Search results for "RAIN-FOREST"

showing 4 items of 4 documents

HONO Emissions from Soil Bacteria as a Major Source of Atmospheric Reactive Nitrogen

2013

From Soil to Sky Trace gases emitted either through the activity of microbial communities or from abiotic reactions in the soil influence atmospheric chemistry. In laboratory column experiments using several soil types, Oswald et al. (p. 1233 ) showed that soils from arid regions and farmlands can produce substantial quantities of nitric oxide (NO) and nitrous acid (HONO). Ammonia-oxidizing bacteria are the primary source of HONO at comparable levels to NO, thus serving as an important source of reactive nitrogen to the atmosphere.

Biogeochemical cycle010504 meteorology & atmospheric sciencesReactive nitrogenNitrogenNitrosomonas europaeaNitrous Acid010501 environmental sciencesNO EMISSIONSNITRIFICATION01 natural sciencescomplex mixturesWATER CONTENTchemistry.chemical_compoundAmmoniaDEPENDENCENitrogen FixationEMPIRICAL-MODELNitriteNitrogen cycleTEMPERATURESoil Microbiology0105 earth and related environmental sciences[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]Nitrous acidMultidisciplinaryNITRIC-OXIDEAtmosphereChemistryDENITRIFICATIONRAIN-FORESTReactive Nitrogen SpeciesSOUTH-AFRICA13. Climate actionEnvironmental chemistrySoil waterNitrogen fixationOxidation-ReductionSoil microbiology
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Seasonal and Inter-annual Variation of Evapotranspiration in Amazonia Based on Precipitation, River Discharge and Gravity Anomaly Data

2019

We analyzed seasonal and spatial variations of evapotranspiration (ET) for five Amazon sub-basins and their response to the 2015/16 El Nino episode using a recently developed water-budget approach. ET varied typically between similar to 7 and 10 cm/month with exception of the Xingu basin for which it varied between 10 and 15 cm/month. Outstanding features of ET seasonality are (i) generally weak seasonality, (ii) two ET peaks for the two very wet catchments Solimoes and Negro, with one occurring during the wet season and one during the drier season, and (iii) a steady increase of ET during the second half of the dry season for the three drier catchments (Madeira, Tapajos, Xingu). Peak ET oc…

Wet season1171 Geosciences010504 meteorology & atmospheric sciences010502 geochemistry & geophysicsAtmospheric sciences01 natural sciencesGravity anomalyCARBONSolar induced fluorescenceAmazoniaGRACEEvapotranspirationDry seasonmedicinePrecipitationEl NiñoFLUORESCENCElcsh:ScienceSATELLITE0105 earth and related environmental sciencesBASINForest ProductivityEvapotranspirationAmazon rainforestDischargePHOTOSYNTHESISSENSORRAIN-FOREST15. Life on landSeasonalitymedicine.diseaseBRAZILVARIABILITY13. Climate actionGeneral Earth and Planetary SciencesEnvironmental sciencelcsh:QEl Nino
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The summertime Boreal forest field measurement intensive (HUMPPA-COPEC-2010): an overview of meteorological and chemical influences

2011

This paper describes the background, instrumentation, goals, and the regional influences on the HUMPPACOPEC intensive field measurement campaign, conducted at the Boreal forest research station SMEAR II (Station for Measuring Ecosystem-Atmosphere Relation) in Hyyti¨al¨a, Finland from 12 July–12 August 2010. The prevailing meteorological conditions during the campaign are examined and contrasted with those of the past six years. Back trajectory analyses show that meteorological conditions at the site in 2010 were characterized by a higher proportion of southerly flow than in the other years studied. As a result the summer of 2010 was anomalously warm and high in ozone making the campaign rel…

Meteorologie en Luchtkwaliteitacid-water nucleationscots pineWIMEKMeteorology and Air Qualityatmospheric particlesboundary-layervolatile organic-compoundsEarth System Sciencegas chromatography/mass spectrometrytropical rain-forestsulfuric-acidphase microextractionLeerstoelgroep Aardsysteemkundenatural aerosol
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Impact of Manaus City on the Amazon Green Ocean atmosphere: Ozone production, precursor sensitivity and aerosol load

2010

As a contribution to the Large-Scale Biosphere-Atmosphere Experiment in Amazonia – Cooperative LBA Airborne Regional Experiment (LBA-CLAIRE-2001) field campaign in the heart of the Amazon Basin, we analyzed the temporal and spatial dynamics of the urban plume of Manaus City during the wet-to-dry season transition period in July 2001. During the flights, we performed vertical stacks of crosswind transects in the urban outflow downwind of Manaus City, measuring a comprehensive set of trace constituents including O3, NO, NO2, CO, VOC, CO2, and H2O. Aerosol loads were characterized by concentrations of total aerosol number (CN) and cloud condensation nuclei (CCN), and by light scattering proper…

biomass-burning emissionstropospheric ozonecloud condensation nucleirain-foresttrace gas exchangesWIMEKdry seasonLeerstoelgroep Aardsysteemkundephysical-propertiestropical south-atlanticsecondary organic aerosolEarth System Sciencepower-plant plumes
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