From 82a0bdb9b2eeaa9aaa9e4ff9ded45f601f423944 Mon Sep 17 00:00:00 2001 From: tfisher Date: Mon, 25 Nov 2019 11:05:47 -0600 Subject: [PATCH] Issue #14531 flip PD2805 function map params pco2a,pco2w --- RELEASE_NOTES.md | 2 ++ csv/ParameterDefs.csv | 2 +- 2 files changed, 3 insertions(+), 1 deletion(-) diff --git a/RELEASE_NOTES.md b/RELEASE_NOTES.md index 0c108ff..e794078 100644 --- a/RELEASE_NOTES.md +++ b/RELEASE_NOTES.md @@ -4,6 +4,8 @@ - Issue #14524 - Use CTD pressure if needed for bin_depths in adcp_velocity_earth stream. +- Issue #14531 - pco2_co2flux calculation appears to be inverting the flux direction + - Issue #14542 - Add bin_depth parameter to ADCP pd12 streams # Version 1.4.0 (2019-09-11) diff --git a/csv/ParameterDefs.csv b/csv/ParameterDefs.csv index 201a75d..df370ee 100644 --- a/csv/ParameterDefs.csv +++ b/csv/ParameterDefs.csv @@ -2294,7 +2294,7 @@ WAVSS_A_DCL,WAVSS-A,number_directional_bands,PD2801,quantity,,int32,,1,-9999999, WAVSS_A_DCL,WAVSS-A,initial_directional_frequency,PD2802,quantity,,float32,,Hz,-9999999,Initial Directional Frequency,4,,,,,,,initial directional frequency,,, WAVSS_A_DCL,WAVSS-A,directional_frequency_spacing,PD2803,quantity,,float32,,Hz,-9999999,Directional Frequency Spacing,4,,,,,,,directional frequency spacing,,, WAVSS_A_DCL,WAVSS-A,fourier_coefficient_2d_array,PD2804,array,"[""wavss_four_dim0"", ""wavss_four_dim1""]",float32,,1,-9999999,Fourier Coefficient 2D Array,4,,,,,,,2d array of fourier coefficients,,, -PCO2A_A_DCL,PCO2W,pco2_co2flux,PD2805,function,,float32,,mol m-2 s-1,-9999999,CO2 Flux from Ocean to Atmosphere,4,,PFID94,"{""pco2w"":""PD1002"",""pco2a"":""PD1003"",""u10"":""PD3092"",""t"":""PD1056"",""s"":""PD3077""}",,,CO2FLUX_L2,Flux of CO2 from the Ocean into the Atmosphere refers to the exchange of CO2 between the sea surface and the overlying atmosphere. CO2 Flux is estimated from the difference between measurements of the partial pressure of CO2 in the surface ocean and the overlying air. The flux is then estimated as the proportional difference of these partial pressures. The proportionality factor is parameterized using wind speed and adjusted according to sea surface temperature and salinity.,Flux of CO2 from the Ocean into the Amosphere,Science Data,L2 +PCO2A_A_DCL,PCO2W,pco2_co2flux,PD2805,function,,float32,,mol m-2 s-1,-9999999,CO2 Flux from Ocean to Atmosphere,4,,PFID94,"{""pco2a"":""PD1002"",""pco2w"":""PD1003"",""u10"":""PD3092"",""t"":""PD1056"",""s"":""PD3077""}",,,CO2FLUX_L2,Flux of CO2 from the Ocean into the Atmosphere refers to the exchange of CO2 between the sea surface and the overlying atmosphere. CO2 Flux is estimated from the difference between measurements of the partial pressure of CO2 in the surface ocean and the overlying air. The flux is then estimated as the proportional difference of these partial pressures. The proportionality factor is parameterized using wind speed and adjusted according to sea surface temperature and salinity.,Flux of CO2 from the Ocean into the Amosphere,Science Data,L2 CTDMO_GHQR,CTDMO-GHQR,pressure_range,PD2806,quantity,,int32,,psia,-9999999,Pressure Range,0,,,,,,,,,, ADCPT_ACFGM_PD8_DCL,ADCPT-ACFGM,instrument_timestamp,PD2807,quantity,,string,,1,-9999999,Timestamp Provided by the Instrument,0,,,,,,,Format is: yyyy/mm/dd hh:mm:ss.sss,,, ADCPT_ACFGM_PD8_DCL,ADCPT-ACFGM,water_direction,PD2808,array,"[""bin""]",float32,,degrees,-9999999,"Direction (Calculated From VLE, VLN Corrected for EH Heading)",1,,,,,,,1xN array of unsigned direction which is 000.0 to 359.9 degrees as measured toward the instrument and corrected for heading and magnetic deviation (EX11111) or the same with correction for pitch and roll (EX11011). Resolution 0.1 degrees,,,