Factors limiting the reduction of atmospheric CO, by iron fertilization. Limnol. Oceanogr. 36: 19 19-l 927
A limit on the reduction in atmospheric CO, partial pressure (PC03 in the next century resulting from purposeful Fe fertilization of the Antarctic Ocean is estimated with an advection-diffusion model calibrated with transient tracer distributions. To evaluate the possible increase in atmo-spheric CO...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.523.90 2023-05-15T13:59:34+02:00 Factors limiting the reduction of atmospheric CO, by iron fertilization. Limnol. Oceanogr. 36: 19 19-l 927 Tsung-hung Peng Wallace S. Broecker The Pennsylvania State University CiteSeerX Archives 1991 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.523.90 http://www.aslo.org/lo/toc/vol_36/issue_8/1919.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.523.90 http://www.aslo.org/lo/toc/vol_36/issue_8/1919.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aslo.org/lo/toc/vol_36/issue_8/1919.pdf text 1991 ftciteseerx 2016-01-08T10:16:12Z A limit on the reduction in atmospheric CO, partial pressure (PC03 in the next century resulting from purposeful Fe fertilization of the Antarctic Ocean is estimated with an advection-diffusion model calibrated with transient tracer distributions. To evaluate the possible increase in atmo-spheric CO, with and without fertilization, we adopt a “business-as-usual ” scenario of anthro-pogenic CO, emission. Such increase is computed from the atmospheric pC0, in the ocean-atmosphere total C system as it responds to this emission scenario. Assuming completely successful Fe fertilization, we calculate an 8 % atmospheric CO2 reduction for a case with a 3 cm2 s-I vertical diffusivity and 17.4 Sv upwelling flux, as derived from distribution of bomb-14C in the ocean. Hence, if atmosphericpC0, reaches 800 patm in the next century, the maximum possible reduction is- 64 patm. Doubling of upwelling flux to 34.8 Sv results in a reduction of 96 palm. If we assume the surface area of the Antarctic Ocean is 16 % of the total ocean area instead of 10 % as used in the standard case, the reduction is- 7 1 patm. These results are independent of the respiration function adopted. As we hold the surface water PO, content at a near-zero value, it makes no difference at what depth the organic material is oxidized (or whether it falls to the bottom and Text Antarc* Antarctic Antarctic Ocean Unknown Antarctic Antarctic Ocean The Antarctic |
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ftciteseerx |
language |
English |
description |
A limit on the reduction in atmospheric CO, partial pressure (PC03 in the next century resulting from purposeful Fe fertilization of the Antarctic Ocean is estimated with an advection-diffusion model calibrated with transient tracer distributions. To evaluate the possible increase in atmo-spheric CO, with and without fertilization, we adopt a “business-as-usual ” scenario of anthro-pogenic CO, emission. Such increase is computed from the atmospheric pC0, in the ocean-atmosphere total C system as it responds to this emission scenario. Assuming completely successful Fe fertilization, we calculate an 8 % atmospheric CO2 reduction for a case with a 3 cm2 s-I vertical diffusivity and 17.4 Sv upwelling flux, as derived from distribution of bomb-14C in the ocean. Hence, if atmosphericpC0, reaches 800 patm in the next century, the maximum possible reduction is- 64 patm. Doubling of upwelling flux to 34.8 Sv results in a reduction of 96 palm. If we assume the surface area of the Antarctic Ocean is 16 % of the total ocean area instead of 10 % as used in the standard case, the reduction is- 7 1 patm. These results are independent of the respiration function adopted. As we hold the surface water PO, content at a near-zero value, it makes no difference at what depth the organic material is oxidized (or whether it falls to the bottom and |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Tsung-hung Peng Wallace S. Broecker |
spellingShingle |
Tsung-hung Peng Wallace S. Broecker Factors limiting the reduction of atmospheric CO, by iron fertilization. Limnol. Oceanogr. 36: 19 19-l 927 |
author_facet |
Tsung-hung Peng Wallace S. Broecker |
author_sort |
Tsung-hung Peng |
title |
Factors limiting the reduction of atmospheric CO, by iron fertilization. Limnol. Oceanogr. 36: 19 19-l 927 |
title_short |
Factors limiting the reduction of atmospheric CO, by iron fertilization. Limnol. Oceanogr. 36: 19 19-l 927 |
title_full |
Factors limiting the reduction of atmospheric CO, by iron fertilization. Limnol. Oceanogr. 36: 19 19-l 927 |
title_fullStr |
Factors limiting the reduction of atmospheric CO, by iron fertilization. Limnol. Oceanogr. 36: 19 19-l 927 |
title_full_unstemmed |
Factors limiting the reduction of atmospheric CO, by iron fertilization. Limnol. Oceanogr. 36: 19 19-l 927 |
title_sort |
factors limiting the reduction of atmospheric co, by iron fertilization. limnol. oceanogr. 36: 19 19-l 927 |
publishDate |
1991 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.523.90 http://www.aslo.org/lo/toc/vol_36/issue_8/1919.pdf |
geographic |
Antarctic Antarctic Ocean The Antarctic |
geographic_facet |
Antarctic Antarctic Ocean The Antarctic |
genre |
Antarc* Antarctic Antarctic Ocean |
genre_facet |
Antarc* Antarctic Antarctic Ocean |
op_source |
http://www.aslo.org/lo/toc/vol_36/issue_8/1919.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.523.90 http://www.aslo.org/lo/toc/vol_36/issue_8/1919.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766268181390819328 |