Maria Uilhiana Gomes de Andrade

Prof. Maria Uilhiana Gomes de Andrade


Research Focus & Metrics

Academic Career Length

5Years (2022-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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15 August 2022 in Remote Sensing
Verified
Journal Article
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GABRIEL BRITO COSTAGABRIEL BRITO COSTA
GABRIEL BRITO COSTA
KMKeila Mendes
Keila Mendes
LVLosany Branches Viana
Losany Branches Viana
GAGabriele Vieira Almeida
Gabriele Vieira Almeida
Pedro MuttiPedro Mutti
Pedro Mutti
RMRomulo Simoes Cezar Menezes
Romulo Simoes Cezar Menezes
The Caatinga dry forest encompasses 11% of the total continental territory of Brazil. Nevertheless, most research on the relationship between phenology and ecosystem productivity of Brazilian tropical forests is aimed at the Amazon basin. Thus, in this study we evaluated the seasonality of ecosystem productivity (gross primary production—GPP) in a preserved Caatinga environment in northeast Brazil. Analyses were carried out using eddy covariance measurements and satellite-derived data from sensor MODIS (MODerate Resolution Imaging Spectroradiometer, MOD17 and MOD13 products). In addition to GPP, we investigated water use efficiency (WUE) and meteorological and phenological aspects through remotely sensed vegetation indices (NDVI and EVI). We verified that ecosystem productivity is limited mainly by evapotranspiration, with maximum GPP values registered in the wetter months, indicating a strong dependency on water availability. NDVI and EVI were positively associated with GPP (r = 0.69 and 0.81, respectively), suggesting a coupling between the emergence of new leaves and the phenology of local photosynthetic capacity. WUE, on the other hand, was strongly controlled by consecutive dry days and not necessarily by total precipitation amount. The vegetation indices adequately described interannual variations of the forest response to environmental factors, and GPP MODIS presented a good relationship with tower-measured GPP in dry (R2 = 0.76) and wet (R2 = 0.62) periods.

6 July 2022 in Remote Sensing
Verified
Journal Article
Open access
PDF file
GABRIEL BRITO COSTAGABRIEL BRITO COSTA
GABRIEL BRITO COSTA
Cláudio Moisés Santos e SilvaCláudio Moisés Santos e Silva
Cláudio Moisés Santos e Silva
KMKeila Mendes
Keila Mendes
JSJosé Guilherme GUILHERME MARTINS Dos Santos
José Guilherme GUILHERME MARTINS Dos Santos
TNTheomar Trindade de Araújo Tiburtino Neves
Theomar Trindade de Araújo Tiburtino Neves
MAMaria Uilhiana Gomes de Andrade
Maria Uilhiana Gomes de Andrade
The analysis of gross primary production (GPP) is crucial to better understand CO2 exchanges between terrestrial ecosystems and the atmosphere, while the quantification of water-use efficiency (WUE) allows for the estimation of the compensation between carbon gained and water lost by the ecosystem. Understanding these dynamics is essential to better comprehend the responses of environments to ongoing climatic changes. The objective of the present study was to analyze, through AMERIFLUX and LBA network measurements, the variability of GPP and WUE in four distinct tropical biomes in Brazil: Pantanal, Amazonia, Caatinga and Cerrado (savanna). Furthermore, data measured by eddy covariance systems were used to assess remotely sensed GPP products (MOD17). We found a distinct seasonality of meteorological variables and energy fluxes with different latent heat controls regarding available energy in each site. Remotely sensed GPP was satisfactorily related with observed data, despite weak correlations in interannual estimates and consistent overestimations and underestimations during certain months. WUE was strongly dependent on water availability, with values of 0.95 gC kg−1 H2O (5.79 gC kg−1 H2O) in the wetter (drier) sites. These values reveal new thresholds that had not been previously reported in the literature. Our findings have crucial implications for ecosystem management and the design of climate policies regarding the conservation of tropical biomes, since WUE is expected to change in the ongoing climate change scenario that indicates an increase in frequency and severity of dry periods.