asian Monsoon  Monsoon develops because of temperature differences between land and sea.
The Physical Environment of Kaikoura Dr Martin Single Department of Geography University of Canterbury CGTA Kaikoura Workshop2004.
The Role of Zooxanthellae in the thermal tolerance of corals
Erica Weston. The Importance of Coral Reefs Coral reefs are like the rainforests of the sea Biologically diverse Support 33% of marine fish species Provides.
Physiologically relevant bleaching threshold methods provide updated global coral bleaching predictions Cheryl Logan, California State University, Monterey.
Biomes and the Physical Environment Temperature and precipitation determine ranges of species and biomes Atmospheric circulation patterns determine climatic.
Impacts of Global Warming on the Ocean and Coral Reefs Emily Underriner ChE 359 November 24, 2008.
Climate model projections of acidification and thermal bleaching in the world’s coral reef areas Ruben van Hooidonk 1 and Jeffrey Maynard – NOAA.
Carbon Dioxide, Global Warming and Coral Reefs: Prospects for the Future Dr. Craig D. Idso, Chairman Center for the Study of Carbon Dioxide and Global.
Impacts of Climate Change on Coral reefs in the Caribbean Mrs. Marcia Creary.
Aquatic Ecosystems Monday, August 22nd Reminder: HW3 Part II due Wednesday! Midterm Thursday.
Vulnerabilities and Small Islands October 24, 2002 COP 8 New Delhi, India.
UCSB Climate Research Meeting Dept. of Geography ICESS- UCSB October 16, 2009 Earth Space Research Group Climate Variations and Impacts: Monthly Discussion.
PENNSYLVANIA Pennsylvania is home to 12,440,621 people Pennsylvania is approximately 46,055 square feet. That makes Pennsylvania the 33 rd largest state.
What causes Climate ? Text Book page #
Can cyclone induced cooling offer refuge to thermally stressed corals? Adam Carrigan and Dr. Marji Puotinen.
Physical processes in a mesophotic coral refuge across bleaching events Joanna Gyory 1 · Tyler Smith 1 · Laurent Cherubin 2 1 University of the Virgin.
Monthly Composites of Sea Surface Temperature and Ocean Chlorophyll Concentrations These maps were created by Jennifer Bosch by averaging all the data.
Seasonal outlook of the East Asian Summer in 2015 Motoaki Takekawa Tokyo Climate Center Japan Meteorological Agency May th FOCRAII 1.
First Session of South Asian Climate Outlook Forum (SASCOF – 1) Pune, India, April 2010 Impact of Extreme Climate Events on Maldives Abdul Muhsin.
Sea Land Reef Tropical cyclones, (n = 2,261) Tropical storm Tropical cyclone Hurricane Dr. Marji Puotinen and Adam Carrigan Modelling tropical.
OCEANOGRAPHY SOL 5.6.
Introduction The environmental factors such as light, temperature and nutrients interact with each other in the marine environment and play a major role.
science.com.
WOW THIS IS FUN!  THE SUN : CLIMATE IS DIRECTLY LINKED TO THE SUN. SOME AREAS RECEIVE MORE OF THE SUN’S HEAT ENERGY THAN OTHERS.  WINDS : MOVEMENT.
Chapter 3 cont. (Heat & Temperatures). Heat & Temperature Basics temperature: the energy of molecular movement heat: a measure of the amount of energy.
Madden/Julian Oscillation: Recent Evolution, Current Status and Forecasts Update prepared by Climate Prediction Center / NCEP July 17, 2006.
Video: normal and bleached
Basic Geoscience Unit 5 Lecture.
Geography of the Bahamas Miss White’s Third Grade Class.
< BackNext >PreviewMain Exploring the Oceans Chapter 13 Preview CRCT Preparation.
ASSIGNMENT. Luanda, Angola Latitude: 8° 50' 18 S Longitude: 13° 14' 4 E.
Oceanography Sarah Hall. Marine Biology vs. Oceanography Marine Biology is the study of life in the ocean. Oceanography is the study of the physical characteristics.
Climate Change Indicators and Evidence. Temperature Changes Temperature records can be gathered from around the globe and have been consistently monitored.
What Causes Climate? Notes. Introduction A climate is the average, year-after- year weather conditions in an area. Two factors are important in describing.
Animals of the Benthic Environment.. There are well over 300,000 known species in the ocean. 98% of them live in the benthic environment (diversity)
Class #16 Monday, October 5 Class #16: Monday, October 5 Chapter 7 Global Winds 1.
Chapter 26 Modern Earth Science
Chapter 26 Section 2 Climate and Vegetation. Climate and Regions Physical features such as highlands, mountain barriers, and coastal regions shape east.
Coral reef. All the different kinds There are many different kinds of coral reef and they vary from 45 meters deep to 450 meters deep in the ocean.
Projected and observed changes to coral reefs, mangroves and seagrass in Vanuatu.
Climate Change Science Rapid change and “tipping points” Jim Quinn Information Center for the Environment UC Davis.
LONG RANGE FORECAST SW MONSOON
El Niño and La Niña.
El Niño- Southern Oscillation
LONG RANGE FORECAST SW MONSOON
CORAL REEFS © 2016 Paul Billiet ODWS.
Review: Greenhouse Effect
LONG RANGE FORECAST SW MONSOON
Projected changes to coral reefs, mangroves and seagrasses
Natural Climate Variability
Coral Stress and Bleaching
Global Average Barometric Pressure: January
What Causes Climate? Notes.
What Causes Climate? Notes.
Projected changes to coral reefs, mangroves and seagrasses
India’s Summer and Winter Monsoon Seasons
Projected changes to coral reefs, mangroves and seagrasses
Chapter 3 cont. (Heat & Temperatures)
What Causes Climate? Notes.
Projected changes to coral reefs, mangroves and seagrasses
Projected changes to coral reefs and mangroves
The Nuts and Bolts of Climate Change
What Causes Climate? Notes.
GEO 602 INTRODUCTION TO OCEANOGRAPHY PRESENTATION GROUP MEMBERS JOANA VOSAYACO CAROLINE DOUGHTY
Presentation transcript:

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Schmidt Gertraud M. 1, Wall M. 1, Jantzen C. 1, Bürger P. 1, Khokiattiwong S. 2, Richter C. 1 1 Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany 2 Phuket Marine Biological Center, Phuket, Thailand Solitons mitigate coral bleaching in the Andaman Sea – the Porites perspective

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Study site: Similan Islands West East working depth: 15 m

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Shelf facing East Andaman bleaching 2010 Ocean facing West

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Study organsim: Porites lutea

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Thermal anomaly 2010 May10 July10 Dec10 March11 temperature mode 30.1°C Thermal anomaly > 80 days above threshold peak values around 32 °C March08

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Zooxanthellae density and Chlorophyll a East West N = per sampling

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Photosynthetic performance East West N = per sampling measurements after 30min dark adaptation measurements after 1min actinic light stress (600 µmol m -2 s -1 )

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Coral total protein East West N = per sampling

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Thermal anomaly and raw temperature record 2010 May10 July10 Dec10 March11 temperature mode 30.1°C temperature record (3min interval) ∆T cooling < 3 °C ∆T heating > 2 °C ∆T cooling > 6 °C ∆T heating < 2 °C

12th ICRS: Solitons mitigate coral bleaching in the Andaman Sea – the Porites perspective Modified after Jackson 2004 Large amplitude internal waves (LAIW) or solitons peak activity January through April Oceanographic and climatic conditions Similan West 15m

12th ICRS: Solitons mitigate coral bleaching in the Andaman Sea – the Porites perspective Modified after Jackson 2004 Large amplitude internal waves (LAIW) or solitons peak activity Januar y through April SW monsoon regime from May to October Oceanographic and climatic conditions

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Summary and conclusions heating > 30.1 °C cooling < mode temperature West versus East > 50% less heating > 70% higher cooling Solitons cooling effect mitigate coral bleaching facilitate recovery East West Monsoon heavy rain and ocean swell hydrodynamic energy sedimentation retarding recovery sedimentation effect only in West East West rainfall (cm) wind speed ( m s -1 ) 0

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space Relevance Locations of observed oceanic internal waves © Jackson 2004

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space ● shallow tropical coral reefs Center of coral reef biodiversity Relevance

12th ICRS: Climate Change and Bleaching – Refuges for Corals in Time and Space © N. Phongsuwan Thank you for your attention!