This table is a reference tool for rapidly locating Wikipedia articles on Historic and Prehistoric climate indicators of all types.
More information Method, Type ...
Method |
Type |
Basis |
Interpret |
Instruments |
Back To |
Varve Analysis |
Geological |
Annual bands of seasonally differing particle size in glacial lake deposits |
Samples carry Proxies. Thicker bands = warmer, wetter weather |
Visual and Microscope |
ca 13,000 yrs BP |
Dendroclimatology |
Biological |
Annual bands of seasonally differing woody growth tissue in trees |
Thicker bands = warmer and/or wetter weather, although some studies found thinner trunks for higher temperatures [1] |
Visual and Microscope |
ca 10,000 yrs BP |
Ice cores |
Geological |
Annual (or periodic) layers of differing ice crystals in glaciers and ice caps |
Samples carry Proxies. Thicker bands = snowier weather |
Chemical and Mass Spectrometer |
ca 800,000 yrs BP |
Speleothems |
Geological |
Layers of seasonally differing stalagmite/stalactite deposits in limestone caves |
Samples carry Proxies. Thicker bands = warmer, wetter surface weather |
Visual and Microscope |
ca 500,000 yrs BP |
Sun Spots |
Astronomical |
Number of spots visible on the surface of the Sun over various periods |
More spots = warmer weather cycles (this is controversial) |
Visual and Telescope |
1700 AD |
Oxygen Isotope Analysis, see marine isotope stage |
Geochemical Climate Proxy |
Ratio of Oxygen-18 to Oxygen-16 in calcite from deep sea sediment, and coral cores |
More Oxygen-18 = colder climatic periods |
Mass Spectrometer |
ca 542,000,000 yrs BP |
Beryllium-10 Analysis |
Geochemical Climate Proxy |
Ratio of Beryllium-10 to daughter isotopes in dust from ice cores |
Produced in atmosphere by cosmic rays and absorbed into the hydrologic cycle. Level of Beryllium-10 has been shown to closely match recent solar activity measured by sun spots |
Mass Spectrometer |
ca 80,000 yrs BP |
Close
To Add: