Padrões de evapotranspiração em área de cerrado para cenários de aquecimento com simulações do modelo SiB2

Trabalho publicado em: Ciência e Natura, Santa Maria, v. esp., p. 147-149, dez. 2013

Water and energy fluxes from a woodland savanna (cerrado) in southeast Brazil

Study region: The area of woodland savanna (cerrado) is located in southeast Brazil (21°36′ to 44′ S, 47°34′ to 41′ W). Study focus: The cerrado sensu-stricto savanna evapotranspiration was observed using the eddy-covariance method over three years. New hydrological insights for the region: The first year total rainfall (R = 1664 mm) was 11% above the long-term rainfall (1498 mm) and the total evapotranspiration (ET = 1242 mm) and water equivalent of available energy (Av = 1835 mm) were approximately 4% and 2% greater, respectively, than in the second year when the rainfall total was 5% lower than the long-term average. In the third year despite the total rainfall (1259 mm) being 24% lower than the first year and 16% lower than the average, the totals of ET (1242 mm) and Av (1815 mm) were approximately the same. The small variation in the observed annual ET totals shows that in this cerrado vegetation the deep soil moisture content supports the ET in a dry year and the water available for recharging the soil profile and groundwater (∼R − ET) was dominated by the rainfall amount being significantly greater in the wet year (422 mm) than in the dry year (13 mm)

Fluxos de Superfície em Topografia Complexa

Fluxos de superfície em topografia complex

Variabilidade das Medidas de Fluxos de Co2 do Solo obtidas pelo Método da Correlação de Vórtices

Variabilidade das medidas de fluxos de CO2 do solo obtidaspelo método da correlação de vórtice

Comparação da Radiação Solar Global Incidente Obtida por Diferentes Fontes de Dados para o Norte de SP

O objetivo deste trabalho foi comparar os dados de radiaçãosolar global incidente de três torres micrometeorológicas localizados naregião norte do estado de São Paulo, com os dados disponíveis de outrasfontes: estações meteorológicas de superfície mais próximas e estimativasa partir de satélites (modelo GL1.2). A regressão linear entre as estimativasde radiação do modelo GL1.2 com as observações na área decerrado indicou um ajuste melhor do que o obtido com a estaçãometeorológica mais próxima. Esses resultados sugerem que as estimativasde radiação do modelo GL1.2 podem ser usadas para o preenchimentode falhas de Ki medida nas torres micrometeorológicas e potencialmentecomo forçante em esquemas de superfície e modelos hidrológicosaplicados a bacias hidrográficas da região

Calibração do Módulo de Transferência Turbulenta do Modelo sib2 para Floresta Tropical Amazônica

Calibração do módulo de transferência turbulenta domodelo SiB2 para Floresta Tropical Amazônic

Avaliação do Método de Multiple Imputation no Preenchimento de Falhas de Fluxos de Energia sobre uma Área de Cana-de-Açúcar

Avaliação do método de Multiple Imputation nopreenchimento de falhas de fluxos de energia sobre umaárea de cana-de-açúca

Global transpiration data from sap flow measurements : the SAPFLUXNET database

Plant transpiration links physiological responses of vegetation to water supply and demand with hydrological, energy, and carbon budgets at the land-atmosphere interface. However, despite being the main land evaporative flux at the global scale, transpiration and its response to environmental drivers are currently not well constrained by observations. Here we introduce the first global compilation of whole-plant transpiration data from sap flow measurements (SAPFLUXNET, https://sapfluxnet.creaf.cat/, last access: 8 June 2021). We harmonized and quality-controlled individual datasets supplied by contributors worldwide in a semi-automatic data workflow implemented in the R programming language. Datasets include sub-daily time series of sap flow and hydrometeorological drivers for one or more growing seasons, as well as metadata on the stand characteristics, plant attributes, and technical details of the measurements. SAPFLUXNET contains 202 globally distributed datasets with sap flow time series for 2714 plants, mostly trees, of 174 species. SAPFLUXNET has a broad bioclimatic coverage, with woodland/shrubland and temperate forest biomes especially well represented (80 % of the datasets). The measurements cover a wide variety of stand structural characteristics and plant sizes. The datasets encompass the period between 1995 and 2018, with 50 % of the datasets being at least 3 years long. Accompanying radiation and vapour pressure deficit data are available for most of the datasets, while on-site soil water content is available for 56 % of the datasets. Many datasets contain data for species that make up 90 % or more of the total stand basal area, allowing the estimation of stand transpiration in diverse ecological settings. SAPFLUXNET adds to existing plant trait datasets, ecosystem flux networks, and remote sensing products to help increase our understanding of plant water use, plant responses to drought, and ecohydrological processes. SAPFLUXNET version 0.1.5 is freely available from the Zenodo repository (https://doi.org/10.5281/zenodo.3971689; Poyatos et al., 2020a). The "sapfluxnetr" R package - designed to access, visualize, and process SAPFLUXNET data - is available from CRAN.Peer reviewe

Measurements of CO2 exchange over a woodland savanna (Cerrado Sensu stricto) in southeast Brasil

The technique of eddy correlation was used to measure the net ecosystem exchange over a woodland savanna (Cerrado Sensu stricto) site (Gleba Pé de Gigante) in southeast Brazil. The data set included measurements of climatological variables and soil respiration using static soil chambers. Data were collected during the period from 10 October 2000 to 30 March 2002. Measured soil respiration showed average values of 4.8 molCO2 m-2s-1 year round. Its seasonal differences varied from 2 to 8 molCO2 m-2s-1 (Q10 = 4.9) during the dry (April to August) and wet season, respectively, and was concurrent with soil temperature and moisture variability. The net ecosystem CO2 flux (NEE) variability is controlled by solar radiation, temperature and air humidity on diel course. Seasonally, soil moisture plays a strong role by inducing litterfall, reducing canopy photosynthetic activity and soil respiration. The net sign of NEE is negative (sink) in the wet season and early dry season, with rates around -25 kgC ha-1day-1, and values as low as 40 kgC ha-1day-1. NEE was positive (source) during most of the dry season, and changed into negative at the onset of rainy season. At critical times of soil moisture stress during the late dry season, the ecosystem experienced photosynthesis during daytime, although the net sign is positive (emission). Concurrent with dry season, the values appeared progressively positive from 5 to as much as 50 kgC ha-1day-1. The annual NEE sum appeared to be nearly in balance, or more exactly a small sink, equal to 0.1 0.3 tC ha-1yr-1, which we regard possibly as a realistic one, giving the constraining conditions imposed to the turbulent flux calculation, and favourable hypothesis of succession stages, climatic variability and CO2 fertilization

The influence of advective transports in the net ecosystem CO2 exchange: a case study for the Atlantic forest using micrometeorological techniques

Para este trabalho, foram realizadas observações de variáveis climáticas e medidas de fluxo de carbono, durante o período de 2008 a 2010, sobre uma floresta de mata atlântica, buscando estimar o balanço de carbono neste sítio experimental, com o objetivo de melhor compreender as trocas de CO2 entre esta floresta e a atmosfera. Para tanto, foram utilizadas técnicas micrometeorológicas de vórtices turbulentos associadas a medidas de transportes advectivos. Este estudo investigou uma área de características singulares, de intensos gradientes topográficos, na cidade de São Luiz do Paraitinga, estado de São Paulo, região sudeste do Brasil. Com vegetação de dossel irregular e circundada por encostas íngremes de até 30º (em distâncias de 50 metros), uma torre micrometeorológica com 60 m de altura foi instalada ao final de 2007. Em 2010, em uma segunda etapa do estudo, foi finalizado o sistema para medidas de fluxos advectivos composto por outras quatro torres de 27 m de modo a definir um volume de controle em uma das encostas próxima à torre micrometeorológica, assim como sugere a técnica utilizada ao considerar os transportes advectivos na equação da conservação de massa, o que caracteriza uma abordagem mais criteriosa em função do relevo. As análises mostraram que estes transportes 1. atuam na alteração da concentração de CO2, tanto na vertical como na horizontal; 2. apresentam ciclos diários e 3. estão bem correlacionados com o armazenamento vertical de CO2, elemento participante na determinação da produtividade primária líquida de uma vegetação monitorada com a técnica comumente utilizada. Considerados os erros inerentes nas estimativas, ao final de três anos de estudo, esta floresta de mata atlântica mostrou comportar-se como uma modesta fonte de CO2, podendo ainda atuar de forma neutra, mesmo tendo acumulados anuais estimados da forma tradicionalmente encontrada na literatura. Estes resultados concordam com outros obtidos em trabalhos independentes de igual teor científico realizados nesta mesma área investigada. Dessa forma, a exclusão dos transportes advectivos não penalizou o balanço de massa; considerá-los causaria maior incerteza nas somas anuais em função do período de dados disponível e da complexidade da sua determinação, como já discutido em outros trabalhos encontrados na literatura.For this study, observations of climate variables and measurements of carbon fluxes have been done between the years 2008 and 2010 above a brazilian Atlantic forest, aiming to estimate the carbon balance in this experimental site, in order to better understand the exchanges of CO2 between this forest and the atmosphere. To carry it out, micrometeorological eddy covariance technique was associated with advective transport measurements. This study investigated an specific area with intense topographic gradients located in São Luiz do Paraitinga city, São Paulo state, southeastern Brazil. Surrounded by vegetation with irregular canopy and steep slopes of up to 30° (at distances of 50 meters), a micrometeorological tower 60 m height was installed at the end of 2007. In 2010, the installation has been finished with four towers of 27 m height in order to define a control volume over one of the slopes near the micrometeorological tower, for measurements of advective flows as suggests the technique when advective transports are considered, from equation of mass conservation, which features a more careful approach regarding the relief conditions. The analysis showed that these transports 1. act on changes in CO2 concentration, both vertically and horizontally; 2. show daily cycles and 3. are well correlated with the vertical CO2 storage, a key participant element in determining the net primary productivity of vegetation when monitored by the technique as it is commonly applied. Considering the inherent estimated errors, at the end of three years of study, this forest was a modest source of CO2, and may also acts in a neutral way, even with annual estimated sums obtained as traditionally found in the literature. These results agree with those found through independent studies with considerable scientific content developed in the same investigated area. Thus, the exclusion of advective transport did not penalize the mass balance; consider them could cause greater uncertainty in annual amounts based on the available dataset and the complexity for its determination, as discussed in other works in the literature