*2025/01/07 14:21:56.36 *IOS HEADER VERSION 2.0 2016/04/28 2016/06/13 IVF16 *FILE START TIME : UTC 2007/08/24 06:03:00.000 NUMBER OF RECORDS : 24 DATA DESCRIPTION : 'Bottle:Rosette:Up:NoStop and Stop as specified in' CONTINUED : ' SAMPLE METHOD' FILE TYPE : ASCII NUMBER OF CHANNELS : 31 $TABLE: CHANNELS ! No Name Units Minimum Maximum !--- -------------------------------------- --------------- -------------- -------------- 1 Sample_Number n/a 2009 2032 2 Sample_Method n/a 3 Bottle_Number n/a 1 24 4 Pressure decibar 7.3 3055.4 5 Temperature 'deg C (ITS90)' -1.5472 3.3426 6 Salinity PSS-78 18.5543 34.9576 7 Oxygen:Dissolved:SBE mL/L 6.3 9.21 8 Fluorescence:Calibrated:Seapoint mg/m^3 0.31E-01 0.128 9 Transmissivity %/metre 77.57 90.49 10 Nitrate_plus_Nitrite:ISUS volts 0 0 11 PAR uE/m^2/sec 0 0 12 PAR:Reference uE/m^2/sec 169.21 699.91 13 Salinity:Bottle PSS-78 20.6985 34.9553 14 Flag:Salinity:Bottle n/a 15 Oxygen:Dissolved mL/L 6.252 9.118 16 Oxygen:Dissolved umol/kg 279.22 407.23 17 Flag:Oxygen:Dissolved n/a 18 Nitrate_plus_Nitrite umol/L 0 14.5 19 Flag:Nitrate_plus_Nitrite n/a 20 Silicate umol/L 2.5 33.8 21 Flag:Silicate n/a 22 Alkalinity:Total:Potentiometric umol/kg 1767.4 2202.9 23 Flag:Alkalinity:Total:Potentiometric n/a 24 Chlorophyll:Extracted mg/m^3 0.23E-01 0.169 25 Flag:Chlorophyll:Extracted n/a 26 Phaeo-Pigment:Extracted mg/m^3 0.2E-01 0.12 27 Flag:Phaeo-Pigment:Extracted n/a 28 Oxygen:Isotope:18 /mille -6.01 0.19 29 Flag:Oxygen:Isotope:18 n/a 30 Barium:Dissolved nmol/L 45 140 31 Flag:Barium:Dissolved n/a $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places !--- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' ' ' I5 I ' ' 2 ' ' ' ' 8 NQ C ' ' 3 -99 ' ' ' ' I5 I ' ' 4 -99 ' ' ' ' F7.1 R4 ' ' 5 -99 ' ' ' ' F9.4 R4 ' ' 6 -99 ' ' ' ' F9.4 R4 ' ' 7 -99 ' ' ' ' F7.2 R4 ' ' 8 -99 ' ' ' ' F8.3 R4 ' ' 9 -99 ' ' ' ' F7.2 R4 ' ' 10 -99 ' ' ' ' F7.3 R4 ' ' 11 -99 ' ' ' ' F11.3 R4 ' ' 12 -99 ' ' ' ' F11.3 R4 ' ' 13 -99 ' ' ' ' F9.4 R4 ' ' 14 ' ' ' ' 3 NQ C ' ' 15 -99 ' ' ' ' F8.3 R4 ' ' 16 -99 ' ' ' ' F7.2 R4 ' ' 17 ' ' ' ' 3 NQ C ' ' 18 -99 ' ' ' ' F6.1 R4 ' ' 19 ' ' ' ' 3 NQ C ' ' 20 -99 ' ' ' ' F6.1 R4 ' ' 21 ' ' ' ' 3 NQ C ' ' 22 -99 ' ' ' ' F8.2 R4 ' ' 23 ' ' ' ' 3 NQ C ' ' 24 -99 ' ' ' ' F8.3 R4 ' ' 25 ' ' ' ' 3 NQ C ' ' 26 -99 ' ' ' ' F7.2 R4 ' ' 27 ' ' ' ' 3 NQ C ' ' 28 -99 ' ' ' ' F7.2 R4 ' ' 29 ' ' ' ' 3 NQ C ' ' 30 -99 ' ' ' ' F7.1 R4 ' ' 31 ' ' ' ' 3 NQ C ' ' $END $REMARKS Flag channels were initialized with zeros. Non-zero values have the following significance: ------------------------------------------------------------------------------------------ 1 = Sample for this measurement was collected but not analyzed. Sample lost. 2 = Acceptable Measurement 3 = Questionable Measurement (Probably Good) 4 = Poor Measurement (Probably Bad) 5 = Measurement Not Reported (Bad) 6 = Mean of replicate measurements 7 = Manual chromatographic peak measurement 8 = Irregular digital chromatographic peak integration 9 = Sample was planned for this measurement from this bottle but was not collected ------------------------------------------------------------------------------------------ Sampling Methods are expressed with the following codes: -------------------------------------------------------------------------------------- ROS:UN - No Stop ROS:US - Stop for 30 seconds ROS:USM - Up Stop Mix (Stop 30s, up 1m, down 2m, up 1m, wait 30s, close bottle) -------------------------------------------------------------------------------------- $END *ADMINISTRATION MISSION : 2007-20 AGENCY : IOS, Ocean Sciences Division, Sidney, B.C COUNTRY : Canada PROJECT : Joint Ocean Ice Study (JOIS incl JWACS and BGOS) SCIENTIST : McLaughlin F. PLATFORM : Louis S. St. Laurent *LOCATION STATION : STA-A EVENT NUMBER : 99 LATITUDE : 72 41.31000 N ! (deg min) LONGITUDE : 144 41.81000 W ! (deg min) WATER DEPTH : 3468 *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! ------------ ------ ---------- -------- --------- --------- SPRD2IS 5.1 2017/03/25 11:14:31 24 24 CLEAN 5.2.2 2017/03/25 11:15:56 24 24 SORT 3.6 2017/03/25 11:21:45 24 24 HDREDIT2 3.1.1 2017/04/01 12:39:44 ? ? CHANGE_FLAGS 2.0 2017/04/01 12:59:03 24 24 HDREDIT2 3.2 2025/01/07 14:21:56 ? ? $END $REMARKS -CLEAN functions: 2017/03/25 11:15:48 20 Reset #RECS, MIN & MAX values in header. Delete Empty Channels: 25 deleted. -SORT parameters: 2017/03/25 11:21:45 Sorted in ascending order of channel Pressure [decibar] -HEADER EDITS: 2017/04/01 12:39:44 Applied edit header: Z:\SHARE\DATA\Data Archive Process - 2017\Joe's work\2007-20\Headers\2007-20 CHE Header.txt -HEADER EDITS: 2025/01/07 14:21:56 - none. $END *COMMENTS CTD Data Processing Notes: -------------------------- For full details see report Physical and chemical data from the Canada Basin July 26 to August 31, 2007 cited below. Standard seabird processing steps and Matlab based routines were used. CTD Pressure: Lab calibration (29th Oct 2002) adjusted by applying -0.48dbar offset to the bias based on in-air surface readings of the CTD. CTD Temperature: Pre-cruise lab calibration was used after comparisons with dual sensor and post-cruise calibration information. CTD Conductivity: Pre-cruise lab calibration adjusted after comparisons with dual sensor, post-cruise calibrations and water sample data. Primary conductivity adjusted by bias of +0.0018 mS/cm . Secondary conductivity adjusted by bias of +0.0016 mS/cm. CTD Oxygen: Oxygen data are from a SeaBird SBE43 sensor with pumped flow in-line after the primary temperature and conductivity sensors. A lag of -8 seconds was applied to oxygen voltage in the Seabird processing step Align. Downcast CTD oxygen voltage and upcast temperature and salinity were used to calibrate CTD to water sample oxygen (upcast). The 107 casts required 6 calibration groups. Fitting method followed Seabirds Application Note 64-2 (“SBE 43 Dissolved Oxygen Sensor Calibration and Data Corrections using Winkler Titrations”). A remaining pressure dependent shape in the residual between water sample and CTD oxygen was removed by subtracting a mean curve. Parts of the mean curve were found by fitting sections of data from discreet pressure ranges. The parts were then stitched together via spline interpolation to create a full profile mean curve. CTD Fluorometer: Fluorometer data are from a Seapoint sensor with pumped flow in-line after the secondary temperature and conductivity sensors. Calibration with bottle data performed using bottle chlorophyll values between 0.025 and 0.60 mg/m3. The number of observations used were 116 out of 141 with a standard deviation of 0.03 in the residuals. Coefficients used: Slope: 0.7909, Bias: -0.0045. Alignment of -4 seconds was used. Frequent single dropouts in fluorescence to 0 have been fixed by setting to neighbor value. ISUS: Data are uncalibrated. The voltage is proportional to nitrate. Transmissometer data are unprocessed, using calibration from 28 Aug 2006. PAR data are unprocessed, using corrected calibration from 13 Mar 2007. Altimeter data are unprocessed, using calibration from Mar 2005. Data Notes: - Spikes in temperature, conductivity and oxygen have been linearly interpolated over and where needed secondary values (when available) have replaced the primary values. Chemistry Sampling and Analysis Methods: --------------------------------------- For full details see report "Physical and chemical Data from the Canada Basin, July 26 to August 31, 2007." cited below. Salinity samples were collected in 200 mL type II glass bottles with disposable plastic inserts and screw caps. On board, samples were analyzed in a temperature-controlled lab on a Guildline AutoSalinometer Model 8400B (SN: 69086), which was standardized with IAPSO standard seawater. Onshore, 2 casts were analyzed November 2007 on the Guildline AutoSalinometer Model 8400B (SN: 68572), which was standardized with IAPSO standard seawater. Dissolved Oxygen: Oxygen samples were collected in glass flasks and analyzed on board on an automated Micro-Winkler titration system following the procedures of Carpenter (1965). The titration was performed with a Metrohn Dosimat 665 and the end point was detected using a Brinkmann probe Colorimeter PC910 (SN: 910-358). Software written at the Institute of Ocean Sciences, NewAutoOxy.exe, was used to calculate dissolved oxygen (ml/L). Oxygen data received correction post-cruise in May 2008 and February 2009 of 0.0 to 0.3 mL/L after recalibrating the volume of potassium iodide standard, identifing one unexplained drift in the uniform bottom water, and recalibrating flask volumes. Nutrient samples (nitrate plus nitrite, silicate and orthophosphate) were collected in polystyrene test tubes. If analysis could be performed on board within 24 hours the samples were stored at 4 degree C, if not they were frozen at -20 degree C. Note Surfactants for all three nutrients were misplaced during shipping. Palmolive dish detergent was an effective surfactant for nitrate and silicate but not for phosphate. Beginning August 12th with Cast 43, all phosphate samples were frozen in glass for analysis at the Institute of Ocean Sciences(IOS). Frozen samples were analyzed at IOS February and March 2008. Samples were not filtered. Samples were analyzed using a Technicon auto-analyzer following methods described in Barwell-Clarke and Whitney (1996). Ammonium samples were collected in 50 mL glass tubes, and analysed onboard following the Holmes et al. (1999) fluorometric protocol. Samples were kept in the dark for 5 to 8 hours at room temperature. Samples were then measured using a Turner Designs TD-700 fluorometer. Oxygen Isotopes Samples were collected into 30 ml glass vials. Once at room temperature, the caps were retightened and wrapped with parafilm for storage. The bulk of the samples (623) were analyzed January to March 2008 at Oregon State University's COAS Stable Isotope Lab using a Thermo Finnigan Delta Plus XL isotope ratio mass spectrometer with precision between +/- <0.05%.Samples from 9 stations (92) were analyzed at Hokkaido University using a mass spectrometer. Samples were analyzed December 2007. Barium samples were collected in ~20 ml plastic vials. Once at room temperature the caps were retightened for storage. Barium concentrations were determined at Oregon State University, using isotope-dilution and a VG Thermo Excel Inductively coupled quadrupole mass spectrometer as previously described with minor modifications (Falkner et al., 1994). Dissolved Inorganic Carbon (DIC) and Alkalinity: DIC and Alkalinity were collected into 250 or 500 mL glass bottles. Samples were kept at 4 degree C until analysis and preserved with HgCl2. Alkalinity ("Alkalinity:Total") and DIC ("Carbon:Dissolved:Inorganic") were measured from the same sample bottle at select stations. In addition, more frequent samples of Alkalinity were collected at most stations and have been labelled "Alkalinity:Total:Potentiometric" to distinguish this set of separate samples, even though both sets of Alkalinity samples were measured using potentiometric titration. DIC was analyzed at the Institute of Ocean Sciences using a SOMMA (Single-Operator Multi-Metabolic Analyzer) - Coulometer system to determine DIC. Alkalinity samples were analyzed at the Institute of Ocean Sciences using an automated potentiometric titration system to determine the total alkalinity. Total Chlorophyll-a (>0.7um) samples were collected into 2 L brown Nalgene sample bottles, immediately placed in dark bags and stored in a fridge. Samples were filtered onto 25mm GF/F filters using low vacuum filtration. The filters were put in scintillation vials and either extracted immediately or frozen at -20 degree C until analysis. All samples were analyzed on board. For analysis, 10 ml of 90% acetone was added to the scintillation vial which was then put into a -20 degree C freezer for 24 hours. The samples were allowed to adjust to room temperature for an hour before being read with the fluorometer. Chlorophyll-a and phaeo-pigment levels were measured with a Turner Designs 10 AU-005 Field Fluorometer SN:5152FRXX calibrated with a commercially pure chl-a standard (Sigma). The sample was acidified with 2 drops of 1N hydrochloric acid to obtain the phaeo-pigment reading. Chlorophyll estimates and phaeopigment estimates are calculated following the procedure in JGOFS manual (1994) cited below. Phytoplankton and bacterioplankton were collected in 2 ml capacity cryogenic vial and fixed with 0.2 ml of 10% paraformaldehyde by vortex mixing. Samples were maintained for at least 15 min at laboratory temperature to allow fixation, and then stored at -80 degree C until analysis at the Bedford Institute of Oceanography. Cell concentrations of picophytoplankton, nanophytoplankton, and bacterioplankton (i.e. non-autofluorescent picoplankton) in thawed samples were analyzed by flow cytometry (Becton Dickinson FACSort) following protocols in routine use (Li and Dickie, 2001). Iodine 129 samples were collected into 1 L PVC bottles Samples and returned to the Laboratory of the Atlantic Environmental Radioactivity Unit (AERU) at the Bedford Institute of Oceanography (BIO). In the laboratory, a NaI carrier was added to a 200 mL aliquot of the seawater sample, it was slightly acidified, purified using multiple hexane extractions and iodine was precipitated as NaI. The NaI precipitate was shipped to the IsoTrace Laboratory at the University of Toronto where 129I analyses were performed by accelerator mass spectrometry (Smith et al. 1998; 1999; 2005). Cesium 137 samples were collected into four 10 L plastic carboys from approximately 40 L of seawater. The water samples were passed through a potassium ferrocyanide (KCFC) packed resin column in the laboratory (AERU) which quantitatively extracts 137Cs from seawater (Smith et al. 1990; Smith & Ellis 1995). The KCFC resin was deployed in a standard geometry and measured using a hyperpure Ge detector having an efficiency of 25%. Particulate organic carbon (POC) samples were collected into 2 L Nalgene bottles. Onboard ship, 4 L samples were filtered onto 47 mm GF75 filters that had been pre-combusted at 500 degree C for 4 hours. The filtration was performed within 4 hours of sampling unless otherwise noted. Samples were analyzed at the University of British Columbia. The filters were first dried for 24 hours at 50 degree C, then fumed with HCl for 48 hours, dried again at 50 degree C for 24 hours, and then wrapped in aluminum foil and pressed into pellets. The pellets were run through the CN analyzer where the POC was determined. Total suspended solids samples were collected into 2 L Nalgene bottles. Onboard ship, 4 to 6 L were filtered onto 47 mm 0.4 µm polycarbonate nucleopore filters, that had been rinsed acid cleaned, rinsed with DMQ water, dried at 50 °C and pre-weighed to 0.001 mg. The filters were rinsed with 3% Ammonium carbonate solution after filtration was complete. The filters were then placed in a labeled 50 mm plastic petrie dish and frozen at -20 °C. The filtration was performed within 4 hours of sampling unless otherwise noted. Samples were analyzed at the University of British Columbia. Once in the lab, the TSS samples were dried at 50 °C for 24 hours and then weighed. The TSS concentration was equal to the final weight minus the initial weight divided by the volume of water filtered. References: 1. McLaughlin, F., Proshutinsky, A., Carmack, E.C., Shimada, K., Brown, K., Corkum, M., Dempsey, M., Drost, H., Eert, J., Guay, C., Gueguen, C., Hutchings, J., Itoh, M., Jackson, J., Kane, T., Krishfield, R., Li, B., Lovejoy, C., Maclean, H., Nelson, J., Nelson, R., Orlich, A., Smith, J., Steel, M., White, L., Wrohan, I., and Zimmermann, S. 2017. Physical and chemical data from the Canada Basin July 26 to August 31, 2007. Can. Data Rep. Hydrogr. Ocean Sci. 189: xx + xxx p. (in preparation). 2. Owens, W. B., and R. C. Millard Jr., 1985, A new algorithm for CTD oxygen calibration. J. Physical Oceanography., 15, 621-631. 3. Carpenter, J.H., 1965. The Chesapeake Bay Institute technique for the Winkler dissolved oxygen method, Limnol. Oceanogr., 10, 141-3. 4. J. Barwell-Clarke and F. Whitney. 1996. Institute of Ocean Sciences Nutrient Methods and Analysis. Canadian Technical Report of Hydrography and Ocean Sciences, No. 182, 43 pp. 5. Falkner, K.K., MacDonald, R.W., Carmack, E.C., and Weingartner, T. 1994. The potential of barium as a tracer of Arctic water masses, p. 63-76. In: O.M. Johannessen, R.D. Muench and J.E. Overland [eds.]. The Polar Oceans and Their Role in Shaping the Global Environment: The Nansen Centennial Volume, AGU Geophys. Monograph Series, AGU Books, Washington, DC. 6. Li, W.K.W., and Dickie, P.M. 2001. Monitoring phytoplankton, bacterioplankton, and virioplankton in a coastal inlet (Bedford Basin) by flow cytometry. Cytometry 44: 236-246. 7. Smith, J.N., Ellis, K.M. and Kilius, L.R. 1998. 129I and 137Cs tracer measurementsin the Arctic Ocean. Deep-Sea Research I. 45(6):959-984. 8. Smith, J.N., Ellis, K.M. and Boyd, T.M. 1999. Circulation features in the Central Arctic Ocean revealed by nuclear fuel reprocessing tracers from SCICEX 95 and 96, 1999. Journal of Geophysical Research. 104(C12):29,663-29,677. 9. Smith, J.N., Jones, E.P., Moran, S.B., Smethie Jr., W.M. and Kieser, W.E. 2005. 129I/CFC-11 Transit times for Denmark Strait Overflow Water in the Labrador and Irminger Seas. Journal of Geophysical Research. 110, C05006, doi:10.1029/2004JC002516. 10. Holmes, R.M., Aminot, A., Kérouel, R., Hooker, B.A. and Peterson, B.J. (1999). A simple and precise method for measuring ammonium in marine and freshwater ecosystems. Can. J. Fish. Aquat. Sci., 56: 1801-1808. 11. JGOFS. 1994. Protocols for the Joint Global Ocean Flux Study (JGOFS) core measurements, Manual and guides 29, Scientific Committee on Ocean Research, United Nations Educational, Scientific and Cultural Organization, Paris, 170 pp. . *INSTRUMENT $REMARKS A rosette, holding 24 ten-litre Niskin Bottles, with a CTD was used. $END *CALIBRATION $TABLE: CORRECTED CHANNELS !Name Units Fmla Pad Coefficients !--------------------------- ------------ ---- ------ ------------ Conductivity:Primary mS/cm 10 -99 () (0.18E-02 1) Conductivity:Secondary mS/cm 10 -99 () (0.16E-02 1) Fluorescence:URU:Seapoint mg/m^3 10 -99 () (-0.45E-02 0.7909) Transmissivity %/metre 10 -99 () (0.559E-01 0.525E-01) Transmissivity %/metre 10 -99 () (-1.084 19.36) PAR uE/m^2/sec 10 -99 () (0 1.5976) $END !-1-- ---2--- -3-- --4--- ---5---- ---6---- --7--- ---8--- --9--- --10-- ----11---- ----12---- ---13--- 14 ---15-- --16-- 17 --18- 19 --20- 21 ---22-- 23 ---24-- 25 --26-- 27 --28-- 29 --30-- 31 !Samp Sample_ Bott Pressu Temperat Salinity Oxygen Fluores Transm Nitrat PAR PAR: Salinity Fl Oxygen: Oxygen Fl Nitra Fl Silic Fl Alkalin Fl Chlorop Fl Phaeo- Fl Oxygen Fl Barium Fl !le_ Method le_ re ure : cence: issivi e_ Reference :Bottle ag Dissolv : ag te_ ag ate ag ity: ag hyll: ag Pigmen ag : ag : ag !Numb Numb Dissol Calibra ty plus_ ~o ed Dissol ~o plus_ ~t ~i Total: ~e Extract ~a t: ~a Isotop ~p Dissol ~o !er er ved: ted:Sea Nitrit tt ved lv Nitri ri ca Potenti tr ed ct Extrac ct e:18 e: ved lv ! SBE point e:ISUS le ed te te te ometric ic ed ted ed 18 ed !---- ------- ---- ------ -------- -------- ------ ------- ------ ------ ---------- ---------- -------- -- ------- ------ -- ----- -- ----- -- ------- -- ------- -- ------ -- ------ -- ------ -- *END OF HEADER 2032 UN 24 7.3 3.3426 18.5543 8.02 0.128 77.57 0.000 0.000 699.910 20.6985 0 8.435 376.72 0 0.0 0 2.5 0 1767.40 0 0.169 0 0.07 0 -6.01 0 67.0 0 2031 UN 23 22.4 0.2490 27.5022 8.80 0.093 88.62 0.000 0.000 693.990 28.1150 0 9.005 402.14 0 0.0 0 3.3 0 2022.10 0 0.151 0 0.07 0 -3.37 0 140.0 0 2030 UN 22 40.0 -0.6434 29.6359 9.21 0.093 89.52 0.000 0.000 684.380 30.1977 0 9.118 407.23 0 0.1 0 10.2 0 2138.40 0 -99.000 0 -99.00 0 -2.94 0 66.0 0 2029 UN 21 74.6 -0.7744 31.8365 7.67 0.122 90.04 0.000 0.000 669.000 31.9244 0 7.765 346.80 0 7.2 0 15.9 0 2202.90 0 0.112 0 0.12 0 -1.91 0 65.0 0 2028 UN 20 103.1 -1.2477 32.3617 7.08 0.041 90.27 0.000 0.000 659.090 32.3646 0 7.082 316.29 0 11.1 0 23.9 0 -99.00 0 0.023 0 0.02 0 -1.80 0 56.0 0 2027 UN 19 127.7 -1.4459 32.6568 6.75 0.037 90.25 0.000 0.000 648.140 32.6549 0 6.706 299.50 0 13.2 0 29.5 0 -99.00 0 -99.000 0 -99.00 0 -1.62 0 69.0 0 2026 UN 18 156.9 -1.5472 32.9248 6.71 0.038 90.22 0.000 0.000 637.640 32.9281 0 6.662 297.50 0 14.2 0 32.8 0 -99.00 0 -99.000 0 -99.00 0 -1.63 0 70.0 0 2025 UN 17 178.1 -1.5351 33.1739 6.66 0.037 90.16 0.000 0.000 628.030 33.1640 0 6.647 296.87 0 14.5 0 33.8 0 -99.00 0 -99.000 0 -99.00 0 -1.49 0 46.0 0 2024 UN 16 206.0 -1.3247 33.6051 6.38 0.037 90.18 0.000 0.000 618.850 33.5767 0 6.408 286.19 0 14.5 0 30.7 0 -99.00 0 -99.000 0 -99.00 0 -1.24 0 65.0 0 2023 UN 15 232.4 -1.0071 34.0672 6.30 0.037 90.25 0.000 0.000 612.050 34.0520 0 6.252 279.22 0 13.3 0 21.9 0 -99.00 0 -99.000 0 -99.00 0 -0.68 0 54.0 0 2022 UN 14 272.5 -0.2884 34.4451 6.34 0.035 90.29 0.000 0.000 599.180 34.4374 0 6.536 291.91 3 12.4 0 13.9 0 -99.00 0 -99.000 0 -99.00 0 -0.20 0 45.0 0 2021 UN 13 319.0 0.1634 34.6252 6.36 0.035 90.23 0.000 0.000 201.900 34.6229 0 6.287 280.79 0 13.0 0 13.6 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2020 UN 12 356.5 0.3998 34.7099 6.37 0.033 90.24 0.000 0.000 199.970 34.7096 0 6.363 284.17 0 13.1 0 12.2 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2019 UN 11 398.8 0.5479 34.7627 6.49 0.033 90.25 0.000 0.000 198.050 34.7607 0 6.489 289.79 0 12.9 0 10.7 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2018 UN 10 455.4 0.6203 34.8129 6.61 0.033 90.25 0.000 0.000 241.690 34.8121 0 6.616 295.45 0 12.7 0 9.5 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2017 UN 9 508.2 0.5759 34.8327 6.67 0.033 90.26 0.000 0.000 537.500 34.8324 0 6.669 297.82 0 12.6 0 8.8 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2016 UN 8 606.7 0.3646 34.8560 6.80 0.033 90.22 0.000 0.000 188.440 34.8557 0 6.790 303.26 0 12.5 0 8.2 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2015 UN 7 711.0 0.1770 34.8693 6.86 0.033 90.24 0.000 0.000 503.780 34.8748 0 6.880 307.24 0 12.5 0 7.8 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2014 UN 6 812.4 0.0914 34.8748 6.87 0.033 90.25 0.000 0.000 182.970 34.8855 0 6.906 308.44 0 12.6 0 7.7 0 -99.00 0 -99.000 0 -99.00 0 0.19 0 -99.0 0 2013 UN 5 1015.2 -0.0454 34.8852 6.90 0.032 90.38 0.000 0.000 456.010 34.9170 0 6.882 307.37 0 13.1 0 9.2 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2012 UN 4 1524.1 -0.3171 34.9177 6.88 0.031 90.47 0.000 0.000 374.950 34.9433 0 -99.000 -99.00 5 13.9 0 11.5 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2011 UN 3 2033.7 -0.4095 34.9436 6.73 0.031 90.49 0.000 0.000 296.120 34.9533 0 6.648 296.88 0 14.3 0 13.0 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2010 UN 2 2543.6 -0.3802 34.9546 6.63 0.031 90.49 0.000 0.000 228.820 34.9553 0 6.582 293.96 0 14.4 0 14.1 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0 2009 UN 1 3055.4 -0.3280 34.9576 6.57 0.032 90.49 0.000 0.000 169.210 34.8699 0 -99.000 -99.00 0 -99.0 0 -99.0 0 -99.00 0 -99.000 0 -99.00 0 -99.00 0 -99.0 0