Rights statement: Copyright 1997 by the American Geophysical Union
Final published version, 1.79 MB, PDF document
Final published version
Research output: Contribution to Journal/Magazine › Journal article › peer-review
Research output: Contribution to Journal/Magazine › Journal article › peer-review
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TY - JOUR
T1 - Evaluation and intercomparison of global atmospheric transport models using Rn-222 and other short-lived tracers
AU - Jacob, DJ
AU - Prather, MJ
AU - Rasch, PJ
AU - Shia, RL
AU - Balkanski, YJ
AU - Beagley, [No Value]
AU - Bergmann, DJ
AU - Blackshear, WT
AU - Brown, M
AU - Chiba, M
AU - Chipperfield, MP
AU - deGrandpre, J
AU - Dignon, JE
AU - Feichter, J
AU - Genthon, C
AU - Grose, WL
AU - Kasibhatla, PS
AU - Kohler, J.
AU - Kritz, MA
AU - Law, K
AU - Penner, JE
AU - Ramonet, M
AU - Reeves, CE
AU - Rotman, DA
AU - Stockwell, DZ
AU - VanVelthoven, PFJ
AU - Verver, G
AU - Wild, O
AU - Yang, H
AU - Zimmermann, P
N1 - Copyright 1997 by the American Geophysical Union
PY - 1997/3/20
Y1 - 1997/3/20
N2 - Simulations of Rn-222 and other short-lived tracers are used to evaluate and intercompare the representations of convective and synoptic processes in 20 global atmospheric transport models. Results show that most established three-dimensional models simulate vertical mixing in the troposphere to within the constraints offered by the observed mean Rn-222 concentrations and that subgrid parameterization of convection is essential for this purpose. However, none of the models captures the observed variability of Rn-222 concentrations in the upper troposphere, and none reproduces the high Rn-222 concentrations measured at 200 hPa over Hawaii. The established three-dimensional models reproduce the frequency and magnitude of high- Rn-222 episodes observed at Crozet Island in the Indian Ocean, demonstrating that they can resolve the synoptic-scale transport of continental plumes with no significant numerical diffusion. Large differences between models are found in the rates of meridional transport in the upper troposphere (interhemispheric exchange, exchange between tropics and high latitudes). The four two-dimensional models which participated in the intercomparison tend to underestimate the rate of vertical transport from the lower to the upper troposphere but show concentrations of Rn-222 in the lower troposphere that are comparable to the zonal mean values in the three-dimensional models.
AB - Simulations of Rn-222 and other short-lived tracers are used to evaluate and intercompare the representations of convective and synoptic processes in 20 global atmospheric transport models. Results show that most established three-dimensional models simulate vertical mixing in the troposphere to within the constraints offered by the observed mean Rn-222 concentrations and that subgrid parameterization of convection is essential for this purpose. However, none of the models captures the observed variability of Rn-222 concentrations in the upper troposphere, and none reproduces the high Rn-222 concentrations measured at 200 hPa over Hawaii. The established three-dimensional models reproduce the frequency and magnitude of high- Rn-222 episodes observed at Crozet Island in the Indian Ocean, demonstrating that they can resolve the synoptic-scale transport of continental plumes with no significant numerical diffusion. Large differences between models are found in the rates of meridional transport in the upper troposphere (interhemispheric exchange, exchange between tropics and high latitudes). The four two-dimensional models which participated in the intercomparison tend to underestimate the rate of vertical transport from the lower to the upper troposphere but show concentrations of Rn-222 in the lower troposphere that are comparable to the zonal mean values in the three-dimensional models.
KW - ZONALLY AVERAGED CIRCULATION
KW - SEASONAL-VARIATION
KW - NONGEOSTROPHIC THEORY
KW - GENERAL-CIRCULATION MODEL
KW - TROPOSPHERIC OZONE
KW - 3-DIMENSIONAL SIMULATION
KW - ODD NITROGEN
KW - TWO-DIMENSIONAL MODEL
KW - CLIMATE MODEL
KW - MIDDLE ATMOSPHERE
U2 - 10.1029/96JD02955
DO - 10.1029/96JD02955
M3 - Journal article
VL - 102
SP - 5953
EP - 5970
JO - Journal of Geophysical Research: Atmospheres
JF - Journal of Geophysical Research: Atmospheres
SN - 0747-7309
IS - D5
ER -