Lecture 13: Ocean warming Flashcards
sea surface global ocean temperature anomalies
since 1980 considerable warmer seas
the sea has been steadily ____ over the past last century
warming
– the last twenty years include 18 of the hottest global Sea surface temperatures ever recorded
__% of earths waters occurs in ocean
97% and the mean depth is nearly 4km
oceans/air able to absorb more heat
oceans
– reflected in sea surface temperatures but moreso in Ocean Heat Content (OHC)
Ocean heat content:
post 1995 we’ve seen steady increase in temps
oceans have absorbed ___% of excess heat due to global warming
> 90%
– ocean surface takes a lot
if the lower 10km of atmosphere was to absorbs the same quantity of heat the oceans have it would warm by
36 degrees c
consequences of a warming ocean, direct:
- rising sea levels (coastal impacts)
- methane gas hydrate dissociation
- deoxygenation (increase temp, decrease waters ability to take in O2)
- melting of sea ice
consequences of a warming ocean, indirect: ecological consequences
ecological consequences:
– populations responses: move, adapt, or suffer
Consequence of a warming ocean: ecological consequence case study: FISH
- shifting fish on the European Continental Shelf
- ours and marine food webs
- european sea’s warmed particularly rapidly
- bottom-trawl surveys between 1980 and 2008
- some thrive, some abundances decline i.e cod, haddock
- 1DC had little effect, but abundance varied (in 39/50)
- some are moving in response
- commercial fisheries are effected i.e. in haddock and cod
Consequence of a warming ocean: ecological consequence case study: FISH. Why did not all fish move?
- can move polewards or deeper to find water
- so dont see strong signal as they are just going deeper, depths are limited though
- fish movements aren’t determined by temp, maybe require certain environments
- those unable to shift they experience ~3.2dc in 21st century
generalising across taxa response to climate change
met analysis of many marine taxa we see predictable consistent responses across the taxa
- in shift polewards and phenology
generalising across taxa response to climate change: phenology
- phytoplankton respond v quickly
- pelagic animals responding fast
consequences of not moving or adapting example
not moving fast enough?
- i.e. bleaching of corals (can’t move)
- warm the seas, corals bleach
- corals have symbiotic algae, is u stress the corals they expel the algae
- bleaching itself is not lethal, but they need time to recover
- recover time is shortening, return time of bleaching events is now only 6 years (not long enough)
- likely to become annual
our seas play a key role in maintaining Earths
relatively stable climate, but the energy they have absorbed has caused damages and these will continue
- populations must adapt, move, or suffer