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Surface pressure observation - A view from Reanalysis -

Surface pressure observation - A view from Reanalysis -. By Masao Kanamitsu Presented by Shyh-Chin Chen CRD/SIO/UCSD. Reanalysis. Long series of historical analysis using fixed assimilation system (and data quality control system), to avoid climate change due to analysis system change.

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Surface pressure observation - A view from Reanalysis -

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  1. Surface pressure observation- A view from Reanalysis - By Masao Kanamitsu Presented by Shyh-Chin Chen CRD/SIO/UCSD

  2. Reanalysis • Long series of historical analysis using fixed assimilation system (and data quality control system), to avoid climate change due to analysis system change. • Fictitious climate signal due to change in observation system is unavoidable • may require fixed observation reanalysis

  3. Reanalysis in progress • ECMWF ERA-45 • US National Reanalysis Program is now under consideration (2005?) • NOAA, NASA, NSF, DOE, DOD, …

  4. Surface pressure observation in reanalysis • Modern objective analysis utilizes a variety of observations simultaneously to analyze desired fields. • Surface pressure can be analyzed from: • Surface pressure • Surface (10m) winds • Satellite (IR and SSM/I) obs • Upper air obs. • Satellite cloud motion vectors • SST • Analysis is consistent to these observations within their observation error

  5. Objective analysis and surface pressure • Dynamical constraints in objective analysis makes surface pressure as “weak” variable, meaning easily driven by other fields (such as winds), and prone to modification by initialization process. • But this is strongly dependent on the analysis system (more true for 3-D var but probably not so for 4-D var) • It may not be easy to obtain surface pressure observation using simple dynamical balance

  6. Dynamical property of surface pressure • Strongly affected by gravity wave • Large diurnal and semi-diurnal oscillation, particularly in tropics • “Weak” variable

  7. Research required • Research on reconstruction of 3-dimensional atmospheric fields from surface pressure. • May be possible with the use of 4-D var • Surface pressure tendency observation may become important. • Research on diurnal and semi-diurnal variation of surface pressure needs to be performed to properly analyze global pressure field. • It is necessary to maintain instantaneous observation for use in data assimilation.

  8. Recommendation • Make the data freely available to Reanalysis communities. • Archive of surface pressure tendency should be considered. • Consider separate archive of instantaneous and monthly average observation. • Observational from new instruments should be properly archived. • Any consultation with Roy Jenne (NCAR)?

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