On sharp spectrial lines in the climate record and the millenial peak

Paleoceanography

Volumn 15, Issue 4, 2000, Pages 417-424

  Wunsch, C ^a  

^a MASSACHUSETTS INSTITUTE OF TECHNOLOGY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CLIMATE CYCLE; CLIMATE VARIATION; DEEP-SEA SEDIMENT; ICE CORE; PALEOCLIMATE; SEDIMENT CORE;

ALIAS;

EID: 0034450407     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/1999PA000468     Document Type: Article

References (27)

1. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland
2. A pervasive millennial-scale cycle in North Atlantic climate and deep-ocean flow south of Iceland
3. Corrected tables of tidal harmonics
4. A tidal period of 1800 years
5. The harmonic development of the tide-generating potential
6. Frequency sensitivity of the deep sea climatic record
7. Major features and forcing of high-latitude Northern Hemisphere atmospheric circulation using a 110,000-year-long glaciochemical series
8. The δ18O record along the Greenland Ice Core Project deep ice core and the problem of possible Eemian climatic instability
9. A low-order model of the Heinrich event cycle
10. Major features and forcing of high-latitude Northern Hemisphere atmospheric circulation using a 110,000-year-long glaciochemical series
11. Impact of jittered sampling on conventional spectral estimates
12. Glacial cycles and orbital inclination
13. Super-resolution
14. Spectral analysis for physical applications
15. Aliasing of the geologic record and the search for long-period Milankovich cycles
16. A simple model of the North Atlantic thermohaline circulation
17. The seasons, global temperature, and precession
18. Estimation of second-order properties from jittered time series
19. Chaotically modulated stellar dynamos
20. Styles of spectrum analysis
21. Physics of the solar dynamo
22. Bermuda sea level in relation to tides, weather, and baroclinic fluctuations
23. The interpretation of short climate records, with comments on the North Atlantic and Southern Oscillations