CAFA Publications

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Comparing Dynamic And Static Time-Area Closures For Bycatch Mitigation: A Management Strategy Evaluation Of A Swordfish Fishery

Project: From physics to fisheries: A social-ecological management strategy evaluation for the California Current Large Marine Ecosystem
Year: 2021

Author(s): Smith JA, et al


Project PI: Jacox
DOI: https://doi.org/10.3389/fmars.2021.630607

Time-area closures are a valuable tool for mitigating fisheries bycatch. There is increasing recognition that dynamic closures, which have boundaries that vary across space and time, can be more effective than static closures at protecting mobile species in dynamic environments. We created a management strategy evaluation to compare static and dynamic closures in a simulated fishery based on the California drift gillnet swordfish fishery, with closures aimed at reducing bycatch of leatherback turtles. We tested eight operating models that varied swordfish and leatherback distributions, and within each evaluated the performance of three static and five dynamic closure strategies. We repeated this under 20 and 50% simulated observer coverage to alter the data available for closure creation. We found that static closures can be effective for reducing bycatch of species with more geographically associated distributions, but to avoid redistributing bycatch the static areas closed should be based on potential (not just observed) bycatch. Only dynamic closures were effective at reducing bycatch for more dynamic leatherback distributions, and they generally reduced bycatch risk more than they reduced target catch. Dynamic closures were less likely to redistribute fishing into rarely fished areas, by leaving open pockets of lower risk habitat, but these closures were often fragmented which would create practical challenges for fishers and managers and require a mobile fleet. Given our simulation’s catch rates, 20% observer coverage was sufficient to create useful closures and increasing coverage to 50% added only minor improvement in closure performance. Even strict static or dynamic closures reduced leatherback bycatch by only 30–50% per season, because the simulated leatherback distributions were broad and open areas contained considerable bycatch risk. Perfect knowledge of the leatherback distribution provided an additional 5–15% bycatch reduction over a dynamic closure with realistic predictive accuracy. This moderate level of bycatch reduction highlights the limitations of redistributing fishing effort to reduce bycatch of broadly distributed and rarely encountered species, and indicates that, for these species, spatial management may work best when used with other bycatch mitigation approaches. We recommend future research explores methods for considering model uncertainty in the spatial and temporal resolution of dynamic closures.

A Case Study In Connecting Fisheries Management Challenges With Models And Analysis To Support Ecosystem-Based Management In The California Current Ecosystem

Project: From physics to fisheries: A social-ecological management strategy evaluation for the California Current Large Marine Ecosystem
Year: 2021

Author(s): Tommasi, Desiree, et al


Project PI: Jacox
DOI: https://doi.org/10.3389/fmars.2021.624161

One of the significant challenges to using information and ideas generated through ecosystem models and analyses for ecosystem-based fisheries management is the disconnect between modeling and management needs. Here we present a case study from the U.S. West Coast, the stakeholder review of NOAA’s annual ecosystem status report for the California Current Ecosystem established by the Pacific Fisheries Management Council’s Fisheries Ecosystem Plan, showcasing a process to identify management priorities that require information from ecosystem models and analyses. We then assess potential ecosystem models and analyses that could help address the identified policy concerns. We screened stakeholder comments and found 17 comments highlighting the need for ecosystem-level synthesis. Policy needs for ecosystem science included: (1) assessment of how the environment affects productivity of target species to improve forecasts of biomass and reference points required for setting harvest limits, (2) assessment of shifts in the spatial distribution of target stocks and protected species to anticipate changes in availability and the potential for interactions between target and protected species, (3) identification of trophic interactions to better assess tradeoffs in the management of forage species between the diet needs of dependent predators, the resilience of fishing communities, and maintenance of the forage species themselves, and (4) synthesis of how the environment affects efficiency and profitability in fishing communities, either directly via extreme events (e.g., storms) or indirectly via climate-driven changes in target species availability. We conclude by exemplifying an existing management process established on the U.S. West Coast that could be used to enable the structured, iterative, and interactive communication between managers, stakeholders, and modelers that is key to refining existing ecosystem models and analyses for management use.

Climate Change May Cause Shifts In Growth And Instantaneous Natural Mortality Of American Shad Throughout Their Native Range

Project: Understanding climate impacts on American shad recovery, fisheries management, and influences of dams
Year: 2021

Author(s): Gilligan‐Lunda, Erin K., Daniel S. Stich, Katherine E. Mills, Michael M. Bailey, and Joseph D. Zydlewski


Project PI: Stich
DOI: https://doi.org/10.1002/tafs.10299

American Shad Alosa sapidissima is an anadromous species with populations ranging along the U.S. Atlantic coast. Past American Shad stock assessments have been data limited and estimating system-specific growth parameters or instantaneous natural mortality (M) was not possible. This precluded system-specific stock assessment and management due to reliance on these parameters for estimating other population dynamics (such as yield per recruit). Furthermore, climate-informed biological reference points remain a largely unaddressed need in American Shad stock assessment. Population abundance estimates of American Shad and other species often rely heavily on M derived from von Bertalanffy growth function (VBGF) parameters. Therefore, we developed Bayesian hierarchical models to estimate coastwide, regional, and system-specific VBGF parameters and M using data collected from 1982 to 2017. We tested predictive performance of models that included effects of various climate variables on VBGF parameters within these models. System-specific models were better supported than regional or coast-wide models. Mean asymptotic length (L∞) decreased with increasing mean annual sea surface temperature (SST) and degree days (DD) experienced by fish during their lifetime. Although uncertain, K (Brody growth coefficient) decreased over the same range of lifetime SST and DD. Assuming no adaptation, we projected changes in VBGF parameters and M through 2099 using modeled SST from two climate projection scenarios (Representative Concentration Pathways 4.5 and 8.5). We predicted reduced growth under both scenarios, and M was projected to increase by about 0.10. It is unclear how reduced growth and increased mortality may influence population productivity or life history adaptation in the future, but our results may inform stock assessment models to assess those trade-offs.

Impact Of Larval Behaviors On Dispersal And Connectivity Of Sea Scallop Larvae Over The Northeast U.S. Shelf

Project: Climate-fisheries dynamics: Individual-based end-to-end sea scallop model with socio-economic feedbacks
Year: 2021

Author(s): Chen, C., Zhao, L., Gallager, S., Ji, R., He, P., Davis, C. S., Beardsley, R.C., Hart, D., Gentleman, W.C., Wang, L., Li, S., Lin, H., Stokesbury, K., Bethoney, D.


Project PI: Ji/David/Rubao
DOI: https://doi.org/10.1016/j.pocean.2021.102604

Sea scallops (Placopecten magellanicus) are a highly fecund species that supports one of the most commercially valuable fisheries in the northeast U.S. continental shelf region. Scallop landings exhibit significant interannual variability, with abundances widely varied due to a combination of anthropogenic and natural factors. By coupling a pelagic-stage Individual-Based scallop population dynamics Model (hereafter referred to as Scallop-IBM) with the Northeast Coastal Ocean Forecast System (NECOFS) and considering the persistent aggregations over Georges Bank (GB)/Great South Channel (GSC) as source beds, we have examined the dispersion and settlement of scallop larvae over 1978–2016. The results demonstrated that the significant interannual variability of larval dispersal was driven by biophysical interactions associated with scallop larval swimming behaviors in their early stages. The duration, frequency, and stimulus of larval vertical migration in the ocean mixed layer (OML) affected the residence time of larvae in the water column over GB. It thus sustained the persistent aggregations of scallops in the GB/GSC and Southern New England region. In addition to larval behavior in the OML, the larval transport to the Middle Atlantic Bight (MAB) was also closely related to the intensity and duration of northeasterly wind in autumn. There was no conspicuous connectivity of scallop larvae between GB/GSC and MAB in the past 39 years except in the autumn of 2009. In 2009, the significant larval transport to the MAB was produced by unusually strong northeasterly winds. Ignoring larval behavior in the OML could overestimate the scallop population’s connectivity between GB and the MAB and thus provide an unrealistic prediction of scallop larval recruitment in the region. Both satellite-derived SST and NECOFS show that the northeast U.S. shelf experienced climate change-induced warming. The extreme warming at the shelfbreak off GB tends to intensify the cross-isobath water temperature gradient and enhance the clockwise subtidal gyre over GB. This change can increase the larval retention rate over GB/GSC, facilitating enhanced productivity on GB.

Projected shifts in 21st century sardine distribution and catch in the California Current

Project: A high-resolution physical-biological study of the Northeast U.S. shelf: past variability and future change
Year: 2021

Author(s): Fiechter, J., Buil, M.P., Jacox, M.G., Alexander, M.A. and Rose, K.A.


Project PI: Curchister
DOI: http://doi.org/10.3389/fmars.2021.685241

Predicting changes in the abundance and distribution of small pelagic fish species in response to anthropogenic climate forcing is of paramount importance due to the ecological and socioeconomic importance of these species, especially in eastern boundary current upwelling regions. Coastal upwelling systems are notorious for the wide range of spatial (from local to basin) and temporal (from days to decades) scales influencing their physical and biogeochemical environments and, thus, forage fish habitat. Bridging those scales can be achieved by using high-resolution regional models that integrate global climate forcing downscaled from coarser resolution earth system models. Here, “end-to-end” projections for 21st century sardine population dynamics and catch in the California Current system (CCS) are generated by coupling three dynamically downscaled earth system model solutions to an individual-based fish model and an agent-based fishing fleet model. Simulated sardine population biomass during 2000–2100 exhibits primarily low-frequency (decadal) variability, and a progressive poleward shift driven by thermal habitat preference. The magnitude of poleward displacement varies noticeably under lower and higher warming conditions (500 and 800 km, respectively). Following the redistribution of the sardine population, catch is projected to increase by 50–70% in the northern CCS and decrease by 30–70% in the southern and central CCS. However, the late-century increase in sardine abundance (and hence, catch) in the northern CCS exhibits a large ensemble spread and is not statistically identical across the three downscaled projections. Overall, the results illustrate the benefit of using dynamical downscaling from multiple earth system models as input to high-resolution regional end-to-end (“physics to fish”) models for projecting population responses of higher trophic organisms to global climate change.

Changes to the structure and function of the albacore fishery reveal shifting social-ecological realities for Pacific Northwest fishermen

Project: A high-resolution physical-biological study of the Northeast U.S. shelf: past variability and future change
Year: 2021

Author(s): Frawley, T.H., Muhling, B.A., Brodie, S., Fisher, M.C., Tommasi, D., Le Fol, G., Hazen, E.L., Stohs, S.S., Finkbeiner, E.M. and Jacox, M.G.


Project PI: Curchister
DOI: http://doi.org/10.1111/faf.12519

Marine fisheries around the globe are increasingly exposed to external drivers of social and ecological change. Though diversification and flexibility have historically helped marine resource users negotiate risk and adversity, much of modern fisheries management treats fishermen as specialists using specific gear types to target specific species. Here, we describe the evolution of harvest portfolios amongst Pacific Northwest fishermen over 35+ years with explicit attention to changes in the structure and function of the albacore (Thunnus alalunga, Scombridae) troll and pole-and-line fishery. Our analysis indicates that recent social–ecological changes have had heterogenous impacts upon the livelihood strategies favoured by different segments of regional fishing fleets. As ecological change and regulatory reform have restricted access to a number of fisheries, many of the regional small (<45 ft) and medium (45–60 ft) boat fishermen who continue to pursue diverse livelihood strategies have increasingly relied upon the ability to opportunistically target albacore in coastal waters while retaining more of the value generated by such catch. In contrast, large vessels (>60 ft) targeting albacore are more specialized now than previously observed, even as participation in multiple fisheries has become increasingly common for this size class. In describing divergent trajectories associated with the albacore fishery, one of the US West Coast's last open-access fisheries, we highlight the diverse strategies and mechanisms utilized to sustain fisheries livelihoods in the modern era while arguing that alternative approaches to management and licensing may be required to maintain the viability of small-scale fishing operations worldwide moving forward.

Management strategy evaluation: allowing the light on the hill to illuminate more than one species

Project: A high-resolution physical-biological study of the Northeast U.S. shelf: past variability and future change
Year: 2021

Author(s): Kaplan, I.C., Gaichas, S.K., Stawitz, C.C., Lynch, P.D., Marshall, K.N., Deroba, J.J., Masi, M., Brodziak, J.K., Aydin, K.Y., Holsman, K. and Townsend, H


Project PI: Curchister
DOI: http:// https://doi.org/10.3389/fmars.2021.624355

Management strategy evaluation (MSE) is a simulation approach that serves as a “light on the hill” (Smith, 1994) to test options for marine management, monitoring, and assessment against simulated ecosystem and fishery dynamics, including uncertainty in ecological and fishery processes and observations. MSE has become a key method to evaluate trade-offs between management objectives and to communicate with decision makers. Here we describe how and why MSE is continuing to grow from a single species approach to one relevant to multi-species and ecosystem-based management. In particular, different ecosystem modeling approaches can fit within the MSE process to meet particular natural resource management needs. We present four case studies that illustrate how MSE is expanding to include ecosystem considerations and ecosystem models as ‘operating models’ (i.e., virtual test worlds), to simulate monitoring, assessment, and harvest control rules, and to evaluate tradeoffs via performance metrics. We highlight United States case studies related to fisheries regulations and climate, which support NOAA’s policy goals related to the Ecosystem Based Fishery Roadmap and Climate Science Strategy but vary in the complexity of population, ecosystem, and assessment representation. We emphasize methods, tool development, and lessons learned that are relevant beyond the United States, and the additional benefits relative to single-species MSE approaches.

Bering Sea dynamical downscaling: Environmental and lower trophic level responses to climate forcing in CMIP6

Project: The Alaska climate integrate modeling project phase 2: Building pathways to resilience, through evaluation of climate impacts, risk, and adaptation responses of marine ecosystems, fisheries, and coastal communities in the Bering Sea, Alaska
Year: 2021

Author(s): Cheng, Wei, A. Hermann, A. Hollowed, K. Holsman, K. Kearney, D. Pilcher, C. Stock, K. Aydin


Project PI: Hollowed
DOI: http://doi.org/10.1016/j.dsr2.2021.104975

In this study we present projected changes in the Eastern Bering Sea shelf (EBS) biophysical processes in response to climate forcing scenarios from the Coupled Model Intercomparison Phase 6 (CMIP6). These changes are obtained by dynamical downscaling using a Bering Sea regional model. Surface atmospheric and ocean boundary forcing from three Earth System Models (ESMs) in CMIP6, and a low and a high emission scenario of Shared Socioeconomic Pathway (SSP126 and SSP585) of each of the ESMs are considered. Ensemble mean results suggest that, contrary to an anticipated increase in ocean stratification under warming, diminishing ice cover in response to climate forcing and resultant reduced surface freshening weakens EBS stratification in the melt season. Modeled ensemble mean phytoplankton and zooplankton biomass on the EBS exhibits subsurface maxima during the growing season; the amplitude of these maxima decreases with warming, along with a reduction in primary productivity and oxygen concentration over much of the EBS water column. Phenology of both phytoplankton and zooplankton biomass on the EBS shifts earlier, leading to an increase (decrease) in biomass averaged between April–July (August–November), while annually averaged biomass decreases under warming. Projected changes of primary and secondary plankton biomass at the end of the 21st century are not well separated between the SSP126 and SSP585 scenario in light of the large across model spread under each scenario. The projected ensemble mean warming amplitude of the EBS summer bottom temperature is largely unchanged between results forced by the Coupled Model Intercomparison Phase 5 Representative Concentration Pathway 8.5 (CMIP5 RCP8.5) and CMIP6 SSP585 scenarios. Likewise, the reduction rate of annual mean phytoplankton and large zooplankton biomass are comparable between RCP8.5 and SSP585 projections, even though the absolute amplitudes of biomass are sensitive to modeling parameters such as the solar irradiance attenuation curve. Hence, within the Bering Sea dynamical downscaling framework, projected long-term warming trends in EBS bottom temperature and plankton biomass reduction rates are robust responses to climate forcing.

Next-generation regional ocean projections for living marine resource management in a changing climate

Project: The Alaska climate integrate modeling project phase 2: Building pathways to resilience, through evaluation of climate impacts, risk, and adaptation responses of marine ecosystems, fisheries, and coastal communities in the Bering Sea, Alaska
Year: 2021

Author(s): Drenkard, E., C. Stock, A. Adcroft, M. Alexander, V. Balaji, S. J. Bograd, M. Butenschön, W. Cheng, E. Curchitser, E. Di Lorenzo, K. W. Dixon, R. Dussin, A. Haynie, M. Harrison, A. Hermann, A. Hollowed, K. Holsman, J. Holt, M. G. Jacox, C. Joo Jang, K. A. Kearney, B. A. Muhling, M. Pozo Buil, A. C. Ross, V. Saba, A. Britt Sandø, D. Tommasi, M. Wang.


Project PI: Hollowed
DOI: http://doi.org/10.1093/icesjms/fsab100

Efforts to manage living marine resources (LMRs) under climate change need projections of future ocean conditions, yet most global climate models (GCMs) poorly represent critical coastal habitats. GCM utility for LMR applications will increase with higher spatial resolution but obstacles including computational and data storage costs, obstinate regional biases, and formulations prioritizing global robustness over regional skill will persist. Downscaling can help address GCM limitations, but significant improvements are needed to robustly support LMR science and management. We synthesize past ocean downscaling efforts to suggest a protocol to achieve this goal. The protocol emphasizes LMR-driven design to ensure delivery of decision-relevant information. It prioritizes ensembles of downscaled projections spanning the range of ocean futures with durations long enough to capture climate change signals. This demands judicious resolution refinement, with pragmatic consideration for LMR-essential ocean features superseding theoretical investigation. Statistical downscaling can complement dynamical approaches in building these ensembles. Inconsistent use of bias correction indicates a need for objective best practices. Application of the suggested protocol should yield regional ocean projections that, with effective dissemination and translation to decision-relevant analytics, can robustly support LMR science and management under climate change.

Fitting growth models to otolith increments to reveal time-varying growth

Project: The Alaska climate integrate modeling project phase 2: Building pathways to resilience, through evaluation of climate impacts, risk, and adaptation responses of marine ecosystems, fisheries, and coastal communities in the Bering Sea, Alaska
Year: 2021

Author(s): Essington, T. E., M. E. Matta, B. A. Black, T. E. Helser, P. D. Spencer.


Project PI: Hollowed
DOI: http://doi.org/10.1139/cjfas-2021-0046

Identifying changes in fish growth is important for accurate scientific advice used for fisheries management, because environmental change is affecting fish growth and size-at-age is a critical component of contemporary stock assessment methods. Growth-increment biochronologies are time series of growth-increments derived from hard parts of marine organisms that may reveal dynamics of somatic fish growth. Here we use time series of otolith increments of two fish stocks to fit and compare a biologically derived growth model and a generalized statistical model. Both models produced similar trajectories of annual growth trends, but the biologically based one was more precise and predicted smaller interannual fluctuations than the statistical model. The biologically based model strongly indicated covariance between anabolic and catabolic rates among individuals. Otolith size-at-age did not closely match fish length-at-age, and consequently the growth model could not accurately hindcast observed fish length-at-age. For these reasons, fitted growth dynamics from otolith biochronologies may best suited to identify growth rate fluctuations, understand past drivers of growth dynamics, and improve ecological forecast in the face of rapid environmental change.



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A look back at 2014: NOAA Climate Program Office articulates roadmap for future progress in climate science

  • 12 January 2015
A look back at 2014: NOAA Climate Program Office articulates roadmap for future progress in climate science

In 2014, NOAA’s Climate Program Office, led by Director Wayne Higgins, went through the process of rearticulating its mission, vision, and unique value through the development of the CPO Strategic Plan. The office also made major progress on an Implementation Plan that provides a roadmap to achieving important outcomes in climate science.

These accomplishments were just one of the highlights of a productive year for NOAA CPO, which continued to make advances in climate observation, research, modeling, and decision support activities for society. We also moved forward with global observations, advanced modeling and prediction capabilities, coastal resilience, drought monitoring and decision-support services, and so many other activities that will help people, businesses and ecosystems thrive in the face of climate and its impacts.

 

Observing the Climate System

NOAA joins with Princeton and other institutions in six-year study to help public better understand Southern Ocean

Princeton University, NOAA and eight other partner institutions now seek to make the Southern Ocean better known scientifically and publicly through a $21 million program that will create a biogeochemical and physical portrait of the ocean using hundreds of robotic floats deployed around Antarctica and an expanded computational capacity. The Southern Ocean Carbon and Climate Observations and Modeling program, or SOCCOM, is a six-year initiative headquartered at Princeton and funded by the National Science Foundation’s Division of Polar Programs, with additional support from the NOAA and NASA. The U.S. Argo program will play a major role in the project.

Deep Argo floats deployed in Pacific

In mid-June, the Research Vessel Tangaroa, operated by New Zealand’s National Institute of Water and Atmospheric Research, set off from Wellington, New Zealand, for the Deep Argo Development cruise. The primary objectives of the cruise were (1) to deploy two prototype Deep Argo (6,000 meter plus) floats and (2) undertake deep (~5500m) CTD casts for sensor testing and development.  In addition, 6 SOLO2 Argo (2,000 meter) floats were deployed in transit, finally, to make a "virtual field trip" for school uptake. The SOLO2 floats and the Deep Argo floats were provided by Scripps Institution of Oceanography as part of NOAA’s Argo Program.

Advancing our Understanding of the Climate System

Developing the Next-Generation CFS

NOAA’s Climate program Office continued to move forward with advancing modeling and prediction capabilities. Along with the National Centers for Environmental Prediction (NCEP), the office co-organized a topical collection of papers presented at a 2012 workshop held to evaluate progress in Climate Forecast System version 2 (CFSv2) performance.  CFSv2 is a couple global climate model used to simulate intraseasonal-to-interannual climate variability. CPO sponsored research significantly contributed to the development of CFSv2. This collection of papers should provide insight for the development of the next generation CFS.

Researchers offer new insights into predicting future droughts in California

A report from the NOAA Drought Task Force, organized by the Modeling, Analysis, and Predictions, and projections (MAPP) Program of NOAA’s Climate Program Office, contributed to a growing field of science-climate attribution--where teams of scientists aim to identify the sources of observed climate and weather patterns. According to the study, natural oceanic and atmospheric patterns are the primary drivers behind California's ongoing drought. Further studies on these oceanic conditions and their effect on California's climate may lead to advances in drought early warning that can help water managers and major industries better prepare for lengthy dry spells in the future.

Understanding aerosol processes using measurements collected from field campaigns

A paper published in the Journal for Atmospheric Chemistry and Physics quantified the performance of the Weather Research and Forecasting regional model with chemistry (WRF-Chem) in simulating the spatial and temporal variations in aerosol mass, composition, and size over California using the extensive meteorological, trace gas, and aerosol measurements collected during the California Nexus of Air Quality and Climate Experiment (CalNex) and the Carbonaceous Aerosol and Radiative Effects Study (CARES) conducted during May and June of 2010. The scientists concluded that the combined CalNex and CARES data sets are an ideal test bed that can be used to evaluate aerosol models in great detail and develop improved treatments for aerosol processes.

Informing Society

President signs NIDIS Reauthorization Act

NOAA’s Climate Program Office played major roles in flagship climate programs, including the reauthorization of the National Integrated Drought Information System (NIDIS). On March 6, President Barack Obama signed the National Integrated Drought Information System Reauthorization Act into law in order to ensure that the federal government can provide timely, effective drought warning forecasts and vital support to communities that are vulnerable to drought. States, cities, towns, farmers, and businesses rely on tools and data from the National Integrated Drought Information System to make informed decisions about water use, crop planting, wildfire response, and other critical areas.  

CPO Supports Major Assessment Reports Released in 2014

CPO’s funded scientists, projects, and program managers contributed to several major assessment reports released over the past year. Among these, the Arctic Research Program in the NOAA Climate Program Office supported the 2014 Arctic Report Card. The latest update confirmed that Arctic air temperatures continue to rise at more than twice the rate of the planet as a whole. Earlier in the year, NOAA and the American Meteorological Society released the 2013 State of the Climate report. The report, a 24-year tradition encompassing the work of 425 authors from 57 countries, uses dozens of climate indicators to track patterns, changes, and trends of the global climate system. Scientific research funded by CPO was also foundational to advancing the 2014 Third National Climate Assessment Report and the Intergovernmental Panel on Climate Change (IPCC) reports.

Climate.gov wins two Webby Awards and a People’s Voice Award

With 12,000 entries from all 50 US states and 60 plus countries and two millions votes in the Webby People’s Voice Awards, the 18th Annual Webby Awards was the biggest yet. NOAA Climate.gov was selected by the International Academy of the Digital Arts & Sciences to receive two Webby Awards in the "Government" and "Green" categories.  The cross-agency team of world-class scientists, data visualizers, web developers, and science writers also garnered a People's Voice Award in the "Green" category (placing second overall in the "Government" category).

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