Katherine Pingree - Shippee will presented a poster on the representation of storm activity on Canadian coasts in commonly
used global reanalysis products.
I'm interested to
use a global reanalysis data to force hydrological models such as SWAT for a meso watershed with sparse hydrometeorological stations.
Not exact matches
Given that quite a few folks (Gore and some enviros particularly) have often
used the USA temp trends in arguments for action (string of record years) it's hard for me to ignore the
reanalysis of those annual temps — even though my own focus remains
global mean temps.
MERRA is a NASA
reanalysis for the satellite era
using a major new version (circa 2008) of the Goddard Earth Observing System Data Assimilation System Version 5 (GEOS - 5) produced by the NASA GSFC
Global Modeling and Assimilation Office (GMAO).
Global average temperatures are also estimated using reanalysis systems, which use a weather forecasting system to combine many sources of data to provide a more complete picture of global tempera
Global average temperatures are also estimated
using reanalysis systems, which
use a weather forecasting system to combine many sources of data to provide a more complete picture of
global tempera
global temperatures.
Errors associated with
using this statistical model to determine the
global average time series is estimated by subsampling the observations (primarily ship tracks) in the earlier period against
reanalysis data for the modern period.
Metzger et al. (NRL Stennis Space Center), 5.0 (3.4 - 6.0), Modeling The
Global Ocean Forecast System (GOFS) 3.1 was run in forecast mode without data assimilation, initialized with July 1, 2015 ice / ocean analyses, for ten simulations
using National Centers for Environmental Prediction (NCEP) Climate Forecast System
Reanalysis (CFSR) atmospheric forcing fields from 2005 - 2014.
NRL - ocn - ice, 5.2 (4.3 - 6.0), Modeling (ice - ocean) The
Global Ocean Forecast System (GOFS) 3.1 was run in forecast mode without data assimilation, initialized with June 1, 2016 ice / ocean analyses, for ten simulations
using National Centers for Environmental Prediction (NCEP) Climate Forecast System
Reanalysis (CFSR) atmospheric forcing fields from 2005 - 2014.
Deliverables shall be
used as input for future climate reanalyses, including the next - generation C3S
global reanalysis ERA6 which is scheduled to go into production by 2021.
Using a state - of - the - art data assimilation system and surface pressure observations, the Twentieth Century
Reanalysis Project is generating a six - hourly, four - dimensional
global atmospheric dataset spanning 1851 to 2014 to place current atmospheric circulation patterns into a historical perspective.
This is all done on a
global reanalysis dataset
using objective methods.
Excuse me for pointing you to a physical oceanography textbook
used by Texas A&M University and in particular to Figure 5.8
Global map of annual - mean insolation into the sea in W / m2 calculated from the ECMWF 40 - year
reanalysis.
ABSTRACT Sampling uncertainties in the voluntary observing ship (VOS)- based
global ocean — atmosphere flux fields were estimated
using the NCEP — NCAR
reanalysis and ECMWF 40 - yr Re-Analysis (ERA - 40) as well as seasonal forecasts without data assimilation.
The difference is that the
reanalysis process involves
using the observations to inform a physical model in order to construct a
global average, whereas the other estimates
use statistical models.
Compute the surface radiative forcing and its amplification by the atmospheric warming in a manner following Myhre and Stordal 1997,
using gridded
global fields of of the input variables obtained from observations (e.g. the ECMWF
reanalysis, ISCCP clouds, satellite ozone, some sort of aerosol optical depth from satellite.
For this study, the area - weighted polar cap geopotential height and air temperature anomalies (PCH and PCT) were computed for the months December through February
using the National Centers for Environmental Prediction (NCEP)
reanalysis at
global 2.5 ° resolution for latitudes north of 65 ° N,
using the period 1950 to 2016 for analysis69.