Damian L. Arévalo‐Martínez

ORCID: 0000-0003-2933-1586
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About
Contact & Profiles
Research Areas
  • Marine and coastal ecosystems
  • Ocean Acidification Effects and Responses
  • Atmospheric and Environmental Gas Dynamics
  • Methane Hydrates and Related Phenomena
  • Oceanographic and Atmospheric Processes
  • Atmospheric Ozone and Climate
  • Marine Biology and Ecology Research
  • Ionosphere and magnetosphere dynamics
  • Atmospheric chemistry and aerosols
  • Groundwater and Isotope Geochemistry
  • Arctic and Antarctic ice dynamics
  • Wastewater Treatment and Nitrogen Removal
  • Microbial Community Ecology and Physiology
  • Spectroscopy and Laser Applications
  • Geological Studies and Exploration
  • Geophysics and Gravity Measurements
  • Earthquake Detection and Analysis
  • Arctic and Russian Policy Studies
  • Cardiovascular and Diving-Related Complications
  • Coastal and Marine Management
  • Analytical Chemistry and Sensors
  • Hydrocarbon exploration and reservoir analysis
  • Solar and Space Plasma Dynamics
  • Agriculture Sustainability and Environmental Impact
  • Environmental and Cultural Studies in Latin America and Beyond

GEOMAR Helmholtz Centre for Ocean Research Kiel
2015-2024

Radboud University Nijmegen
2022-2024

Kiel University
2021-2024

Universidad de Bogotá Jorge Tadeo Lozano
2008-2016

Abstract. The climate active trace-gas carbonyl sulfide (OCS) is the most abundant sulfur gas in atmosphere. A missing source its atmospheric budget currently suggested, resulting from an upward revision of vegetation sink. Tropical oceanic emissions have been proposed to close gap budget. We present a bottom-up approach including (i) new observations OCS surface waters tropical Atlantic, Pacific and Indian oceans (ii) further improved global box model show that direct are unlikely account...

10.5194/acp-17-385-2017 article EN cc-by Atmospheric chemistry and physics 2017-01-10

1. Abstract Nitrous oxide (N2O) is an important atmospheric trace gas involved in tropospheric warming and stratospheric ozone depletion. Estimates of the global ocean contribution to N2O emissions average 21 % (range: 10 53 %). Ongoing environmental changes such as warming, deoxygenation acidification are affecting oceanic cycling atmosphere. International activities over last decades aimed at improving estimates emissions, including (i) MarinE MethanE NiTrous Oxide database (MEMENTO) for...

10.3389/fmars.2019.00157 article EN cc-by Frontiers in Marine Science 2019-04-02

Abstract. Oxygen-deficient zones (ODZs) are major sites of net natural nitrous oxide (N2O) production and emissions. In order to understand changes in the magnitude N2O response global change, knowledge on individual contributions microbial pathways (nitrification denitrification) their regulation is needed. ODZ coastal area off Peru, sensitivity oxygen organic matter was investigated using 15N tracer experiments combination with quantitative PCR (qPCR) microarray analysis total active...

10.5194/bg-17-2263-2020 article EN cc-by Biogeosciences 2020-04-22

The air–sea exchange and oceanic cycling of greenhouse gases (GHG), including carbon dioxide (CO2), nitrous oxide (N2O), methane (CH4), monoxide (CO), nitrogen oxides (NOx = NO + NO2), are fundamental in controlling the evolution Earth’s atmospheric chemistry climate. Significant advances have been made over last 10 years understanding, instrumentation methods, as well deciphering production consumption pathways GHG upper ocean (including surface subsurface down to approximately 1000 m)....

10.1525/elementa.2023.00044 article EN cc-by Elementa Science of the Anthropocene 2024-01-01

Abstract. A new system for continuous, highly resolved oceanic and atmospheric measurements of N2O, CO CO2 is described. The based upon off-axis integrated cavity output spectroscopy (OA-ICOS) a non-dispersive infrared analyzer (NDIR), both coupled to Weiss-type equilibrator. Performance the combined setup was evaluated by testing its precision, accuracy, long-term stability, linearity response time. Furthermore, tested during two oceanographic campaigns in equatorial Atlantic Ocean order...

10.5194/os-9-1071-2013 article EN cc-by Ocean science 2013-12-11

Abstract. Large-scale climatic forcing is impacting oceanic biogeochemical cycles and expected to influence the water-column distribution of trace gases, including methane nitrous oxide. Our ability as a scientific community evaluate changes in inventories oxide depends largely on our capacity obtain robust accurate concentration measurements that can be validated across different laboratory groups. This study represents first formal international intercomparison whereby participating...

10.5194/bg-15-5891-2018 article EN cc-by Biogeosciences 2018-10-05

Abstract. Depth profiles of nitrous oxide (N2O) were measured during six cruises to the upwelling area and oxygen minimum zone (OMZ) off Peru in 2009 2012/2013, covering both coastal shelf region adjacent open ocean. N2O displayed a strong sensitivity towards concentrations. Open ocean with distances break larger than first baroclinic Rossby radius deformation showed transition from broad maximum close Equator double-peak structure south 5° S where was more pronounced. Maximum concentrations...

10.5194/bg-13-827-2016 article EN cc-by Biogeosciences 2016-02-12

Abstract The Benguela Upwelling System (BUS) is the most productive of all eastern boundary upwelling ecosystems and it hosts a well‐developed oxygen minimum zone. As such, BUS potential hotspot for production N 2 O, potent greenhouse gas derived from microbially driven decay sinking organic matter. Yet, extent at which near‐surface waters emit O to atmosphere in highly uncertain. Here we present first high‐resolution surface measurements across northern part (nBUS). We found strong...

10.1029/2018gl081648 article EN Geophysical Research Letters 2019-02-26

Abstract. For millennia, humans have gravitated towards coastlines for their resource potential and as geopolitical centres global trade. A basic requirement ensuring water security coastal communities relies on a delicate balance between the supply demand of potable water. The interaction freshwater saltwater in settings is, therefore, complicated by both natural human-driven environmental changes at land–sea interface. In particular, ongoing sea-level rise, warming deoxygenation might...

10.5194/bg-20-647-2023 article EN cc-by Biogeosciences 2023-02-10

Abstract. In the current era of rapid climate change, accurate characterization climate-relevant gas dynamics – namely production, consumption, and net emissions is required for all biomes, especially those ecosystems most susceptible to impact change. Marine environments include regions that act as sources or sinks numerous climate-active trace gases including methane (CH4) nitrous oxide (N2O). The temporal spatial distributions CH4 N2O are controlled by interaction complex biogeochemical...

10.5194/bg-17-5809-2020 article EN cc-by Biogeosciences 2020-11-26

Abstract. Recent observations in the eastern tropical South Pacific (ETSP) have shown key role of meso- and submesoscale processes (e.g. eddies) shaping its hydrographic biogeochemical properties. Off Peru, elevated primary production from coastal upwelling combination with sluggish ventilation subsurface waters fuels a prominent oxygen minimum zone (OMZ). Given that nitrous oxide (N2O) production–consumption water column are sensitive to (O2) concentrations, ETSP is region particular...

10.5194/bg-13-1105-2016 article EN cc-by Biogeosciences 2016-02-23

10.1016/j.dsr2.2017.12.023 article EN Deep Sea Research Part II Topical Studies in Oceanography 2018-01-10

Abstract. Carbon monoxide (CO) influences the radiative budget and oxidative capacity of atmosphere over Arctic Ocean, which is a source atmospheric CO. Yet, oceanic CO cycling understudied in this area, particularly light ongoing rapid environmental changes. We present results from incubation experiments conducted Fram Strait August–September 2019 under different conditions: while lower pH did not affect production (GPCO) or consumption (kCO) rates, enhanced GPCO kCO were positively...

10.5194/bg-20-1371-2023 article EN cc-by Biogeosciences 2023-04-12

In order to determine the influence of ocean and atmospheric coupling dynamics on upwelling events, caused by Ekman’s transport continental winds, as well possible fertilization effect produced increasing concentration inorganic nutrients in coastal waters Gaira’s inlet, Magdalena department, during minor dry season 2006, atmospheric, oceanographic, biological variables were measured implementation Eurelian method. A total four samplings carried out, among which two presented oceanic...

10.25268/bimc.invemar.2008.37.2.195 article EN Boletín de Investigaciones Marinas y Costeras 2016-01-01

Abstract. The open ocean is a major source of nitrous oxide (N2O), an atmospheric trace gas attributable to global warming and ozone depletion. Intense sea-to-air N2O fluxes occur in oceanic upwelling regions such as the eastern tropical South Pacific (ETSP). ETSP influenced by El Niño–Southern Oscillation that leads inter-annual variations physical, chemical, biological properties water column. In October 2015, strong Niño event was developing ETSP; we conduct field observations investigate...

10.5194/bg-16-2079-2019 article EN cc-by Biogeosciences 2019-05-17

Human activities are changing the Arctic environment at an unprecedented rate resulting in rapid warming, freshening, sea ice retreat and ocean acidification of Ocean. Trace gases such as nitrous oxide (N2O) methane (CH4) play important roles both atmospheric reactivity radiative budget thus have a high potential to influence region's climate. However, little is known about how these physical chemical changes will impact emissions major climate-relevant trace from The combined consequences...

10.1007/s13280-021-01633-8 article EN cc-by AMBIO 2021-10-10

Abstract Methane (CH 4 ) is a climate‐relevant trace gas that emitted from the open and coastal oceans in considerable amounts. However, its distribution remote oceanic areas largely unknown. To fill this knowledge gap, dissolved CH was measured at nine stations 75°S Ross Sea during austral summer January 2020. undersaturation (mean: 82 ± 20%) found throughout water column. In subsurface waters, of mainly resulted mixing masses situ consumption, whereas concentrations surface mixed layer...

10.1002/lol2.10315 article EN cc-by Limnology and Oceanography Letters 2023-02-09

Abstract The tropical Atlantic exerts a major influence in climate variability through strong air‐sea interactions. Within this region, the eastern side of equatorial band is characterized by seasonality, whereby most prominent feature annual development cold tongue (ACT). This low sea surface temperatures (∼22–23°C) typically associated with upwelling‐driven enhancement nutrient concentrations and primary production. Based on detailed investigation distribution sea‐to‐air fluxes N 2 O...

10.1002/2016jc012238 article EN Journal of Geophysical Research Oceans 2016-11-16

From 2008 to 2019, a comprehensive research project, ‘SFB 754, Climate – Biogeochemistry Interactions in the Tropical Ocean,’ was funded by German Research Foundation investigate climate-biogeochemistry interactions tropical ocean with particular emphasis on processes determining oxygen distribution. During three 4-year long funding phases, consortium of more than 150 scientists conducted or participated 34 major cruises and collected wealth physical, biological, chemical, meteorological...

10.3389/fmars.2021.723304 article EN cc-by Frontiers in Marine Science 2021-09-28

Abstract Upward transport and/or mixing of trace gas‐enriched subsurface waters fosters the exchange nitrous oxide (N 2 O) and methane (CH 4 ) with atmosphere in Eastern‐South Atlantic (ESA). To date, it is, however, unclear whether this source is maintained by local production or advection water masses. The meridional zonal variability N O CH ESA were investigated to identify contributions major regional masses overall budget . maximal sea surface concentrations main upwelling cells...

10.1029/2020jc016878 article EN Journal of Geophysical Research Oceans 2021-10-20
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