Lecture 13: Ocean warming Flashcards

1
Q

sea surface global ocean temperature anomalies

A

since 1980 considerable warmer seas

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2
Q

the sea has been steadily ____ over the past last century

A

warming

– the last twenty years include 18 of the hottest global Sea surface temperatures ever recorded

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3
Q

__% of earths waters occurs in ocean

A

97% and the mean depth is nearly 4km

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4
Q

oceans/air able to absorb more heat

A

oceans

– reflected in sea surface temperatures but moreso in Ocean Heat Content (OHC)

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5
Q

Ocean heat content:

A

post 1995 we’ve seen steady increase in temps

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6
Q

oceans have absorbed ___% of excess heat due to global warming

A

> 90%

– ocean surface takes a lot

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7
Q

if the lower 10km of atmosphere was to absorbs the same quantity of heat the oceans have it would warm by

A

36 degrees c

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8
Q

consequences of a warming ocean, direct:

A
  • rising sea levels (coastal impacts)
  • methane gas hydrate dissociation
  • deoxygenation (increase temp, decrease waters ability to take in O2)
  • melting of sea ice
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9
Q

consequences of a warming ocean, indirect: ecological consequences

A

ecological consequences:

– populations responses: move, adapt, or suffer

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10
Q

Consequence of a warming ocean: ecological consequence case study: FISH

A
  • 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
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11
Q

Consequence of a warming ocean: ecological consequence case study: FISH. Why did not all fish move?

A
  • 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
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12
Q

generalising across taxa response to climate change

A

met analysis of many marine taxa we see predictable consistent responses across the taxa
- in shift polewards and phenology

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13
Q

generalising across taxa response to climate change: phenology

A
  • phytoplankton respond v quickly

- pelagic animals responding fast

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14
Q

consequences of not moving or adapting example

A

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
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15
Q

our seas play a key role in maintaining Earths

A

relatively stable climate, but the energy they have absorbed has caused damages and these will continue
- populations must adapt, move, or suffer

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16
Q

2018 ocean heat content:

A

2018 warmest year for the global oceans