The Argo Program : present and future
The Argo Program : present and future
dc.contributor.author | Jayne, Steven R. | |
dc.contributor.author | Roemmich, Dean | |
dc.contributor.author | Zilberman, Nathalie | |
dc.contributor.author | Riser, Stephen C. | |
dc.contributor.author | Johnson, Kenneth S. | |
dc.contributor.author | Johnson, Gregory C. | |
dc.contributor.author | Piotrowicz, Stephen R. | |
dc.date.accessioned | 2017-10-06T14:13:03Z | |
dc.date.available | 2017-10-06T14:13:03Z | |
dc.date.issued | 2017-06 | |
dc.description | Author Posting. © The Oceanography Society, 2017. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 30, no. 2 (2017): 18–28, doi:10.5670/oceanog.2017.213. | en_US |
dc.description.abstract | The Argo Program has revolutionized large-scale physical oceanography through its contributions to basic research, national and international climate assessment, education, and ocean state estimation and forecasting. This article discusses the present status of Argo and enhancements that are underway. Extensions of the array into seasonally ice-covered regions and marginal seas as well as increased numbers of floats along the equator and around western boundary current extensions have been proposed. In addition, conventional Argo floats, with their 2,000 m sampling limit, currently observe only the upper half of the open ocean volume. Recent advances in profiling float technology and in the accuracy and stability of float-mounted conductivity-temperature-depth sensors make it practical to obtain measurements to 6,000 m. The Deep Argo array will help observe and constrain the global budgets of heat content, freshwater, and steric sea level, as well as the full-depth ocean circulation. Finally, another extension to the Argo Program is the addition of a diverse set of chemical sensors to profiling floats in order to build a Biogeochemical-Argo array to understand the carbon cycle, the biological pump, and ocean acidification. | en_US |
dc.description.sponsorship | S.R.J. was supported by US Argo Program through NOAA Grant NA14OAR4320158 (CINAR). D.R. and N.Z. were supported by the US Argo Program through NOAA Grant NA10OAR4310139 (CIMEC). S.C.R. was supported by the US Argo Program through NOAA Grants NAOAR4320063 and NA16OAR4310161 (JISAO). K.S.J. was supported by the David and Lucile Packard Foundation and by the Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) Project funded by National Science Foundation, Division of Polar Programs (NSF PLR-1425989). G.C.J. is supported by the Ocean Observations and Monitoring Division, Climate Program Office, National Oceanic and Atmospheric Administration (NOAA), US Department of Commerce and NOAA Research. | en_US |
dc.identifier.citation | Oceanography 30, no. 2 (2017): 18–28 | en_US |
dc.identifier.doi | 10.5670/oceanog.2017.213 | |
dc.identifier.uri | https://hdl.handle.net/1912/9271 | |
dc.language.iso | en_US | en_US |
dc.publisher | Oceanography Society | en_US |
dc.relation.uri | https://doi.org/10.5670/oceanog.2017.213 | |
dc.title | The Argo Program : present and future | en_US |
dc.type | Article | en_US |
dspace.entity.type | Publication | |
relation.isAuthorOfPublication | 1cf5a888-fe2f-46c7-b501-514baea90a26 | |
relation.isAuthorOfPublication | 17ccafee-ce8d-40e5-83db-4f824181caf8 | |
relation.isAuthorOfPublication | aedbc1b1-18c2-4588-90ca-4df5598165bc | |
relation.isAuthorOfPublication | 327dcbc3-d848-4489-8a6b-644601d746af | |
relation.isAuthorOfPublication | 14fee751-30ae-4311-adf2-051019f89c19 | |
relation.isAuthorOfPublication | d285781b-5a74-46fe-a809-2a654169b77b | |
relation.isAuthorOfPublication | f774a6bb-3161-4106-af74-cdec9935d7bf | |
relation.isAuthorOfPublication.latestForDiscovery | 1cf5a888-fe2f-46c7-b501-514baea90a26 |