1. CLIMATE CHANGE, SEA-LEVEL RISE and CALIFORNIA’S COAST Gary Griggs Director Institute of Marine Sciences University of California Santa Cruz

2. Climate changes have been recorded in: Deep-sea sediment cores Ice cores from Greenland and Antarctica Tree rings- dendrochronology Pollen records in lake sediments Corals from tropical oceans

4. Antarctic ice cores 11,500 feet deep extend back 850,000 years and contain air bubbles, which record atmospheric carbon dioxide content. 402 ppm 2015 – 34% increase

5. GLOBAL CARBON DIOXIDE EMISSIONS EVEN IF WE WERE ABLE TO COMPLETELY ELIMINATE ALL CARBON EMISSIONS TOMORROW, WE WOULD STILL FEEL THE EFFECTS OF PAST EMISSIONS FOR CENTURIES TO COME.

7. Likely Local Climate Change Effects based on climate models and historic trends 1] higher temperatures 2] summer water shortages and longer droughts 3] increase in wild land fires 4] more concentrated winter rainfall and more flooding 5] sea-level rise with increased rates of coastal flooding and cliff erosion These would not be new events, but would likely occur more frequently and be more intense than in the past.

8. As the Earth has cooled and warmed, glaciers and ice sheets have advanced and retreated, and sea level has fallen and risen. 20,000 years ago, ~3% of the ocean’s water, some 10 million cubic miles, was transferred to the continents as ice. Sea level dropped about 400 feet (125 meters) and then rose again. 400 ft 375,000 years of sea-level fluctuations

9. Large parts of North America were covered by ice and glaciers during the last Ice Age 20,000 years ago Sea level was lowered ~400 feet

10. 600 ft. 3000 feet of ice SEATTLE AT END OF LAST ICE AGE 20,000 YEARS AGO WAS UNDER 3,000 FEET OF ICE.

11. Sea Level End of last Ice Age ended Present Rate 3.2mm/yr (12”/100 yrs) Rapid Rise 11mm/yr 45”/100 yrs Very slow rise/ Little change <1mm/yr Very rapid rise >20mm/yr 6.5 ft/100 yrs

12. Components of Global and Regional Sea-Level Rise Sea-level rise at a particular place can be higher or lower than the global mean due to regional effects 66% 33%

13. The rate of global sea-level rise was measured from tide gages historically and satellites since 1993. 1.7 mm/yr 3.2 mm/yr

14. Greenland ~22 feet of SLR Mountain Glaciers ~ 2 feet of SLR Potential future sea- level rise is very large (~225 feet total), but uncertainties in rate of rise. Antarctica ~200 feet of SLR

15. 2 0 3 0 72 60 48 36 24 12 0 Height in Inches

16. 2 0 5 0 72 60 48 36 24 12 0 Height in Inches

17. 2 1 0 0 72 60 48 36 24 12 0 Height in Inches

18. Uncertainty “ There are the known knowns, there are the known unknowns, and there are the unknown unknowns”.

19. SAN FRANCISCO: 1.9 mm/yr. (7.4”/100 years) 1982-83 El Niño 12 in. 1997-98 El Niño 11 in. 1940-41 El Niño 11 in. California Recent Sea-Level Rise Short-term events have had greater impacts than sea-level rise over the past century, and this will likely continue until at least 2050, except perhaps in very low lying areas. 15 cm = 6 in.

20. MONTEREY JANUARY 4-6, 2016

21. Sea level is rising and the bathtub is slowly overflowing, but….

22. The extreme events are going to be of greater concern in the near term, however.

23. San Francisco International Airport and Oracle with a 16 inch rise in sea level. San Francisco International Airport and Oracle with a 16-inch rise in sea level.

24. King Tide-December 2012 The Embarcadero San Francisco

25. November 2015 King Tides

26. IMPACTS OF SHORT (AND LONG) TERM SEA-LEVEL RISE Twin Lakes-Flooded Roadways Aptos Seascape- Damaged oceanfront homes Capitola-Flooded park facilities Pacifica-Cliff retreat

27. Seacliff State Beach- Santa Cruz County

28. Seacliff State Beach- El Niño Winter 1983

29. Along with a continuing rise in sea level, climate change projects potential for more intense coastal storms with larger waves. Over past 22 years, average wave heights along central coast have increased 1.4 ft.

30. Capitola- Depot Hill 1972 2010

31. For Sale: 180 degree ocean view Depot Hill, Capitola

33. ADAPTATION OR RESPONSES TO SEA-LEVEL RISE AND EXTREME EVENTS 1. IGNORE SEA-LEVEL RISE 2. BUILD FLOATING CITIES 3. BUILD BARRIERS: SEAWALLS 4. PLAN FOR MANAGED RETREAT

34. We have may have enough time if we start now. It’s real. It’s us. It’s bad. Scientists agree. There’s some hope.