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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 NASA TC4 (Tropical Composition, Cloud and Climate Coupling) mission investigated the structure and properties of the chemical, dynamic, and physical processes in atmosphere of the tropical Eastern Pacific.

        TC4 was based in San Jose, Costa Rica during July 2007.

        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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      • The NASA African Monsoon Multidisciplinary Analyses (NAMMA) campaign was a field research investigation based in the Cape Verde Islands, 350 miles off the coast of Senegal in west Africa.

        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.
    • TCSP (2005)
      • The Tropical Cloud Systems and Processes (TCSP) mission was an Earth science field research investigation focused on the study of the dynamics and thermodynamics of precipitating cloud systems and tropical cyclones. TCSP was conducted during the period July 1-27, 2005 out of the Juan Santamaria Airfield in San Jose, Costa Rica.

        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.
    • ACES (2002)
      • The Altus Cumulus Electrification Study (ACES) was aimed at better understanding the causes and effects of electrical storms.

        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.
    • CAMEX-4 (2001)
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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.

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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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        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.
    • LPVEx (2010)
      • 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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      • DISCOVER was funded by NASA’s MEaSUREs program to provide highly accurate, multi-decadal geophysical products derived from satellite microwave sensors.
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DOCUMENTATION

Documentation

Guide Documents

Dataset PI Documents

Dataset Software

NAMMA Diode Laser Hygrometer(DLH)

Table of Contents

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

Introduction

The Diode Laser Hygrometer (DLH), an instrument developed for the measurement of water vapor in the troposphere and lower stratosphere by NASA’s Langley and Ames Research Centers, has flown on the NASA DC-8 aircraft during several field campaigns. The DLH is a near-infrared spectrometer operating near 1.4 µ, and  was developed for in situ measurements of atmospheric water vapor (H 2O(v)) from aircraft platforms. It is based upon near-infrared tunable diode technology. This spectrometer provides true in situ monitoring of water vapor concentrations with precision levels exceeding those of existing Lyman α and frost point hygrometers.

Campaign

These data files were generated during support of the NASA African Monsoon Multidisciplinary Analyses (NAMMA) campaign, a field research investigation sponsored by the Science Mission Directorate of the National Aeronautics and Space Administration (NASA). This mission was based in the Cape Verde Islands, 350 miles off the coast of Senegal in west Africa. Commencing 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. For more information about the NAMMA Campaign, go to the NAMMA web site: http://namma.nsstc.nasa.gov/

Instrument Description

The DLH utilizes an open-path, double-pass configuration, where the path is defined on one end by a laser transceiver mounted on the interior of a modified window panel, and on the other by a panel of retroreflecting material mounted on the DC-8's outboard engine nacelle. The DLH operates on one of two spectral absorption lines in the 1.4 µm spectral region, in a wavelength-modulated (WM) mode, with the laser locked to the center of the absorption line encountered in a reference cell. The spectral line used is determined by the local conditions - a weak line is used at low altitudes and a stronger one at high altitudes - and is changed at various times during a flight by the operator. Signal detection is accomplished by demodulating the return signal at twice the driving frequency (2F detection). The returned laser power (DC) is also measured. The DLH is calibrated in the laboratory at various combinations of pressure and water vapor density. From the calibration data and a multiparameter spectral model, a set of coefficients is developed, and these coefficients are used to convert the measured 2F/DC ratio, along with local temperature and pressure (which are measured by separate instruments aboard the aircraft), to water vapor mixing ratio. A laser power normalization scheme enables the sensor to accurately measure water vapor even when flying through clouds. An algorithm calculates H 2O(v) concentration based on the differential absorption signal magnitude, ambient pressure and temperature, and spectroscopic parameters that are measured in the laboratory.

File Naming Convention

Data files are in files of the form:

NAMMA_DLH_yyyymmdd_rx.txt

where,

NAMMA_DLH  - Represents the NAMMA project and the DLH instrument
yyyymmdd  - Is the year, month and date of the flight
rx - Indicates The revision level
txt  - indicates that these are tab delimited text files, using "1001" Gaines-Hipskind format

Data Format

The DLH data files are 1 second ASCII data and follow the "1001" Gaines-Hipskind format as described in the document entitled - "ASCII File Format Specification for Data Exchange" found at: http://espoarchive.nasa.gov/archive/docs/formatspec_2_0.pdf. Additional information about the data can be found in the file header.

An example of the contents of a DLH data file is shown in below:

34 1001 ; Gaines-Hipskind format [http://espoarchive.nasa.gov/archive/docs/formatspec_2_0.pdf]
Diskin, Glenn S.; Podolske, James R.
NASA Langley Research Center; NASA Ames Research Center
Diode Laser Hygrometer (DLH); Water Vapor Mixing Ratio from NASA DC-8
NASA NAMMA MISSION 2006
1 1
2006 08 07 2006 08 29 ; flight-date analysis-date
1
Start_UTC
1
1
-999
H2O(v)_ppmv
1
These data are FINAL
18
PI_CONTACT_INFO: NASA LaRC, MS 483, Hampton, VA 23681; e-mail: glenn.s.diskin@nasa.gov;
PLATFORM: NASA/UND DC-8 Aircraft
LOCATION: DC-8 location data in file NAMMA_ICATS_20060807_1Hz.bin
ASSOCIATED_DATA: NAMMA_ICATS_20060807_1Hz.bin
INSTRUMENT_INFO: Diode Laser Hygrometer - external path in-situ water vapor
DATA_INFO: Water Vapor Volumetric Mixing Ratio in ppmv: p(H2O) / p(ambient) * 10^6
UNCERTAINTY: H2O(v) = 5%
ULOD_FLAG: -7777
ULOD_VALUE: 100000;
LLOD_FLAG: -8888
LLOD_VALUE: 1;
DM_CONTACT_INFO: glenn.s.diskin@nasa.gov
PROJECT_INFO: N/A
STIPULATIONS_ON_USE: PI is interested in knowing intended usage of this dataset
OTHER_COMMENTS: Data in this file are 1 sec; higher bandwidth data available from PI
REVISION: R1
R1: No comments for this revision.
UT_Sec     H2O_ppmv
68520.0     12666.56
68521.0     12546.99
68522.0     12637.19
68523.0     12328.16
68524.0     12272.10
68525.0     12200.19
68526.0     12217.56
68527.0     12263.86
68528.0     12556.91
68529.0     12488.31
68530.0     12405.04

Column headers are described as follows:

UT_Sec: 

Time in UTC seconds.

H2O_ppmv: 

Water Vapor Volumetric Mixing Ratio in ppmv: p(H2O) / p(ambient) * 10^6.

References

G. S. Diskin, J. R. Podolske, G. W. Sachse, and T. A. Slate, "Open-Path Airborne Tunable Diode Laser Hygrometer", Soc. of Photoopt. Instrum. Eng., Bellingham, Wash., (2002).

J. R. Podolske, G. W. Sachse, and G. S. Diskin, "Calibration and data retrieval algorithms for the NASA Langley/Ames Diode Laser Hygrometer for the NASA Transport and Chemical Evolution Over the Pacific (TRACE-P) mission", J. Geophys. Res., 108 (D20), 8792-8798 (2003).

Vay, S. A., B. E. Anderson, G. W. Sachse, J. E. Collins, Jr., J. R. Podolske, C. H. Twohy, B. Gandrud, K. R. Chan, S. L. Baughcum, and H. A. Wallio, DC-8-based observations of aircraft CO, CH4, N2O, and H2O(g) emission indices during SUCCESS, Geophys. Res. Lett., in press, 1998a

Glen W. Sachse; Karen B. Bartlett; James Podolski; Nikita S. Pougatchev; Aircraft Measurements and Analysis of CO, CH4, N2O, CO2, and H2O(v) in Support of TRACE P

Podolske, J. R., G. W. Sachse, and G. S. Diskin (2003), Calibration and data retrieval algorithms for the NASA Langley/Ames Diode Laser Hygrometer for the NASA Transport and Chemical Evolution Over the Pacific (TRACE-P) mission, J. Geophys. Res., 108(D20), 8792, doi:10.1029/2002JD003156.

Contact Information

The data producer is:

Glenn Diskin
NASA LaRC, MS 483,
Hampton, VA 23681
e-mail: glenn.s.diskin@nasa.gov

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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