Changes in the atmospheric CH₄ gradient between Greenland and Antarctica during the Holocene

E-ISSN： 2156-2202|102|D13|15987-15997

ISSN： 0148-0227

Source： Journal Of Geophysical Research, Vol.102, Iss.D13, 1997-07, pp. : 15987-15997

Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.

Previous Menu Next

Related content

Modeling atmospheric δ¹³CH₄ and the causes of recent changes in atmospheric CH₄ amounts

Journal Of Geophysical Research, Vol. 101, Iss. D17, 1996-10 ,pp. : 22923-22932

John Wiley & Sons Inc

Access to resources Recommend Favorite

Holocene climatic changes in Greenland: Different deuterium excess signals at Greenland Ice Core Project (GRIP) and NorthGRIP

Journal Of Geophysical Research, Vol. 110, Iss. D14, 2005-07 ,pp. : n/a-n/a

John Wiley & Sons Inc

Access to resources Recommend Favorite

Feedbacks between climate and surface water in northern Africa during the middle Holocene

Journal Of Geophysical Research, Vol. 102, Iss. D10, 1997-05 ,pp. : 11087-11101

John Wiley & Sons Inc

Access to resources Recommend Favorite

CH₄ and δ¹⁸O of O₂ records from Antarctic and Greenland ice: A clue for stratigraphic disturbance in the bottom part of the Greenland Ice Core Project and the Greenland Ice Sheet Project 2 ice cores

Journal Of Geophysical Research, Vol. 102, Iss. C12, 1997-11 ,pp. : 26547-26557

John Wiley & Sons Inc

Access to resources Recommend Favorite

Sensitivity of the CH₄ growth rate to changes in CH₄ emissions from natural gas and coal

Journal Of Geophysical Research, Vol. 101, Iss. D9, 1996-06 ,pp. : 14387-14397

John Wiley & Sons Inc

Access to resources Recommend Favorite