Physical Climate Science - SLR and Australian Climate Flashcards
At the ocean surface, temperature has on average increased by _ from 1850-1900
0.88 C and 0.60 C of this warming having occured since 1980
The SST is projected to increase from 1995-2014 to 2081-2100 on average by
0.86 C in SSP1-2.6 and 2.89 C in SSP 5-8.5
Associated warming for low-emission scenarios will likely continue until 2030 because
Slow circulation of the deep ocean
What since the 1980s has doubled in frequency and become more intense and longer?
Marine Heatwaves
GMSL rose faster in the ____ with a ____ rise over the period ____ to ____
20th Century
0.20m
1901-2018
Accelerated since the late 60s - 2.3mm - 3.7mm
Where has sea level rose the fastest and where has it rose the slowest?
Basin Scale
Fastest in the Western Pacific
Slowest in the Eastern Pacific
1993-2018
How much will GMSL rise by 2050 for SSP1-1.9 and SSP5-85
How much will GMSL rise by 2100 for SSP1-1.9 and SSP5-85
0.18m and 0.23m
0.38m and 0.77m
For 0.77m, there is a range of 0.63-1.02
List 5 causes of sea level rise
Ice sheet and shelves
Glaciers
Thermal Expansion
Land Water Storage
Hydrological cycle
What is the Vertical Land Motion relative to sea level rise?
Change in elevation of the Earth’s surface at a place relative to sea level over time
AKA vertical land displacement or subsidence/uplift
The two big ice sheets contributing to sea level rise are located where?
Greenland
Antartica
Greenland has had the greatest change in surface mass balance and sea level contribution
Higher amounts of GMSL rise before 2100 can be caused by 3 things
Earlier-than-projected disintegration of marine ice shelves
Faster-than-projected changes in surface mass balance and dishcarge from Greenland
Abrupt onset of Marine Ice sheet and cliff instability around Antarctica
Beyond 2100, GMSL will continue to rise for centuries due to
Continuing deep ocean heat uptake
Mass loss of Greenland and Antarctic Ice Sheets
List 3 impacts of Sea Level Rise
Coastal Erosion
Mangrove and Saltmarsh Dieback
Human displacement
11426 km of coastline threatened and 40% of beaches may be lost in Australia
What datasets are required to observe climatic trends?
Long-term datasets
Homogenous datsets
Curated datasets
CSIRO BOM employ sensors ACOR-SAT and rainfall, cloud amount and pan evaporation to track climate change
Australia’s climate and ocean has warmed since
National records began in 1910
Climate warning on average 0.24 C since (1.47 anomaly)