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        A variety of in-situ, satellite observations, airborne data, meteorological analyses, and simulation data were collected with missions over the Atlantic in August and September of three observation years (2012, 2013, 2014). These data are available at GHRC beginning in 2015.
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      • The Genesis and Rapid Intensification Processes (GRIP) experiment was a NASA Earth science field experiment in 2010 that was conducted to better understand how tropical storms form and develop into major hurricanes.

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        The Real Time Mission Monitor provided simultaneous aircraft status for three aircraft during the TC4 experiment. During TC4, the NASA ER-2, WB-57 and DC-8 aircraft flew missions at various times. The science flights were scheduled between 17 July and 8 August 2007.
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        Commenced in August 2006, NASA scientists employed surface observation networks and aircraft to characterize the evolution and structure of African Easterly Waves (AEWs) and Mesoscale Convective Systems over continental western Africa, and their associated impacts on regional water and energy budgets.
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        The TCSP field experiment flew 12 NASA ER-2 science flights, including missions to Hurricanes Dennis and Emily, Tropical Storm Gert and an eastern Pacific mesoscale complex that may possibly have further developed into Tropical Storm Eugene.
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        Based at the Naval Air Station Key West in Florida, researchers in August 2002 chased down thunderstorms using an uninhabited aerial vehicle, or "UAV", allowing them to achieve dual goals of gathering weather data safely and testing new aircraft technology. This marked the first time a UAV was used to conduct lightning research.
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        CAMEX-3 successfully studied Hurricanes Bonnie, Danielle, Earl and Georges, yielding data on hurricane structure, dynamics, and motion. CAMEX-3 collected data for research in tropical cyclone development, tracking, intensification, and landfalling impacts using NASA-funded aircraft and surface remote sensing instrumentation.
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        a) LPVEx, Gulf of Finland in autumn 2010, to study rainfall in high latitude environments

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        c) GCPEx, Ontario, Canada winter of 2011-2012, direct and remove sensing observations, and coordinated model simulations of precipitating snow.

        d) IFloodS, Iowa, spring and early summer 2013, to study the relative roles of rainfall quantities and other factors in flood genesis.

        e) IPHEx, N. Carolina Appalachians/Piedmont region May-June 2014, for hydrologic validation over varied topography.

        f) OLYMPEx, Washington's Olympic Peninsula scheduled November 2015-February 2016, for hydrologic validation in extreme coastal and topographic gradients
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        IPHEx sought to characterize warm season orographic precipitation regimes, and the relationship between precipitation regimes and hydrologic processes in regions of complex terrain.
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        IFloodS' primary goal was to discern the relative roles of rainfall quantities such as rate and accumulation as compared to other factors (e.g. transport of water in the drainage network) in flood genesis.
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      • The GPM Cold-season Precipitation Experiment (GCPEx) occurred in Ontario, Canada during the winter season (Jan 15- Feb 26) of 2011-2012.

        GCPEx addressed shortcomings in GPM snowfall retrieval algorithm by collecting microphysical properties, associated remote sensing observations, and coordinated model simulations of precipitating snow. Collectively the GCPEx data set provides a high quality, physically-consistent and coherent data set suited to the development and testing of GPM snowfall retrieval algorithm physics.
    • MC3E (2011)
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        The overarching goal was to provide the most complete characterization of convective cloud systems, precipitation, and the environment that has ever been obtained, providing constraints for model cumulus parameterizations and space-based rainfall retrieval algorithms over land that had never before been available.
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      • The Light Precipitation Evaluation Experiment (LPVEx) took place in the Gulf of Finland in September and October, 2010 and collected microphysical properties, associated remote sensing observations, and coordinated model simulations of high latitude precipitation systems to drive the evaluation and development of precipitation algorithms for current and future satellite platforms.

        In doing so, LPVEx sought to address the general lack of dedicated ground-validation datasets from the ongoing development of new or improved algorithms for detecting and quantifying high latitude rainfall
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DOCUMENTATION

Documentation

Guide Documents

Dataset PI Documents

Dataset Software

GRIP Cloud Microphysics

Table of Contents

Introduction
Campaign
Instrument Description
File Naming Convention
Data Format
References
Contact Information

Note: The combined CIP+PIP particle size distributions from the GRIP field campaign were updated on 9/12/2012. These updates include improved artifact rejection, improved particle sizing, and a correction for saturation errors on the CIP. The CIP saturation errors occurred primarily in heavy clouds containing at least 0.3 g/m3 of condensed water content. The corrected particle concentrations for the CIP may be up to several times higher than previously reported in the heaviest cloud conditions. Derived parameters have been updated accordingly. The PIP, which measures particles larger than 1mm in diameter, was not affected.

Introduction

The GRIP Cloud Microphysics data set consists of in-situ cloud microphysics data collected from three instruments mounted on the NASA DC-8 aircraft:

  1. The Cloud, Aerosol, and Precipitation Spectrometer (CAPS) is a combination of two probes: the Cloud Imaging Probe-Greyscale (CIP-G), used for two-dimensional images and size distributions nominally between 25 and 1550 µm, and the Cloud and Aerosol Spectrometer (CAS), which uses forward-scatter and back-scatter techniques to measure particle size distributions between 0.35 and 50 µm.
  2. The Precipitation Imaging Probe (PIP) is an optical spectrometer which measures the size and shape of particles from 100µm to 6200µm. 
  3. The Cloud Droplet Probe (CDP) is a cloud particle spectrometer which measures droplets in the range of 2-50 µm.

This data set includes the combined particle size distributions and a small sample of images from each probe. Additional information about the data set may be found in the PI readme grip_microphysics_readme.txt.

Campaign

The Genesis and Rapid Intensification Processes (GRIP) experiment was a NASA Earth science field experiment conducted August 5 to September 30, 2010. The major goal was to better understand how tropical storms form and develop into major hurricanes. NASA used the DC-8 aircraft, the WB-57 aircraft and the Global Hawk Unmanned Airborne System (UAS), configured with a suite of in situ and remote sensing instruments that were used to observe and characterize the lifecycle of hurricanes. This campaign also capitalized on a number of ground networks and space-based assets, in addition to the instruments deployed on aircraft from Ft. Lauderdale, Florida ( DC-8), Houston, Texas (WB-57), and NASA Dryden Flight Research Center, California (Global Hawk). More information about this Campaign can be found on the GRIP web site: http://grip.nsstc.nasa.gov/

Instrument Description

Cloud, Aerosol, and Precipitation Spectrometer (CAPS):  

This multipurpose particle spectrometer has three instruments packaged into a single integrated measurement system that provides aerosol particle and cloud hydrometeor size distributions from 0.35 to 50 µm, particle shape (discrimination between water and ice), particle optical properties (refractive index), precipitation size distributions from 25 µm to 1550 µm, liquid water content from 0.01 to 3 gm-3 and aircraft velocity and atmospheric temperature and pressure. This instrument replaces PMS Inc.'s FSSP-100, FSSP-300, 2D-C, 2D-P and KLWC.
The CAPS has two optical sensors to derive the size of individual particles: the Cloud Imaging Probe-Greyscale (CIP-G) and the Cloud and Aerosol Spectrometer (CAS).

Cloud Imaging Probe-Greyscale (CIP-G):  

This optical spectrometer measures the size and shape of particles passing through its collimated laser beam, from 25µm to 1550 µm, liquid water content from 0.01 to 3 gm-3 and airspeed to 200 ms-1. It uses a fast 64-element photodiode array to generate 2-Dimensional Images of the particles,as well as sizing in 1-Dimensional Histogram form. Included in this instrument package are temperature, pressure and relative humidity sensors. The CIP Greyscale has the functionality of CIP with enhanced particle imaging.

Cloud and Aerosol Spectrometer (CAS):

The CAS collects the light scattered in the forward direction (4-12 °) by particles passing through a focused laser beam and converts the light intensity to a particle diameter between 0.35 and 50 mm using Mie light scattering theory. The CAS also measures backscattered light (168-176 °) in order to derive particle refractive index (Baumgardner et al., 1996) and shape factors (Baumgardner et al., 2004). Three pieces of information are recorded by the CAS about each particle: 1) the forward scattered light intensity, 2) backward scattered light intensity, and 3) the time between each particle. The particle by particle information is used to derive size distributions, particle refractive index and shapes, and concentration fluctuations at scales of a meter or less.

Precipitation Imaging Probe (PIP):

This optical spectrometer measures the size and shape of particles from 100µm to 6200µm. It is the classic airborne 2-Dimensional imaging probe, with the expanded capability of the 64-element diode array and fast Digital Signal Processing electronics. The probe resolution is 100µm with a particle sizing range of 6.2mm. The sample area is 26cm x 6.2mm and the maximum airspeed is 200m/s.

Cloud Droplet Probe (CDP):

This miniature, lightweight, low-power cloud particle spectrometer measures droplets in the range of 2-50 µm in concentrations as high as 2000 particles/cm3. Particle-size and concentration is provided in histogram form with 20, 30 or 40-bin resolution. The concentration range is 0-5000 particles/cm-3, sample area is .24 mm-2, airspeed range is 10-200m/s and maximum altitude is 50,000 feet.

These probes are manufactured by Droplet Measurement Technologies, and additional information can be found here: http://www.dropletmeasurement.com/

File Naming Convention

The data and browse files are of the form:

data:

GRIP_MP_yyyymmdd_CAS.txt
GRIP_MP_yyyymmdd_CDP.txt
GRIP_MP_yyyymmdd_CIPPIP.txt

browse:

GRIP_MP_yyyymmdd_CIPPIP_images.tar

where:

yyyymmdd = year, month and day
MP = microphysics
CAS = Cloud and Aerosol Spectrometer
CDP = Cloud Droplet Probe
CIPPIP = Cloud Imaging Probe / Precipitation Imaging Probe
tar = Tape ARchive

Data Format

These data files are in ASCII, tab delimited, format. An example of the data format from the CAS and the CDP probes are shown below. The concentrations are binned, and not all are shown in these examples.

CAS:

Time       Nt(#/m3)       LWC(g/m3)       Concentration(m^-4)
--------------------------------------------------------------------------------
50595     1.07e+08     1.62e-04            3.57e+14     1.69e+14     1.37e+14     1.39e+14     1.51e+14 .........

CDP:

Time       Nt(#/m3)       LWC(g/m3)          Concentration(m^-4)
--------------------------------------------------------------------------------
50595     5.56e+05     7.85e-06            5.56e+11     0.00e+00     0.00e+00     0.00e+00     0.00e+00 .........

Column headers are described as follows:

TIME - Elapsed UTC seconds from 0 hours on day of flight
Nt(#/m3) - Total concentration
LWC(g/m3) - Liquid water content
Concentration(m^-4) - Particle number concentration normalized by bin width

Additional information on file content and structure can be found in each file header.

References

Baumgardner D., H. Jonsson, W. Dawson, D. O'Connor, and R. Newton, 2001:
The cloud, aerosol and precipitation spectrometer: A new instrument for
cloud investigations. Atmos. Res., 59-60, 251–264.

Contact Information

The data provider is:

Andrew Heymsfield
NCAR
P.O. Box 3000
Boulder, CO 80307-3000
heyms1@ucar.ncar.edu

To order these data or for further information, please contact:

Global Hydrology Resource Center
User Services
320 Sparkman Drive
Huntsville, AL 35805
Phone: 256-961-7932
E-mail: support-ghrc@earthdata.nasa.gov
Web: http://ghrc.nsstc.nasa.gov/

 

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