검색결과 : 5건
| No. | Article |
|---|---|
| 1 |
Preindustrial (CH4)-C-14 indicates greater anthropogenic fossil CH4 emissions Hmiel B, Petrenko VV, Dyonisius MN, Buizert C, Smith AM, Place PF, Harth C, Beaudette R, Hua Q, Yang B, Vimont I, Michel SE, Severinghaus JP, Etheridge D, Bromley T, Schmitt J, Fa?n X, Weiss RF, Dlugokencky E Nature, 578(7795), 409, 2020 |
| 2 |
Old carbon reservoirs were not important in the deglacial methane budget Dyonisius MN, Petrenko VV, Smith AM, Hua Q, Yang B, Schmitt J, Beck J, Seth B, Bock M, Hmiel B, Vimont I, Menking JA, Shackleton SA, Baggenstos D, Bauska TK, Rhodes RH, Sperlich P, Beaudette R, Harth C, Kalk M, Brook EJ, Fischer H, Severinghaus JP, Weiss RF Science, 367(6480), 907, 2020 |
| 3 |
Minimal geological methane emissions during the Younger Dryas-Preboreal abrupt warming event Petrenko VV, Mith AMS, Chaefer HS, Riedel K, Brook E, Baggenstos D, Harth C, Hua Q, Buizert C, Schilt A, Fain X, Mitchell L, Bauska T, Orsi A, Weiss RF, Everinghaus JPS Nature, 548(7668), 443, 2017 |
| 4 |
Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation Schilt A, Brook EJ, Bauska TK, Baggenstos D, Fischer H, Joos F, Petrenko VV, Schaefer H, Schmitt J, Severinghaus JP, Spahni R, Stocker TF Nature, 516(7530), 234, 2014 |
| 5 |
Methane from the East Siberian Arctic Shelf Petrenko VV, Etheridge DM, Weiss RF, Brook EJ, Schaefer H, Severinghaus JP, Smith AM, Lowe D, Hua QA, Riedel K Science, 329(5996), 1146, 2010 |