@Article{LessCSNVWBDGAKKR:2018:RoHyBi,
author = "Less, Diani F. S. and Cunha, Alan C. and Sawakuchi, Henrique O.
and Neu, Vania and Val{\'e}rio, Aline de Matos and Ward, Nicholas
D. and Brito, Daimio C. and Diniz, Joel E. M. and Gagne-Maynard,
William and Abreu, Carlos M. and Kampel, Milton and Krusche, Alex
V. and Richey, Jeffrey E.",
affiliation = "{Universidade Federal do Oeste do Par{\'a} (UFOPA)} and
{Universidade Federal do Amap{\'a} (UFAP)} and {Universidade de
S{\~a}o Paulo (USP)} and {Universidade Federal Rural da
Amaz{\^o}nia (UFRAM)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Pacific Northwest National Laboratory} and
{Universidade do Estado do Amap{\'a} (UEAP)} and {Universidade
Federal do Amap{\'a} (UFAP)} and {Pacific Northwest National
Laboratory} and {Universidade Federal do Amap{\'a} (UFAP)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidade de S{\~a}o Paulo (USP)} and {University of
Washington}",
title = "The role of hydrodynamic and biogeochemistry on CO2 flux and pCO2
at the Amazon River mouth",
journal = "Biogeosciences Discussions",
year = "2018",
volume = "2018",
number = "465",
month = "Dec.",
abstract = "Recent estimates indicate that the lower Amazon River outgasses
significant amounts of carbon dioxide (CO2) that was not
previously accounted for the global inland water carbon budget.
Detailed evaluation of seasonal variability and 10 controlling
mechanisms behind the CO2 fluxes in this large and complex area
remains incomplete. Previous observations throughout the Amazon
basin showed that higher CO2 fluxes (FCO2) and partial pressure of
CO2 (pCO2) occur during high water and higher wind intensity
seasons. The influence of wind and water speed, depth of water
column, as well as respiration of allochthonous and autochthonous
organic matter, are frequently assigned as the main control
variables. Here, we assess the influence of a set of
biogeochemical and hydrodynamic parameters on the seasonal
variation of FCO2 and 15 pCO2 near the Amazon River mouth. FCO2,
pCO2 and biogeochemical and hydrologic analyses were carried out
from 2010 to 2016 during four different hydrological periods per
year (N=25) in the North Channel of the Amazon River mouth. FCO2
and pCO2 were used as dependent variables and analyzed against 33
biogeochemical, hydrodynamic and meteorological parameters along
the hydrological seasons. The highest FCO2 and pCO2 was obtained
at high discharge season (11.28 ± 7.82 \μmol m- ² s-1 and
(4575 ± 429 \μatm, respectively) when most of these
parameters tend to be higher. Among the 33 parameters 20 analyzed,
the significant correlations with FCO2 and pCO2 (p<0.05) observed
were for water and air temperatures, dissolved oxygen, dissolved
organic carbon, nitrate, dissolved inorganic nitrogen and pH.
These variables could be considered suitable predictors for
estimating pCO2 and FCO2 in the Amazon River mouth area. For a
better estimation and understanding of carbon budgets in tropical
rivers it is still required to verify and to quantify more deeply
the relationship among CO2 evasion and others hydrodynamic,
meteorological and biogeochemical variables.",
doi = "10.5194/bg-2018-465",
url = "http://dx.doi.org/10.5194/bg-2018-465",
issn = "1810-6277",
language = "en",
targetfile = "less-role.pdf",
urlaccessdate = "02 maio 2024"
}