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Past Climate Variability and Change in the Arctic and at High Latitudes

Past Climate Variability and Change in the Arctic and at High Latitudes

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10<br />

The U.S. <strong>Clim<strong>at</strong>e</strong> Science Program Chapter 1<br />

Italicized loc<strong>at</strong>ions <strong>in</strong> <strong>the</strong><br />

text can be found on a<br />

loc<strong>at</strong>ion map (Pl<strong>at</strong>e 1)<br />

th<strong>at</strong> is provided to help<br />

keep <strong>the</strong> reader sp<strong>at</strong>ially<br />

oriented.<br />

A common timel<strong>in</strong>e<br />

(Pl<strong>at</strong>e 2) is also provided<br />

to assist <strong>the</strong> reader<br />

to stay temporally<br />

oriented amid <strong>the</strong><br />

multiple types of event<br />

nomencl<strong>at</strong>ures utilized<br />

by <strong>the</strong> paleoclim<strong>at</strong>ic <strong>and</strong><br />

geologic communities.<br />

Report <strong>and</strong> Chapter Structure<br />

This report is organized <strong>in</strong>to five primary technical chapters. The first of <strong>the</strong>se (Chapter 2)<br />

provides a conceptual framework for <strong>the</strong> <strong>in</strong>form<strong>at</strong>ion presented <strong>in</strong> <strong>the</strong> succeed<strong>in</strong>g chapters,<br />

each of which focuses on one of <strong>the</strong> topics described above. Chapter 2 also conta<strong>in</strong>s <strong>in</strong>form<strong>at</strong>ion<br />

on <strong>the</strong> st<strong>and</strong>ardized use of time scales <strong>and</strong> geological term<strong>in</strong>ology <strong>in</strong> this report.<br />

Each of <strong>the</strong> topical chapters (Chapters 3 through 6) answers, <strong>in</strong> this order, <strong>the</strong> questions “Why,<br />

how, wh<strong>at</strong>, <strong>and</strong> so wh<strong>at</strong>?” The “Why” or open<strong>in</strong>g <strong>in</strong>troductory segment for each chapter<br />

outl<strong>in</strong>es <strong>the</strong> relevance of <strong>the</strong> topic to <strong>the</strong> issue of modern clim<strong>at</strong>e change. The “How”’ segment<br />

discusses <strong>the</strong> sources <strong>and</strong> types of d<strong>at</strong>a compiled to build <strong>the</strong> paleoclim<strong>at</strong>e record <strong>and</strong><br />

<strong>the</strong> strengths <strong>and</strong> weaknesses of <strong>the</strong> <strong>in</strong>form<strong>at</strong>ion. The “Wh<strong>at</strong>” segment is <strong>the</strong> paleo-record<br />

<strong>in</strong>form<strong>at</strong>ion itself, presented <strong>in</strong> chronological order, oldest to most recent. The f<strong>in</strong>al “So wh<strong>at</strong>”<br />

segment discusses <strong>the</strong> significance of <strong>the</strong> m<strong>at</strong>erial conta<strong>in</strong>ed <strong>in</strong> <strong>the</strong> chapter <strong>and</strong> its relevance<br />

to current clim<strong>at</strong>e change. Each technical chapter is preceded by an abstract th<strong>at</strong> outl<strong>in</strong>es <strong>the</strong><br />

pr<strong>in</strong>cipal conclusions conta<strong>in</strong>ed <strong>in</strong> <strong>the</strong> body of <strong>the</strong> chapter itself. Bolded words <strong>in</strong> <strong>the</strong> text<br />

<strong>in</strong>dic<strong>at</strong>e entries <strong>in</strong> <strong>the</strong> technical glossary <strong>at</strong> <strong>the</strong> end of this report. Italicized loc<strong>at</strong>ions <strong>in</strong> <strong>the</strong><br />

text can be found on a loc<strong>at</strong>ion map (Pl<strong>at</strong>e 1) th<strong>at</strong> is provided to help keep <strong>the</strong> reader sp<strong>at</strong>ially<br />

oriented. This figure <strong>in</strong>cludes loc<strong>at</strong>ions referred to <strong>in</strong> <strong>the</strong> text th<strong>at</strong> are loc<strong>at</strong>ed above 64° north<br />

l<strong>at</strong>itude. A common timel<strong>in</strong>e (Pl<strong>at</strong>e 2) is also provided to assist <strong>the</strong> reader to stay temporally<br />

oriented amid <strong>the</strong> multiple types of event nomencl<strong>at</strong>ures utilized by <strong>the</strong> paleoclim<strong>at</strong>ic <strong>and</strong><br />

geologic communities.<br />

The Syn<strong>the</strong>sis <strong>and</strong> Assessment Product Team<br />

Four of <strong>the</strong> Lead Authors of this report were constituted as a Federal Advisory Committee<br />

(FAC) th<strong>at</strong> was charged with advis<strong>in</strong>g <strong>the</strong> U.S. Geological Survey <strong>and</strong> <strong>the</strong> CCSP on <strong>the</strong><br />

scientific <strong>and</strong> technical content rel<strong>at</strong>ed to <strong>the</strong> topic of <strong>the</strong> paleoclim<strong>at</strong>e history of <strong>the</strong> <strong>Arctic</strong><br />

as described <strong>in</strong> <strong>the</strong> SAP 1.2 prospectus. (See Public Law 92-463 for more <strong>in</strong>form<strong>at</strong>ion on<br />

<strong>the</strong> Federal Advisory Committee Act; see <strong>the</strong> GSA website http://fido.gov/facad<strong>at</strong>abase/<br />

for specific <strong>in</strong>form<strong>at</strong>ion rel<strong>at</strong>ed to <strong>the</strong> SAP 1.2 Federal Advisory Committee.) The FAC for<br />

SAP 1.2 acquired <strong>in</strong>put from more than 30 contribut<strong>in</strong>g authors <strong>in</strong> five countries. These<br />

authors provided substantial content to <strong>the</strong> report, but <strong>the</strong>y did not particip<strong>at</strong>e <strong>in</strong> <strong>the</strong> Federal<br />

Advisory Committee deliber<strong>at</strong>ions upon which this SAP was developed.

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