The lack of widespread instrumental climate records introduces the need for the use of
natural climate archives from «proxy» data such as tree - rings, corals, speleothems and ice cores, as well as documentary evidence to reconstruct climate in past centuries (see Jones et al. 2009 for a review).
In 1989, she went to the Galápagos hoping to use
the natural climate archives stored in corals to develop a long - term record of El Niño, but found that none of the large, old corals others reported had survived the intense warming of the 1982 - 1983 El Niño.
In order to reconstruct climate history, it is necessary to study
natural climate archives since, in terms of Earth's history, humankind has only very recently begun measuring the planet.
Not exact matches
«One of our biggest challenges was to make it possible to compare various measured data and
climate archives from a wide variety of regions and filter out the
natural noise that can greatly distort the signal of
climate archives.»
This approach is a
natural fit for
climate science: a single run of a high - resolution
climate model can produce a petabyte of data, and the
archive of
climate data maintained by the UK Met Office, the national weather service, now holds about 45 petabytes of information — and adds 0.085 petabytes a day.
Summary for Policymakers Chapter 1: Introduction Chapter 2: Observations: Atmosphere and Surface Chapter 3: Observations: Ocean Chapter 4: Observations: Cryosphere Chapter 5: Information from Paleoclimate
Archives Chapter 6: Carbon and Other Biogeochemical Cycles Chapter 7: Clouds and Aerosols Chapter 8: Anthropogenic and
Natural Radiative Forcing Chapter 8 Supplement Chapter 9: Evaluation of
Climate Models Chapter 10: Detection and Attribution of
Climate Change: from Global to Regional Chapter 11: Near - term
Climate Change: Projections and Predictability Chapter 12: Long - term
Climate Change: Projections, Commitments and Irreversibility Chapter 13: Sea Level Change Chapter 14:
Climate Phenomena and their Relevance for Future Regional
Climate Change Chapter 14 Supplement Technical Summary
Another way to study the link is through paleoclimate observations where past
climate is reconstructed through
natural archives.
He uses tree - ring records in combination with other
natural archives and documentary sources to reconstruct the histories of fire, insect outbreaks, human land uses, and
climate.
There is more evidence of abrupt and violent change, most of it culled from ice cores, lake sediments, tree rings and other
natural archives of
climate.
However, both the driving force and the
climate reconstructions over the pre-industrial era are based on the analysis of the
natural archives of
climate sensitive quantities, such as the growth of trees and seashells, and the changes of chemical, biological, and isotopic compositions in lake sediments and ice core samples.
According to his
archived profile at the Austrian Academy of Sciences website, Patzelt's research focus is in «Glacier and
climate history research,» «Mass movements (landslides, fluvial Sedimentationsereignisse),» «Historic
natural and cultural landscape development in alpine areas,» and «Participation in projects of Antarctic Research.»
To gain a longer view, Dr Jones and her colleagues used a compilation of records from
natural archives such as ice cores from the Antarctic ice sheet, which show how the region's
climate has changed over the last 200 years.
Information about
climate changes has been obtained mainly from variations in the concentration of stable isotopes in the
natural archives.
Estimates of surface temperature changes further back in time must therefore make use of the few long available instrumental records or historical documents and
natural archives or «
climate proxy» indicators, such as tree rings, corals, ice cores and lake sediments, and historical documents to reconstruct patterns of past surface temperature change.