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Is the Last Glacial Maximum a reverse analog for future hydroclimate changes in the Americas?

Is the Last Glacial Maximum a reverse analog for future hydroclimate changes in the Americas?

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2086029651

Is the Last Glacial Maximum a reverse analog for future hydroclimate changes in the Americas?

About this item

Full title

Is the Last Glacial Maximum a reverse analog for future hydroclimate changes in the Americas?

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

Journal title

Climate dynamics, 2019-04, Vol.52 (7-8), p.4407-4427

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer Berlin Heidelberg

More information

Scope and Contents

Contents

Future hydroclimate change is expected to generally follow a wet-get-wetter, dry-get-drier (WWDD) pattern, yet key uncertainties remain regionally and over land. It has been previously hypothesized that lake levels of the Last Glacial Maximum (LGM) could map a reverse analog to future hydroclimate changes due to reduction of CO
2
levels at th...

Alternative Titles

Full title

Is the Last Glacial Maximum a reverse analog for future hydroclimate changes in the Americas?

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2086029651

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2086029651

Other Identifiers

ISSN

0930-7575

E-ISSN

1432-0894

DOI

10.1007/s00382-018-4385-y

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