Storm frequency and magnitude in response to Holocene climate variability, Lake Tutira, North-Eastern New Zealand

Marine Geology

Volumn 270, Issue 1-4, 2010, Pages 30-44

  Page, M J ^a   Trustrum, N A ^a   Orpin, A R ^b   Carter, L ^b,c   Gomez, B ^d   Cochran, U A ^a   Mildenhall, D C ^a   Rogers, K M ^a   Brackley, H L ^a   Palmer, A S ^e   Northcote, L ^b  

^a GNS SCIENCE   (New Zealand)

^b NATIONAL INSTITUTE OF WATER AND ATMOSPHERIC RESEARCH   (New Zealand)

^c VICTORIA UNIVERSITY OF WELLINGTON   (New Zealand)

^d INDIANA STATE UNIVERSITY   (United States)

^e MASSEY UNIVERSITY   (New Zealand)

Author keywords

climate variability; ENSO; erosion; Holocene; lake sediment; New Zealand; storm magnitude frequency

Indexed keywords

CLIMATE VARIABILITY; HOLOCENES; LAKE SEDIMENT; LAKE SEDIMENTS; NEW ZEALAND;

ANALYTICAL GEOCHEMISTRY; ATMOSPHERIC PRESSURE; LAKES; NICKEL COMPOUNDS; SEDIMENTOLOGY; STORMS; TIME MEASUREMENT;

CLIMATE CHANGE;

BIOGEOCHEMISTRY; CARBON ISOTOPE; CLIMATE EFFECT; CLIMATE VARIATION; CORE ANALYSIS; EL NINO-SOUTHERN OSCILLATION; ENVIRONMENTAL CHANGE; HISTORICAL RECORD; HOLOCENE; LACUSTRINE DEPOSIT; PALEOCLIMATE; PLATE BOUNDARY; PROXY CLIMATE RECORD; SEDIMENT TRANSPORT; TEPHRA;

HAWKES BAY; LAKE TUTIRA; NEW ZEALAND; NORTH ISLAND;

EID: 76449107539     PISSN: 00253227     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.margeo.2009.10.019     Document Type: Article

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