Changeset 11032
- Timestamp:
- 2019-05-21T22:34:05+02:00 (6 years ago)
- Location:
- NEMO/trunk/doc/latex/TOP
- Files:
-
- 2 edited
Legend:
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NEMO/trunk/doc/latex/TOP/main/TOP_manual.bib
r11023 r11032 161 161 162 162 @ARTICLE{Meunier_al_2014, 163 author = {Meunier, C. L. ,Malzahn, A. M. and Boersma, M.},163 author = {Meunier, C. L. and Malzahn, A. M. and Boersma, M.}, 164 164 title = {A New Approach to Homeostatic Regulation: Towards a Unified View of Physiological and Ecological Concepts}, 165 165 journal = {PLoS ONE}, -
NEMO/trunk/doc/latex/TOP/subfiles/model_description.tex
r11019 r11032 539 539 The radiocarbon age is computed as $(-1/\lambda) \ln{ \left( \Rq \right)}$, with zero age corresponding to $\Rq=1$. 540 540 541 The reservoir age is the age difference between the ocean uppermost layer and the atmosphere. It is usually reported as conventional radiocarbon age; i.e., computed by means of the Libby radiocarbon mean life \cite[8033 yr;][]{Stuiver_ polach_1977}541 The reservoir age is the age difference between the ocean uppermost layer and the atmosphere. It is usually reported as conventional radiocarbon age; i.e., computed by means of the Libby radiocarbon mean life \cite[8033 yr;][]{Stuiver_Polach_1977} 542 542 \begin{align} 543 543 {^{14}\tau_\mathrm{c}}= -8033 \; \ln \left(1 + \frac{\Dcq}{10^3}\right), \label{eq:convage}
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