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<article language="en">
	<journal>
		<journal_title>Climate of the Past Discussions</journal_title>
		<journal_url>www.clim-past-discuss.net</journal_url>
		<issn>1814-9340</issn>
		<eissn>1814-9359</eissn>
		<volume_number>2</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2006</publication_year>
	</journal>
	<doi>10.5194/cpd-2-563-2006</doi>
	<article_url>http://www.clim-past-discuss.net/2/563/2006/</article_url>
	<abstract_html>http://www.clim-past-discuss.net/2/563/2006/cpd-2-563-2006.html</abstract_html>
	<fulltext_pdf>http://www.clim-past-discuss.net/2/563/2006/cpd-2-563-2006.pdf</fulltext_pdf>
	<start_page>563</start_page>
	<end_page>604</end_page>
	<publication_date>2006-08-23</publication_date>
	<article_title content_type="html">Climate-human-environment interactions: resolving our past</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. A. Dearing</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Geography, University of Liverpool, UK</affiliation>
	</affiliations>
	<abstract content_type="html">The paper reviews how we can learn from the past about
climate-human-interactions at the present time, and in the future. It
focuses on data sources for environmental change at local and
regional/global spatial scales, and shows the scope and limitations of each.
The use of parallel histories in local case-studies is described in a
case-study from China, where independent records help unravel the complexity
of interactions and provide a basis for assessing the resilience and
sustainability of the landscape system. Holocene global records for Natural
Forcings (e.g.&amp;nbsp;climate and tectonics), Human Society and Ecosystems are
reviewed, and the problems of reconstructing global records of processes
that are only recorded at local scales examined. Existing regional/global
records are used to speculate about the veracity of anthropogenic forcing of
global climate. The paper concludes that a full understanding of causes of
earth system change through (at least) the Holocene can come only through
the most rigorous reconstructions of climate, human activities and earth
processes, and importantly their interactions, at all locations and at all scales.
It follows that we need to promote inter-scale learning: regionalisation and generalisation of existing
data would be useful first steps. There is now a need to develop long-term
simulation models that can help anticipate complex ecosystem behaviour and
environmental processes in the face of global environmental change &amp;ndash; and
resolving our past is an essential element in that endeavour.</abstract>
	<references>
	</references>
</article>

