Precipitation Estimates - A technique is being investigated for
calibrating radar reflectivity using polarization radar measurements
in rain. This technique shows lots of potential for improved rain rate
estimation and it is the only technique that can be implemented for
real-time application. Since the polarization observations are
sensitive to drop size distribution (DSD) and mean raindrop shape,
various calibration equations are derived using model
calculations. The calibration equation based on less oblate raindrop
shape shows almost no bias in radar reflectivity in data from S-POL
deployments in Kansas, Florida and Brazil.
Water Vapor -
IHOP (see Accomplishments Section) focused on improving the ability to
forecast convective rainfall amounts by deploying and evaluating an
unprecedented suite of water vapor sensors. The IHOP PI's
concentrated on designing aircraft tracks for multiple aircraft
missions; coordinating various investigator's activities; organizing
and running planning meetings; serving on the P-3 transition team to
ensure the first-ever P-3 deployment of ELDORA and the French Leandre
II water vapor DIAL; and overseeing logistical planning for field
operations. The yearlong planning effort culminated in a 2-month-long
intensive field campaign. Over 200 researchers coordinated activities
and obtained measurements on convection initiation events, low-level
jets, bores, clear-air boundary layers and heavy rainfall events.
Initial analysis of data and reports from investigators indicate that
this project was a complete success.
To the left is one of the most
complicated flight tracks that was flown during IHOP, involving all
six research aircraft
Water Vapor - Microwave Profiling Radiometer (MWRP) - This is a
study of the diurnal variations of temperature and water vapor
profiles using data from a new microwave profiling radiometer (MWRP)
deployed at the ARM-CART site near Lamont, Oklahoma. MWRP temperature
and humidity data and their diurnal variations were compared with
radiosonde data. Other data were analyzed to understand observed
diurnal variations.
Radiosonde Humidity Data - Coincident soundings were compared
and measured by Vaisala RS80 and VIZ B2 radiosondes during the TRMM
LBA in 1999. The comparison shows significant differences between
Vaisala and VIZ humidity data, which cannot be explained by known
problems associated with these two radiosonde types. Indirect
comparisons of Vaisala and VIZ data from TOGA_COARE and the TRMM
Kwajex experiment also showed these same features. This research led
to development and deployment of a reference radiosonde capable of
carrying both the Vaisala and VIZ humidity sensors. These flights
were made during IHOP-2002.

The left panel shows mean relative humidity (RH) profiles from
Snow White (SW, reference humidity sensor), the carbon hygristor
inside the reference sonde (RS) and Vaisala RS80-H. The comparison
of SW and Vaisala shows that Vaisala RS80-H has very good performance
in the lower and middle troposphere, but has a dry bias in the upper
troposphere. The right panel shos mean RH profiles from SW, the
carbon hgristor inside RS and carbon hygristor inside NWS VIZ
radiosonde. It shows that the carbon hygristor fails to respond to
humidity changes in the upper tropsophere (no sensitivity at all)
and the hygristor inside RS has slower response than that inside NSW
VIZ radiosonde although the two hygristors are exactly the same.
Sydney 2000 Forecast Demonstration Project - Analysis of data
from this experiment is nearing completion. A special issue of Weather
and Forecasting is being prepared which describes the results from
this experiment. This analysis showed the NCAR thunderstorm nowcasting
system called the Auto-nowcaster was the only system capable of
providing statistically better nowcasts than extrapolation.
Boundary Layer Transport - Analysis continues of observations
collected during the DoE VTMX (Vertical Transport and MiXing)
experiment carried out in the Salt Lake Valley in October 2000.
Progress was made in interpreting observations of vertical transport
and mixing from SABL, a sodar, and MAPR. SABL observations are being
analyzed in conjunction with TAOS and sodar measurements to interpret
aerosol distribution and dispersion during mixing events. MM5
mesoscale model runs have been made on selected episodes and have
greatly aided understanding of the dynamics of these events. Results
show the gap flow is a persistent feature that may be representative
of only a small region of the entire Salt Lake Basin, but it plays a
vital role in the vertical mixing in the Jordan Narrows region of the
basin.
Boundary Layer Turbulence and Fluxes - In collaboration with
scientists from NCAR/MMM, Johns Hopkins University, and Pennsylvania
State University ATD researchers used data collected in September 2000
during the HATS (Horizontal Array Turbulence Study) field project to
investigate the statistical properties of turbulence partitioned into
spatially-resolved and sub-filter-scale (SFS) components, as assumed
in Large Eddy Simulation (LES) models. Work over the past year has
focused both on quantifying the accuracy of computational algorithms
used to estimate spatially-filtered statistics and the spatial
gradients of those statistics and on examining the properties of SFS
turbulence.
Surface Energy Budgets - ATD researchers participated in
analysis of Energy Balance Experiment (EBEX-2000) data to determine
why closure of the energy balance utilizing basic physical
measurements, such as sensible and latent heat flux, net radiation,
soil heat flux and storage, is difficult. Typically the error is
larger than expected from an error analysis of the individual terms.
Tropical Convection - Recently published work shows that
tropical convection has a strong sensitivity to middle level relative
humidity. This result, suggested by earlier measurements taken during
TOGA COARE, was confirmed using cloud resolving model simulations. ATD
researchers collaborated with investigators from the Japanese Marine
Science and Technology Center (JAMSTEC) on a study showing the diurnal
variation of tropical deep convection was likely due to diurnal
variations in stability, not to cloud-radiative interactions.
Hurricane/Tornado - ATD researchers refined the objective
vortex circulation center finding algorithm and the VTD/simplex
algorithm. A more sophisticate weighting system that takes into
account the time continuity of radius of maximum wind, position of the
vortex center, and the maximum mean tangential wind can reduce the
uncertainty in the objectively determined vortex centers using the
maximum mean tangential wind as the sole criteria and thereby improve
retrieved vortex circulations. The Mulhall tornado data were
reanalyzed using these new vortex centers. The overall structures of
the tornado improved significantly.
NEXRAD Data Quality Optimization Program - The AP clutter
mitigation scheme was deployed on S-POL for the IMPROVE-II and the
IHOP field experiments. The radar echo classifier algorithms and the
reflectivity-velocity compensation algorithms were run during field
operations. Ongoing research is with the radar echo classifier (REC),
a fuzzy logic algorithm that estimates the type of echo present in
each gate (precipitation, ground clutter or insect clear air
return). This year a set of confidence algorithms for each of the REC
algorithms was developed and tested in the field during IMPROVE-II and
IHOP.