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Grid DAP Data | Sub- set | Table DAP Data | Make A Graph | W M S | Source Data Files | Acces- sible | Title | Sum- mary | FGDC, ISO, Metadata | Back- ground Info | RSS | E | Institution | Dataset ID |
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set | data | graph | files | public | [Particle Flux] - Sediment trap flux measurements from the Hawaii Ocean Time-Series (HOT) project at station ALOHA ([Current] Hawaii Ocean Time-series (HOT): 2018-2023; [Previous] Hawaii Ocean Time-series (HOT): Sustaining ocean ecosystem and climate observations in the North Pacific Subtropical Gyre) | F I M | background | BCO-DMO | bcodmo_dataset_737393 |
Row Type | Variable Name | Attribute Name | Data Type | Value |
---|---|---|---|---|
attribute | NC_GLOBAL | access_formats | String | .htmlTable,.csv,.json,.mat,.nc,.tsv,.esriCsv,.geoJson |
attribute | NC_GLOBAL | acquisition_description | String | Particle flux was measured at a standard reference depth of 150 m using multiple cylindrical particle interceptor traps deployed on a free-floating array for approximately 60 h during each cruise. Sediment trap design and collection methods are described in Winn et al. (1991). Samples were analyzed for particulate C, N, P & Si. Typically six traps are analyzed for PC and PN, three for PP, and another three traps for PSi. The information below has been copied from the HOT Field & Laboratory Protocols page, found at [http://hahana.soest.hawaii.edu/hot/protocols/protocols.html#](\\"http://hahana.soest.hawaii.edu/hot/protocols/protocols.html#\\") (last visited on 2018-05-23). SUMMARY: Passively sinking particulate matter is collected using a free- floating sediment array and, after prescreening (335 \u00b5m) to remove zooplankton and micronekton carcasses, the sample materials are analyzed for C, N, P and mass flux (mg m-2 d-1). 1\. Principle Although most of the particulate matter both on the seafloor and in suspension in seawater is very fine, recent evidence suggests that most of the material deposited on the benthos arrives via relatively rare, rapidly sinking large particles (McCave, 1975). Therefore, in order to describe adequately the ambient particle field and to understand the rates and mechanisms of biogeochemical cycling in the marine environment, it is imperative to employ sampling methods that enable the investigator to distinguish between the suspended and sinking pools of particulate matter. This universal requirement for a careful and comprehensive analysis of sedimenting particles has resulted in the development, evaluation and calibration of a variety of in situ particle collectors or sediment traps. The results, after nearly a decade of intensive field experiments, have contributed significantly to our general understanding of: (1) the relationship between the rate of primary production and downward flux of particulate organic matter, (2) mesopelagic zone oxygen consumption and nutrient regeneration, (3) biological control of the removal of abiogenic particles from the surface ocean and (4) seasonal and interannual variations in particle flux to the deep-sea. Future sediment trap studies will, most likely, continue to provide novel and useful data on the rates and mechanisms of important biogeochemical processes. At Station ALOHA, we presently deploy a free-drifting sediment trap array with 12 individual collectors positioned at 150, 300 and 500 m. The deployment period is generally 72 hours. The passively sinking particles are subsequently analyzed for a variety of chemical properties, including: total mass, C, N and P. 2. Precautions Because particle fluxes in oligotrophic habitats are expected to be low, special attention must be paid to the preparation of individual sediment trap collector tubes so that they are clean and free of dust and other potentially contaminating particles. Traps should be capped immediately after filling and immediately after retrieval. Pay particular attention to airborne and/or shipboard particulate contamination sources. In addition, the time interval between trap retrieval and subsample filtration should be minimized in order to limit the inclusion of extraneous abiotic particles and the post-collection solubilization of particles. 3. Field Operations 3.1. Hardware Our free-floating sediment trap array is patterned after the MULTITRAP system pioneered by Knauer et al. (1979) and used extensively in the decade- long VERTEX program. Twelve individual sediment trap collectors (0.0039 m2) are typically deployed at three depths (150, 300 and 500 m). The traps are affixed to a PVC cross attached to 1/2\" polypropylene line. The traps are tracked using VHF radio and Argos satellite transmitters and strobelights. Typically we deploy our traps for a period of 72 hours each cruise. 3.2. Trap solutions Prior to deployment, each trap is cleaned with 1 M HCl, rinsed thoroughly with deionized water then filled with a high density solution to prevent advective-diffusive loss of extractants and preservatives during the deployment period and to eliminate flushing of the traps during recovery (Knauer et al., 1979). The trap solution is prepared by adding 50 g of NaCl to each liter of surface seawater. This brine solution is pressure filtered sequentially through a 1.0 and 0.5 \u00b5m filter cartridge prior to the addition of 10 ml 100% formalin l-1. Individual traps are filled and at least 10 l of the trap solution is saved for analysis of solution blanks (see sections 4.1 and 5.1). 3.3. Post-recovery processing 3.3.1. Upon recovery, individual traps are capped and transported to the shipboard portable laboratory for analysis. Care is taken not to mix the higher density trap solutions with the overlying seawater. Trap samples are processed from deep to shallow in order to minimize potential contamination. 3.3.2. The depth of the interface between the high density solution and overlying seawater is marked on each trap. The overlying seawater is then aspirated with a plastic tube attached to a vacuum system in order to avoid disturbing the high density solution. Because some sinking particulate material collects near the interface between the high density solution and the overlying seawater, the overlying seawater is removed only to a depth that is 5 cm above the previously identified interface. 3.3.3. After the overlying seawater has been removed from all the traps at a given depth, the contents of each trap is passed through an acid rinsed 335 \u00b5m NitexR screen to remove contaminating zooplankton and micronekton which entered the traps in a living state and are not truly part of the passive flux. Immediately before this sieving process, the contents of each trap are mixed to disrupt large amorphous particles. The traps are rinsed with a portion of the <335 \u00b5m sample in order to recover all particulate matter, and the 335 \u00b5m NitexR screen is examined to determine whether residual material, in addition to the so-called \"swimmers\", is present. If so, the screens are rinsed again with a portion of the 335 \u00b5m filtrate. After all traps from a given depth have been processed, the 335 \u00b5m screen is removed and placed into a vial containing 20 ml of formalin- seawater solution, and stored at 4 \u00b0C for subsequent microscopic examination and organism identification and enumeration. 4. Determination of Mass Flux 4.1. Three of the 12 traps deployed at each water depth are used for the determination of mass flux. At our shore-based laboratory, triplicate 250 ml subsamples of the time-zero high density trap solution (blank) and equivalent volumes individual traps (start with the deepest depth and work up), are vacuum filtered through tared 25 mm 0.2 \u00b5m Nuclepore membrane filters (see Chapter 18, sections 4.1.4 to 4.1.3). The tared filters are prepared as follows: 4.1.1. Rinse filters three times with distilled water. Place rinsed filter on a 2.5 cm2 foil square (to reduce static electricity) in a plastic 47 mm petri dish. 4.1.2. Fold the foil in half over the filter and place the petri dish in a drying oven with the lid ajar for 2 hours at 55 \u00b0C. Remove and cool in dessicator for 30 minutes. 4.1.3. Weigh filter to constant weight (i.e., repeat oven drying, cooling and weighing until a relative standard deviation of <0.005% is achieved), on a microbalance capable of 0.1 \u00b5g resolution. Record weights (to the nearest 0.1 \u00b5g) on label tape placed on top of the petri dish. 4.2. After the last of the sample has passed through the filter, the walls of the filter funnel are washed with three consecutive 5 ml rinses of an isotonic (1 M) ammonium formate solution to remove seawater salts. During each rinse, allow the ammonium formate solution to completely cover the filter. 4.3. Return the processed filter to its petri dish, record sample number (on the dish and data sheet), and place in a drying oven at 55 \u00b0C for 8 hours. Alternately, store in a dessicator, if an oven is not immediately available. Dry to constant weight (as in Chapter 18, section 4.1.3). 5\. Determination of C, N and P Flux 5.1. The quantities of particulate C, N and P in the prescreened trap solutions are determined using methods described in Chapters 10 and 11. Six replicate traps are used for C/N determinations and three additional traps for P. Typically, 1.5-2 liters are used for a single C/N or P measurement. An equivalent volume of the time-zero sediment trap solution, filtered through the appropriate filters is used as a C, N or P blank Addendum - PPO4 protocol (April 7, 2015) The method used for the analysis of particulate phosphate (PPO4) has been modified and applied to samples analyzed November 2011 (HOT 236) to the present. The previous protocol was in use over at least the previous 10-year period. The modified procedure included vortexing of the sample prior to a longer leaching time (1 hour versus 30 min) of the GFF filter in 0.15 N HCl at room temperature. Both the previous and modified procedures were tested in paired analyses on samples collected over one year (12 cruises). The modified procedure resulted in higher yields by approximately 50% for water column samples (integrated 0-100 m: old method 1.00\u00b10.27 mmol P m-2, versus 1.56\u00b10.14 mmol P m-2) and approximately 30% for P-flux estimated from sediment trap samples (old method: 0.31\u00b10.07 mg P m-2 d-1 versus 0.40\u00b10.09 mg P m-2 d-1). Please see the HOT Data Report 2012 for more detail |
attribute | NC_GLOBAL | awards_0_award_nid | String | 54915 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-0926766 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=0926766 |
attribute | NC_GLOBAL | awards_0_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_0_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_0_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_0_program_manager | String | David L. Garrison |
attribute | NC_GLOBAL | awards_0_program_manager_nid | String | 50534 |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | version: 2018-04-25 Particle flux data from monthly HOT cruises to deep-water Station ALOHA |
attribute | NC_GLOBAL | Conventions | String | COARDS, CF-1.6, ACDD-1.3 |
attribute | NC_GLOBAL | creator_email | String | info at bco-dmo.org |
attribute | NC_GLOBAL | creator_name | String | BCO-DMO |
attribute | NC_GLOBAL | creator_type | String | institution |
attribute | NC_GLOBAL | creator_url | String | https://www.bco-dmo.org/ |
attribute | NC_GLOBAL | data_source | String | extract_data_as_tsv version 2.3 19 Dec 2019 |
attribute | NC_GLOBAL | date_created | String | 2018-05-23T15:02:45Z |
attribute | NC_GLOBAL | date_modified | String | 2019-12-11T14:43:51Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.737393.1 |
attribute | NC_GLOBAL | Easternmost_Easting | double | -158.0 |
attribute | NC_GLOBAL | geospatial_lat_max | double | 22.75 |
attribute | NC_GLOBAL | geospatial_lat_min | double | 22.75 |
attribute | NC_GLOBAL | geospatial_lat_units | String | degrees_north |
attribute | NC_GLOBAL | geospatial_lon_max | double | -158.0 |
attribute | NC_GLOBAL | geospatial_lon_min | double | -158.0 |
attribute | NC_GLOBAL | geospatial_lon_units | String | degrees_east |
attribute | NC_GLOBAL | geospatial_vertical_max | double | 500.0 |
attribute | NC_GLOBAL | geospatial_vertical_min | double | 70.0 |
attribute | NC_GLOBAL | geospatial_vertical_positive | String | down |
attribute | NC_GLOBAL | geospatial_vertical_units | String | m |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/737393 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | Sediment Trap |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | sediment trap array (spar buoy, radiotransmitter, strobe light, floats, trap supports, collector tubes) |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 737470 |
attribute | NC_GLOBAL | instruments_0_description | String | Sediment traps are specially designed containers deployed in the water column for periods of time to collect particles from the water column falling toward the sea floor. In general a sediment trap has a jar at the bottom to collect the sample and a broad funnel-shaped opening at the top with baffles to keep out very large objects and help prevent the funnel from clogging. This designation is used when the specific type of sediment trap was not specified by the contributing investigator. |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/33/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Sediment Trap |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 518 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | sediment trap array |
attribute | NC_GLOBAL | instruments_1_acronym | String | CHN |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_description | String | PE-2400 Carbon/Nitrogen analyzer with integrator |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 737472 |
attribute | NC_GLOBAL | instruments_1_description | String | A unit that accurately determines the carbon and nitrogen concentrations of organic compounds typically by detecting and measuring their combustion products (CO2 and NO). |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Particulate Organic Carbon/Nitrogen Analyzer |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 654 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | PE-2400 Carbon/Nitrogen analyzer with integrator |
attribute | NC_GLOBAL | instruments_2_acronym | String | Spectrophotometer |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_description | String | spectrophotometer (Perkin-Elmer Lambda 3B) and 1-cm cuvette |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 737473 |
attribute | NC_GLOBAL | instruments_2_description | String | An instrument used to measure the relative absorption of electromagnetic radiation of different wavelengths in the near infra-red, visible and ultraviolet wavebands by samples. |
attribute | NC_GLOBAL | instruments_2_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB20/ |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | Spectrophotometer |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 707 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | spectrophotometer and 1-cm cuvette |
attribute | NC_GLOBAL | instruments_3_acronym | String | Scale |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_description | String | Cahn electronic microbalance |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_nid | String | 737471 |
attribute | NC_GLOBAL | instruments_3_description | String | An instrument used to measure weight or mass. |
attribute | NC_GLOBAL | instruments_3_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB13/ |
attribute | NC_GLOBAL | instruments_3_instrument_name | String | Scale |
attribute | NC_GLOBAL | instruments_3_instrument_nid | String | 714 |
attribute | NC_GLOBAL | instruments_3_supplied_name | String | Cahn electronic microbalance |
attribute | NC_GLOBAL | keywords | String | bco, bco-dmo, biological, carbon, Carbon_n, Carbon_sd_diff, chemical, cruise, data, dataset, delta, Delta_13C, Delta_13C_n, Delta_13C_sd_diff, Delta_15N, Delta_15N_n, Delta_15N_sd_diff, depth, diff, dmo, erddap, filename, flux, inorganic, latitude, longitude, management, mass, Mass_n, Mass_sd_diff, nitrogen, Nitrogen_n, Nitrogen_sd_diff, oceanography, office, P_flux_filename, particulate, phosphorus, Phosphorus_n, Phosphorus_sd_diff, pic, PIC_n, PIC_sd_diff, preliminary, silica, Silica_n, Silica_sd_diff, treatment |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/737393/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/737393 |
attribute | NC_GLOBAL | Northernmost_Northing | double | 22.75 |
attribute | NC_GLOBAL | param_mapping | String | {'737393': {'lat': 'flag - latitude', 'Depth': 'flag - depth', 'lon': 'flag - longitude'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/737393/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | University of Hawaii at Manoa |
attribute | NC_GLOBAL | people_0_affiliation_acronym | String | SOEST |
attribute | NC_GLOBAL | people_0_person_name | String | David M. Karl |
attribute | NC_GLOBAL | people_0_person_nid | String | 50750 |
attribute | NC_GLOBAL | people_0_role | String | Principal Investigator |
attribute | NC_GLOBAL | people_0_role_type | String | originator |
attribute | NC_GLOBAL | people_1_affiliation | String | University of Hawaii at Manoa |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | SOEST |
attribute | NC_GLOBAL | people_1_person_name | String | Lance A Fujieki |
attribute | NC_GLOBAL | people_1_person_nid | String | 51683 |
attribute | NC_GLOBAL | people_1_role | String | Contact |
attribute | NC_GLOBAL | people_1_role_type | String | related |
attribute | NC_GLOBAL | people_2_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_2_person_name | String | Mathew Biddle |
attribute | NC_GLOBAL | people_2_person_nid | String | 708682 |
attribute | NC_GLOBAL | people_2_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_2_role_type | String | related |
attribute | NC_GLOBAL | project | String | HOT |
attribute | NC_GLOBAL | projects_0_acronym | String | HOT |
attribute | NC_GLOBAL | projects_0_description | String | Systematic, long-term observations are essential for evaluating natural variability of Earth’s climate and ecosystems and their responses to anthropogenic disturbances. Since October 1988, the Hawaii Ocean Time-series (HOT) program has investigated temporal dynamics in biology, physics, and chemistry at Stn. ALOHA (22°45' N, 158°W), a deep ocean field site in the oligotrophic North Pacific Subtropical Gyre (NPSG). HOT conducts near monthly ship-based sampling and makes continuous observations from moored instruments to document and study NPSG climate and ecosystem variability over semi-diurnal to decadal time scales. HOT was founded to understand the processes controlling the time-varying fluxes of carbon and associated biogenic elements in the ocean and to document changes in the physical structure of the water column. To achieve these broad objectives, the program has several specific goals: Quantify time-varying (seasonal to decadal) changes in reservoirs and fluxes of carbon (C) and associated bioelements (nitrogen, oxygen, phosphorus, and silicon). Identify processes controlling air-sea C exchange, rates of C transformation through the planktonic food web, and fluxes of C into the ocean’s interior. Develop a climatology of hydrographic and biogeochemical dynamics from which to form a multi-decadal baseline from which to decipher natural and anthropogenic influences on the NPSG ecosystem. Provide scientific and logistical support to ancillary programs that benefit from the temporal context, interdisciplinary science, and regular access to the open sea afforded by HOT program occupation of Sta. ALOHA, including projects implementing, testing, and validating new methodologies, models, and transformative ocean sampling technologies. Over the past 24+ years, time-series research at Station ALOHA has provided an unprecedented view of temporal variability in NPSG climate and ecosystem processes. Foremost among HOT accomplishments are an increased understanding of the sensitivity of bioelemental cycling to large scale ocean-climate interactions, improved quantification of reservoirs and time varying fluxes of carbon, identification of the importance of the hydrological cycle and its influence on upper ocean biogeochemistry, and the creation of long-term data sets from which the oceanic response to anthropogenic perturbation of elemental cycles may be gauged. A defining characteristic of the NPSG is the perennially oligotrophic nature of the upper ocean waters. This biogeochemically reactive layer of the ocean is where air-sea exchange of climate reactive gases occurs, solar radiation fuels rapid biological transformation of nutrient elements, and diverse assemblages of planktonic organisms comprise the majority of living biomass and sustain productivity. The prevailing Ekman convergence and weak seasonality in surface light flux, combined with relatively mild subtropical weather and persistent stratification, result in a nutrient depleted upper ocean habitat. The resulting dearth of bioessential nutrients limits plankton standing stocks and maintains a deep (175 m) euphotic zone. Despite the oligotrophic state of the NPSG, estimates of net organic matter production at Sta. ALOHA are estimated to range ~1.4 and 4.2 mol C m2 yr1. Such respectable rates of productivity have highlighted the need to identify processes supplying growth limiting nutrients to the upper ocean. Over the lifetime of HOT numerous ancillary science projects have leveraged HOT science and infrastructure to examine possible sources of nutrients supporting plankton productivity. Both physical (mixing, upwelling) and biotic (N2 fixation, vertical migration) processes supply nutrients to the upper ocean in this region, and HOT has been instrumental in demonstrating that these processes are sensitive to variability in ocean climate. Station ALOHA - site selection and infrastructure Station ALOHA is a deep water (~4800 m) location approximately 100 km north of the Hawaiian Island of Oahu. Thus, the region is far enough from land to be free of coastal ocean dynamics and terrestrial inputs, but close enough to a major port (Honolulu) to make relatively short duration (45 m depth), below depths of detection by Earth-orbiting satellites. The emerging data emphasize the value of in situ measurements for validating remote and autonomous detection of plankton biomass and productivity and demonstrate that detection of potential secular-scale changes in productivity against the backdrop of significant interannual and decadal fluctuations demands a sustained sampling effort. Careful long-term measurements at Stn. ALOHA also highlight a well-resolved, though relatively weak, seasonal climatology in upper ocean primary productivity. Measurements of 14C-primary production document a ~3-fold increase during the summer months (Karl et al., 2012) that coincides with increases in plankton biomass (Landry et al., 2001; Sheridan and Landry, 2004). Moreover, phytoplankton blooms, often large enough to be detected by ocean color satellites, are a recurrent summertime feature of these waters (White et al., 2007; Dore et al., 2008; Fong et al., 2008). Analyses of ~13-years (1992-2004) of particulate C, N, P, and biogenic Si fluxes collected from bottom-moored deep-ocean (2800 m and 4000 m) sediment traps provide clues to processes underlying these seasonal changes. Unlike the gradual summertime increase in sinking particle flux observed in the upper ocean (150 m) traps, the deep sea particle flux record depicts a sharply defined summer maximum that accounts for ~20% of the annual POC flux to the deep sea, and appears driven by rapidly sinking diatom biomass (Karl et al., 2012). Analyses of the 15N isotopic signatures associated with sinking particles at Sta. ALOHA, together with genetic analyses of N2 fixing microorganisms, implicates upper ocean N2 fixation as a major control on the magnitude and efficiency of the biological carbon pump in this ecosystem (Dore et al., 2002; Church et al., 2009; Karl et al., 2012). Motivating Questions Science results from HOT continue to raise new, important questions about linkages between ocean climate and biogeochemistry that remain at the core of contemporary oceanography. Answers have begun to emerge from the existing suite of core program measurements; however, sustained sampling is needed to improve our understanding of contemporary ecosystem behavior and our ability to make informed projections of future changes to this ecosystem. HOT continues to focus on providing answers to some of the questions below: How sensitive are rates of primary production and organic matter export to short- and long-term climate variability? What processes regulate nutrient supply to the upper ocean and how sensitive are these processes to climate forcing? What processes control the magnitude of air-sea carbon exchange and over what time scales do these processes vary? Is the strength of the NPSG CO2 sink changing in time? To what extent does advection (including eddies) contribute to the mixed layer salinity budget over annual to decadal time scales and what are the implications for upper ocean biogeochemistry? How do variations in plankton community structure influence productivity and material export? What processes trigger the formation and demise of phytoplankton blooms in a persistently stratified ocean ecosystem? References |
attribute | NC_GLOBAL | projects_0_end_date | String | 2014-12 |
attribute | NC_GLOBAL | projects_0_geolocation | String | North Pacific Subtropical Gyre; 22 deg 45 min N, 158 deg W |
attribute | NC_GLOBAL | projects_0_name | String | Hawaii Ocean Time-series (HOT): Sustaining ocean ecosystem and climate observations in the North Pacific Subtropical Gyre |
attribute | NC_GLOBAL | projects_0_project_nid | String | 2101 |
attribute | NC_GLOBAL | projects_0_project_website | String | http://hahana.soest.hawaii.edu/hot/hot_jgofs.html |
attribute | NC_GLOBAL | projects_0_start_date | String | 1988-07 |
attribute | NC_GLOBAL | publisher_name | String | Biological and Chemical Oceanographic Data Management Office (BCO-DMO) |
attribute | NC_GLOBAL | publisher_type | String | institution |
attribute | NC_GLOBAL | sourceUrl | String | (local files) |
attribute | NC_GLOBAL | Southernmost_Northing | double | 22.75 |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | subsetVariables | String | longitude,latitude |
attribute | NC_GLOBAL | summary | String | Particle flux measurements from the Hawaii Ocean Time-Series (HOT). Particle flux was measured at a standard reference depth of 150 m using multiple cylindrical particle interceptor traps deployed on a free-floating array for approximately 60 h during each cruise. Sediment trap design and collection methods are described in Winn et al. (1991). Samples were analyzed for particulate C, N, P & Si. Typically six traps are analyzed for PC and PN, three for PP, and another three traps for PSi. |
attribute | NC_GLOBAL | title | String | [Particle Flux] - Sediment trap flux measurements from the Hawaii Ocean Time-Series (HOT) project at station ALOHA ([Current] Hawaii Ocean Time-series (HOT): 2018-2023; [Previous] Hawaii Ocean Time-series (HOT): Sustaining ocean ecosystem and climate observations in the North Pacific Subtropical Gyre) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | Westernmost_Easting | double | -158.0 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | Cruise | short | ||
attribute | Cruise | _FillValue | short | 32767 |
attribute | Cruise | actual_range | short | 2, 287 |
attribute | Cruise | bcodmo_name | String | cruise_id |
attribute | Cruise | description | String | Cruise Number |
attribute | Cruise | long_name | String | Cruise |
attribute | Cruise | units | String | unitless |
variable | P_flux_filename | String | ||
attribute | P_flux_filename | bcodmo_name | String | file_name |
attribute | P_flux_filename | description | String | Original filename of the particle flux data from HOT |
attribute | P_flux_filename | long_name | String | P Flux Filename |
attribute | P_flux_filename | units | String | unitless |
variable | longitude | double | ||
attribute | longitude | _CoordinateAxisType | String | Lon |
attribute | longitude | _FillValue | double | NaN |
attribute | longitude | actual_range | double | -158.0, -158.0 |
attribute | longitude | axis | String | X |
attribute | longitude | bcodmo_name | String | longitude |
attribute | longitude | colorBarMaximum | double | 180.0 |
attribute | longitude | colorBarMinimum | double | -180.0 |
attribute | longitude | description | String | Longitude with East negative |
attribute | longitude | ioos_category | String | Location |
attribute | longitude | long_name | String | Longitude |
attribute | longitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LONX/ |
attribute | longitude | standard_name | String | longitude |
attribute | longitude | units | String | degrees_east |
variable | latitude | double | ||
attribute | latitude | _CoordinateAxisType | String | Lat |
attribute | latitude | _FillValue | double | NaN |
attribute | latitude | actual_range | double | 22.75, 22.75 |
attribute | latitude | axis | String | Y |
attribute | latitude | bcodmo_name | String | latitude |
attribute | latitude | colorBarMaximum | double | 90.0 |
attribute | latitude | colorBarMinimum | double | -90.0 |
attribute | latitude | description | String | Latitude with South negative |
attribute | latitude | ioos_category | String | Location |
attribute | latitude | long_name | String | Latitude |
attribute | latitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LATX/ |
attribute | latitude | standard_name | String | latitude |
attribute | latitude | units | String | degrees_north |
variable | depth | double | ||
attribute | depth | _CoordinateAxisType | String | Height |
attribute | depth | _CoordinateZisPositive | String | down |
attribute | depth | _FillValue | double | NaN |
attribute | depth | actual_range | double | 70.0, 500.0 |
attribute | depth | axis | String | Z |
attribute | depth | bcodmo_name | String | depth |
attribute | depth | colorBarMaximum | double | 8000.0 |
attribute | depth | colorBarMinimum | double | -8000.0 |
attribute | depth | colorBarPalette | String | TopographyDepth |
attribute | depth | description | String | Depth |
attribute | depth | ioos_category | String | Location |
attribute | depth | long_name | String | Depth |
attribute | depth | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/DEPH/ |
attribute | depth | positive | String | down |
attribute | depth | standard_name | String | depth |
attribute | depth | units | String | m |
variable | Treatment | String | ||
attribute | Treatment | bcodmo_name | String | treatment |
attribute | Treatment | description | String | C-Solutions from individual traps combined and replicate subsamples drawn from this solution. I-Individual traps sampled as replicates. W-Swimmers picked out before analyzed.O-Some other (special?) treatment. |
attribute | Treatment | long_name | String | Treatment |
attribute | Treatment | units | String | unitless |
variable | Carbon | float | ||
attribute | Carbon | _FillValue | float | NaN |
attribute | Carbon | actual_range | float | 3.5, 61.4 |
attribute | Carbon | bcodmo_name | String | C |
attribute | Carbon | description | String | Carbon |
attribute | Carbon | long_name | String | Carbon |
attribute | Carbon | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Carbon_sd_diff | float | ||
attribute | Carbon_sd_diff | _FillValue | float | NaN |
attribute | Carbon_sd_diff | actual_range | float | 0.1, 28.6 |
attribute | Carbon_sd_diff | bcodmo_name | String | C |
attribute | Carbon_sd_diff | colorBarMaximum | double | 50.0 |
attribute | Carbon_sd_diff | colorBarMinimum | double | 0.0 |
attribute | Carbon_sd_diff | description | String | Standard Deviation presented where Carbon_n=3; Difference between replicate presented where Carbon_n=2 |
attribute | Carbon_sd_diff | long_name | String | Carbon Sd Diff |
attribute | Carbon_sd_diff | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Carbon_n | byte | ||
attribute | Carbon_n | _FillValue | byte | 127 |
attribute | Carbon_n | actual_range | byte | 1, 6 |
attribute | Carbon_n | bcodmo_name | String | replicate |
attribute | Carbon_n | description | String | Number of replicate samples collected for replicate analysis. |
attribute | Carbon_n | long_name | String | Carbon N |
attribute | Carbon_n | units | String | unitless |
variable | Nitrogen | float | ||
attribute | Nitrogen | _FillValue | float | NaN |
attribute | Nitrogen | actual_range | float | 0.27, 14.3 |
attribute | Nitrogen | bcodmo_name | String | N |
attribute | Nitrogen | description | String | Nitrogen |
attribute | Nitrogen | long_name | String | Nitrogen |
attribute | Nitrogen | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Nitrogen_sd_diff | float | ||
attribute | Nitrogen_sd_diff | _FillValue | float | NaN |
attribute | Nitrogen_sd_diff | actual_range | float | 0.03, 3.84 |
attribute | Nitrogen_sd_diff | bcodmo_name | String | N |
attribute | Nitrogen_sd_diff | colorBarMaximum | double | 50.0 |
attribute | Nitrogen_sd_diff | colorBarMinimum | double | 0.0 |
attribute | Nitrogen_sd_diff | description | String | Standard Deviation presented where Nitrogen_n=3; Difference between replicate presented where Nitrogen_n=2 |
attribute | Nitrogen_sd_diff | long_name | String | Nitrogen Sd Diff |
attribute | Nitrogen_sd_diff | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Nitrogen_n | byte | ||
attribute | Nitrogen_n | _FillValue | byte | 127 |
attribute | Nitrogen_n | actual_range | byte | 1, 9 |
attribute | Nitrogen_n | bcodmo_name | String | replicate |
attribute | Nitrogen_n | description | String | Number of replicate samples collected for replicate analysis. |
attribute | Nitrogen_n | long_name | String | Nitrogen N |
attribute | Nitrogen_n | units | String | unitless |
variable | Phosphorus | float | ||
attribute | Phosphorus | _FillValue | float | NaN |
attribute | Phosphorus | actual_range | float | 0.008, 1.136 |
attribute | Phosphorus | bcodmo_name | String | PIP |
attribute | Phosphorus | description | String | Phosphorus Addendum - PPO4 protocol (April 7 2015) The method used for the analysis of particulate phosphate (PPO4) has been modified and applied to samples analyzed November 2011 (HOT 236) to the present. The previous protocol was in use over at least the previous 10-year period. The modified procedure included vortexing of the sample prior to a longer leaching time (1 hour versus 30 min) of the GFF filter in 0.15 N HCl at room temperature. Both the previous and modified procedures were tested in paired analyses on samples collected over one year (12 cruises). The modified procedure resulted in higher yields by approximately 50% for water column samples (integrated 0-100 m: old method 1.00±0.27 mmol P m-2 versus 1.56±0.14 mmol P m-2) and approximately 30% for P-flux estimated from sediment trap samples (old method: 0.31±0.07 mg P m-2 d-1 versus 0.40±0.09 mg P m-2 d-1). Please see the HOT Data Report 2012 for more detail. |
attribute | Phosphorus | long_name | String | Phosphorus |
attribute | Phosphorus | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Phosphorus_sd_diff | float | ||
attribute | Phosphorus_sd_diff | _FillValue | float | NaN |
attribute | Phosphorus_sd_diff | actual_range | float | 0.001, 0.366 |
attribute | Phosphorus_sd_diff | bcodmo_name | String | PIP |
attribute | Phosphorus_sd_diff | colorBarMaximum | double | 50.0 |
attribute | Phosphorus_sd_diff | colorBarMinimum | double | 0.0 |
attribute | Phosphorus_sd_diff | description | String | Standard Deviation presented where Phosphorus_n=3; Difference between replicate presented where Phosphorus_n=2 |
attribute | Phosphorus_sd_diff | long_name | String | Phosphorus Sd Diff |
attribute | Phosphorus_sd_diff | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Phosphorus_n | byte | ||
attribute | Phosphorus_n | _FillValue | byte | 127 |
attribute | Phosphorus_n | actual_range | byte | 1, 3 |
attribute | Phosphorus_n | bcodmo_name | String | replicate |
attribute | Phosphorus_n | description | String | Number of replicate samples collected for replicate analysis. |
attribute | Phosphorus_n | long_name | String | Phosphorus N |
attribute | Phosphorus_n | units | String | unitless |
variable | Mass | float | ||
attribute | Mass | _FillValue | float | NaN |
attribute | Mass | actual_range | float | 8.5, 131.0 |
attribute | Mass | bcodmo_name | String | mass |
attribute | Mass | description | String | Mass |
attribute | Mass | long_name | String | Mass |
attribute | Mass | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Mass_sd_diff | float | ||
attribute | Mass_sd_diff | _FillValue | float | NaN |
attribute | Mass_sd_diff | actual_range | float | 0.3, 49.1 |
attribute | Mass_sd_diff | bcodmo_name | String | mass |
attribute | Mass_sd_diff | colorBarMaximum | double | 50.0 |
attribute | Mass_sd_diff | colorBarMinimum | double | 0.0 |
attribute | Mass_sd_diff | description | String | Standard Deviation presented where Mass_n=3; Difference between replicate presented where Mass_n=2 |
attribute | Mass_sd_diff | long_name | String | Mass Sd Diff |
attribute | Mass_sd_diff | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Mass_n | byte | ||
attribute | Mass_n | _FillValue | byte | 127 |
attribute | Mass_n | actual_range | byte | 2, 8 |
attribute | Mass_n | bcodmo_name | String | replicate |
attribute | Mass_n | description | String | Number of replicate samples collected for replicate analysis. |
attribute | Mass_n | long_name | String | Mass N |
attribute | Mass_n | units | String | unitless |
variable | Silica | float | ||
attribute | Silica | _FillValue | float | NaN |
attribute | Silica | actual_range | float | 0.189, 21.579 |
attribute | Silica | bcodmo_name | String | Si |
attribute | Silica | description | String | Silica |
attribute | Silica | long_name | String | Silica |
attribute | Silica | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Silica_sd_diff | float | ||
attribute | Silica_sd_diff | _FillValue | float | NaN |
attribute | Silica_sd_diff | actual_range | float | 0.03, 7.367 |
attribute | Silica_sd_diff | bcodmo_name | String | Si |
attribute | Silica_sd_diff | colorBarMaximum | double | 50.0 |
attribute | Silica_sd_diff | colorBarMinimum | double | 0.0 |
attribute | Silica_sd_diff | description | String | Standard Deviation presented where Silica_n=3; Difference between replicate presented where Silica_n=2 |
attribute | Silica_sd_diff | long_name | String | Silica Sd Diff |
attribute | Silica_sd_diff | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Silica_n | byte | ||
attribute | Silica_n | _FillValue | byte | 127 |
attribute | Silica_n | actual_range | byte | 2, 3 |
attribute | Silica_n | bcodmo_name | String | replicate |
attribute | Silica_n | description | String | Number of replicate samples collected for replicate analysis. |
attribute | Silica_n | long_name | String | Silica N |
attribute | Silica_n | units | String | unitless |
variable | Delta_15N | float | ||
attribute | Delta_15N | _FillValue | float | NaN |
attribute | Delta_15N | actual_range | float | -1.17, 6.89 |
attribute | Delta_15N | bcodmo_name | String | d15N |
attribute | Delta_15N | description | String | Delta-15N of PN (permil vs. air-N2) |
attribute | Delta_15N | long_name | String | Delta 15 N |
attribute | Delta_15N | units | String | permil vs. air-N2 |
variable | Delta_15N_sd_diff | float | ||
attribute | Delta_15N_sd_diff | _FillValue | float | NaN |
attribute | Delta_15N_sd_diff | actual_range | float | 0.0, 1.93 |
attribute | Delta_15N_sd_diff | bcodmo_name | String | d15N |
attribute | Delta_15N_sd_diff | colorBarMaximum | double | 50.0 |
attribute | Delta_15N_sd_diff | colorBarMinimum | double | 0.0 |
attribute | Delta_15N_sd_diff | description | String | Standard Deviation presented where Delta_15N_n=3; Difference between replicate presented where Delta_15N_n=2 |
attribute | Delta_15N_sd_diff | long_name | String | Delta 15 N Sd Diff |
attribute | Delta_15N_sd_diff | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Delta_15N_n | byte | ||
attribute | Delta_15N_n | _FillValue | byte | 127 |
attribute | Delta_15N_n | actual_range | byte | 1, 6 |
attribute | Delta_15N_n | bcodmo_name | String | replicate |
attribute | Delta_15N_n | description | String | Number of replicate samples collected for replicate analysis. |
attribute | Delta_15N_n | long_name | String | Delta 15 N N |
attribute | Delta_15N_n | units | String | unitless |
variable | Delta_13C | float | ||
attribute | Delta_13C | _FillValue | float | NaN |
attribute | Delta_13C | actual_range | float | -27.5, -16.96 |
attribute | Delta_13C | bcodmo_name | String | delta13C |
attribute | Delta_13C | description | String | Delta-13C of PC (permil vs. VPDB) |
attribute | Delta_13C | long_name | String | Delta 13 C |
attribute | Delta_13C | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/D13CMITX/ |
attribute | Delta_13C | units | String | permil vs. VPDB |
variable | Delta_13C_sd_diff | float | ||
attribute | Delta_13C_sd_diff | _FillValue | float | NaN |
attribute | Delta_13C_sd_diff | actual_range | float | 0.05, 1.94 |
attribute | Delta_13C_sd_diff | bcodmo_name | String | delta13C |
attribute | Delta_13C_sd_diff | colorBarMaximum | double | 50.0 |
attribute | Delta_13C_sd_diff | colorBarMinimum | double | 0.0 |
attribute | Delta_13C_sd_diff | description | String | Standard Deviation presented where Delta_13C_n=3; Difference between replicate presented where Delta_13C_n=2 |
attribute | Delta_13C_sd_diff | long_name | String | Delta 13 C Sd Diff |
attribute | Delta_13C_sd_diff | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/D13CMITX/ |
attribute | Delta_13C_sd_diff | units | String | miligrams per square meter per day (mg/m2/d) |
variable | Delta_13C_n | byte | ||
attribute | Delta_13C_n | _FillValue | byte | 127 |
attribute | Delta_13C_n | actual_range | byte | 1, 6 |
attribute | Delta_13C_n | bcodmo_name | String | replicate |
attribute | Delta_13C_n | description | String | Number of replicate samples collected for replicate analysis. |
attribute | Delta_13C_n | long_name | String | Delta 13 C N |
attribute | Delta_13C_n | units | String | unitless |
variable | PIC | float | ||
attribute | PIC | _FillValue | float | NaN |
attribute | PIC | actual_range | float | 0.04, 9.63 |
attribute | PIC | bcodmo_name | String | PIC |
attribute | PIC | description | String | Particulate Inorganic Carbon |
attribute | PIC | long_name | String | Particulate Inorganic Carbon |
attribute | PIC | units | String | miligrams per square meter per day (mg/m2/d) |
variable | PIC_sd_diff | float | ||
attribute | PIC_sd_diff | _FillValue | float | NaN |
attribute | PIC_sd_diff | actual_range | float | 0.0, 4.56 |
attribute | PIC_sd_diff | bcodmo_name | String | PIC |
attribute | PIC_sd_diff | colorBarMaximum | double | 50.0 |
attribute | PIC_sd_diff | colorBarMinimum | double | 0.0 |
attribute | PIC_sd_diff | description | String | Standard Deviation presented where PIC_n=3; Difference between replicate presented where PIC_n=2 |
attribute | PIC_sd_diff | long_name | String | PIC Sd Diff |
attribute | PIC_sd_diff | units | String | miligrams per square meter per day (mg/m2/d) |
variable | PIC_n | byte | ||
attribute | PIC_n | _FillValue | byte | 127 |
attribute | PIC_n | actual_range | byte | 1, 3 |
attribute | PIC_n | bcodmo_name | String | replicate |
attribute | PIC_n | description | String | Number of replicate samples collected for replicate analysis. |
attribute | PIC_n | long_name | String | PIC N |
attribute | PIC_n | units | String | unitless |
The information in the table above is also available in other file formats (.csv, .htmlTable, .itx, .json, .jsonlCSV1, .jsonlCSV, .jsonlKVP, .mat, .nc, .nccsv, .tsv, .xhtml) via a RESTful web service.