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001 ocn729761517;

003 OCoLC;

005 20141212033344.0;

006 m d f ;

007 cr cn|||||||||;

008 110609s2010 miuab ob f000 0 eng c;

035 a| (Sirsi) o729761517;

040 a| OREc| OREd| GPOd| UtOrBLW;

042 a| pcc;

043 a| n-us---;

049 a| ERE#;

074 a| 0208-C-02 (online);

086 0 a| C 55.13/2:GLERL-152;

100 1 a| Bai, Xuezhi.=| ^A1129674;

245 14 a| The impacts of ENSO and AO/NAO on the interannual variability of Great Lakes ice cover /c| Xuezhi Bai, Jia Wang, Cynthia Sellinger, Anne Clites, and Raymond Assel.;

260 a| [Ann Arbor, Mich.] :b| U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, [Great Lakes Environmental Research Laboratory],c| [2010];

300 a| 1 online resource (44 pages) :b| illustrations, maps (some color).;

336 a| text2| rdacontent;

337 a| computer2| rdamedia;

338 a| online resource2| rdacarrier;

490 1 a| NOAA technical memorandum GLERL ;v| 152;

490 1 a| GLERL contribution ;v| no. 1561;

500 a| "November 2010.";

538 a| System requirements: PDF reader.;

538 a| Mode of access: World Wide Web.;

500 a| Title from Web page (viewed on June 6, 2011).;

520 3 a| The impacts of El Nino and South Oscillation (ENSO) and Arctic Oscillation (AO) or North Atlantic Oscillation (NAO) on Great Lakes ice cover were investigated using ice observations for winters 1963-2008 and National Centers for Environmental Prediction (NCEP) reanalysis data. Signatures of ENSO and AO/NAO were found in Great Lakes ice cover. However, the impacts are nonlinear and asymmetric. Strong El Nino events are often associated with least ice cover on the Great Lakes, while the impacts of weak El Nino and La Nina events (of all intensities) on the Great Lakes are marginally significant. Negative AO/NAO events are often associated with severe ice cover, while positive AO/NAO events often lead to lower ice cover. The strong El Nino and negative AO/NAO events account for about 50% of the least and severe ice cover winters on the Great Lakes, respectively. The interference of the effects of ENSO and AO/NAO over the Great Lakes makes the relationships complicated. This may be an important cause of nonlinear and asymmetric responses of the regional climate and Great Lakes ice to ENSO and AO/NAO. Based on the cross composite analysis, it is found that during the simultaneous occurrence of El Nino (La Nina) and +AO (-AO) events, Great Lakes ice cover tends to be least (severe).;

588 a| Description based on print version record.;

504 a| Includes bibliographical references (p. 41-44).;

650 0 a| Ice on rivers, lakes, etc.z| Great Lakes (North America)=| ^A329212;

650 0 a| Sea icez| Great Lakes (North America)=| ^A262650;

651 0 a| El Niño Currentx| Environmental aspects.=| ^A173041;

650 0 a| Southern oscillationx| Environmental aspects.=| ^A252395;

650 0 a| Arctic oscillationx| Environmental aspects.=| ^A1133613;

650 0 a| North Atlantic oscillationx| Environmental aspects.=| ^A1133220;

650 0 a| Climatic changesx| Environmental aspectsz| Great Lakes (North America)=| ^A349500;

651 0 a| Great Lakes (North America)x| Climate.=| ^A650751;

700 1 a| Wang, Jia,d| 1957-=| ^A1126259;

700 1 a| Sellinger, Cynthia E.=| ^A1129673;

700 1 a| Clites, Anne H.=| ^A428172;

700 1 a| Assel, Raymond A.=| ^A428065;

710 2 a| Great Lakes Environmental Research Laboratory.=| ^A427316;

776 08 i| Print version:a| Bai, Xuezhi.t| impacts of ENSO and AO/NAO on the interannual variability of Great Lakes ice cover.d| [Ann Arbor, Mich.] : U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, [Great Lakes Environmental Research Laboratory, 2010]w| (OCoLC)683255353;

830 0 a| NOAA technical memorandum GLERL ;v| 152.=| ^A570114;

830 0 a| GLERL contribution ;v| no. 1561.=| ^A427314;

856 40 u| https://purl.fdlp.gov/GPO/gpo29731;

949 a| Click on web addressw| ASISh| JOYNER94;

998 a| 3126286;

998 a| u3126286;

596 a| 1;

999 a| CLICK ON WEB ADDRESSw| ASISc| 1i| 3126286-1001l| JNETm| JOYNERr| Ys| Yt| JNE1DOu| 11/12/2012x| EDOCUMENTz| JERESOURCE;

The impacts of ENSO and AO/NAO on the interannual variability of Great Lakes ice cover / Xuezhi Bai, Jia Wang, Cynthia Sellinger, Anne Clites, and Raymond Assel.

Author/creator	Bai, Xuezhi
Format	Electronic
Publication Info	[Ann Arbor, Mich.] : U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, [Great Lakes Environmental Research Laboratory], [2010]
Description	1 online resource (44 pages) : illustrations, maps (some color).
Supplemental Content	https://purl.fdlp.gov/GPO/gpo29731
Subjects	Ice on rivers, lakes, etc.--Great Lakes (North America). Sea ice--Great Lakes (North America). Southern oscillation--Environmental aspects. Arctic oscillation--Environmental aspects. North Atlantic oscillation--Environmental aspects. Climatic changes--Environmental aspects. --Great Lakes (North America). El Niño Current--Environmental aspects. Great Lakes (North America)--Climate.

Other author/creator	Wang, Jia, 1957-
Other author/creator	Sellinger, Cynthia E.
Other author/creator	Clites, Anne H.
Other author/creator	Assel, Raymond A.
Other author/creator	Great Lakes Environmental Research Laboratory.
Series	NOAA technical memorandum GLERL ; 152 GLERL contribution ; no. 1561 NOAA technical memorandum GLERL ; 152. ^A570114 GLERL contribution ; no. 1561. ^A427314
Summary	The impacts of El Nino and South Oscillation (ENSO) and Arctic Oscillation (AO) or North Atlantic Oscillation (NAO) on Great Lakes ice cover were investigated using ice observations for winters 1963-2008 and National Centers for Environmental Prediction (NCEP) reanalysis data. Signatures of ENSO and AO/NAO were found in Great Lakes ice cover. However, the impacts are nonlinear and asymmetric. Strong El Nino events are often associated with least ice cover on the Great Lakes, while the impacts of weak El Nino and La Nina events (of all intensities) on the Great Lakes are marginally significant. Negative AO/NAO events are often associated with severe ice cover, while positive AO/NAO events often lead to lower ice cover. The strong El Nino and negative AO/NAO events account for about 50% of the least and severe ice cover winters on the Great Lakes, respectively. The interference of the effects of ENSO and AO/NAO over the Great Lakes makes the relationships complicated. This may be an important cause of nonlinear and asymmetric responses of the regional climate and Great Lakes ice to ENSO and AO/NAO. Based on the cross composite analysis, it is found that during the simultaneous occurrence of El Nino (La Nina) and +AO (-AO) events, Great Lakes ice cover tends to be least (severe).
General note	"November 2010."
General note	Title from Web page (viewed on June 6, 2011).
Bibliography note	Includes bibliographical references (p. 41-44).
Technical details	System requirements: PDF reader.
Technical details	Mode of access: World Wide Web.
Source of description	Description based on print version record.
Issued in other form	Print version: Bai, Xuezhi. impacts of ENSO and AO/NAO on the interannual variability of Great Lakes ice cover. [Ann Arbor, Mich.] : U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, [Great Lakes Environmental Research Laboratory, 2010]
GPO item number	0208-C-02 (online)
Govt. docs number	C 55.13/2:GLERL-152

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The impacts of ENSO and AO/NAO on the interannual variability of Great Lakes ice cover / Xuezhi Bai, Jia Wang, Cynthia Sellinger, Anne Clites, and Raymond Assel.

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