A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
A Look at Amazon Basin Seasonal Dynamics with the Biophysical ... A Look at Amazon Basin Seasonal Dynamics with the Biophysical ...
Soil Temperature and Moisture Variability, Beneath Forest, Pasture and MangroveAreas, in Eastern AmazoniaJosé Ricardo S. de Souza, Julia C. P. Cohen, Antônio C.L. da Costa, Zilurdes F. LopesDepartment of MeteorologyFederal University of Pará, Belém, Brazile-mail : jricardo@ufpa.brABSTRACTSoil temperatures down to 50 cm depth, and volumetric moisture content within theupper 30 cm layer of soils, were measured with similar thermistor sonde and soil moisturereflectometer probe sensor systems, beneath natural forest (Caxiuanã), pasture (Soure) andmangrove (Bragança) areas, in Eastern Amazônia. The sites were selected along a 500 kmtransect, parallel to the equador, between latitudes of 0 and 2 degrees south.The climatic regimes at all three monitoring sites were quite similar and regulatedby the passage of the ITCZ over the equator, which determines the transition between theirdrier and rainy seasons. The soils temperature and moisture levels and variability, beforeand after the onset of the rainy season, were analysed considering the observed short waveincident solar radiation flux and pluviommetric precipitation, at each site.At the depths studied, the soil temperatures in general decreased in the sequence :pasture, mangrove and forest. On the other hand, the soil moisture beneath the forest washigh throughout the dry season.The soils vegetation coverage was found to be, the principal agent responsible forthe wide range of soil temperatures variability found among the studied sites.The waterstorage recharging beneath the pasture was intense and abrupt, just after the onset of therainy season. A smooth soil moisture transition was observed beneath the forest.Corresponding author address : Dr. José Ricardo S. de SOUZA.Departamento de Meteorologia - Centro de Geociências- UFPACP. 1611 , Belém Pará Brasil CEP 66075-900.
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Soil Temper<strong>at</strong>ure and Moisture Variability, Bene<strong>at</strong>h Forest, Pasture and MangroveAreas, in Eastern <strong>Amazon</strong>iaJosé Ricardo S. de Souza, Julia C. P. Cohen, Antônio C.L. da Costa, Zilurdes F. LopesDepartment of MeteorologyFederal University of Pará, Belém, Brazile-mail : jricardo@ufpa.brABSTRACTSoil temper<strong>at</strong>ures down to 50 cm depth, and volumetric moisture content <strong>with</strong>in <strong>the</strong>upper 30 cm layer of soils, were measured <strong>with</strong> similar <strong>the</strong>rmistor sonde and soil moisturereflectometer probe sensor systems, bene<strong>at</strong>h n<strong>at</strong>ural forest (Caxiuanã), pasture (Soure) andmangrove (Bragança) areas, in Eastern Amazônia. The sites were selected along a 500 kmtransect, parallel to <strong>the</strong> equador, between l<strong>at</strong>itudes of 0 and 2 degrees south.The clim<strong>at</strong>ic regimes <strong>at</strong> all three monitoring sites were quite similar and regul<strong>at</strong>edby <strong>the</strong> passage of <strong>the</strong> ITCZ over <strong>the</strong> equ<strong>at</strong>or, which determines <strong>the</strong> transition between <strong>the</strong>irdrier and rainy seasons. The soils temper<strong>at</strong>ure and moisture levels and variability, beforeand after <strong>the</strong> onset of <strong>the</strong> rainy season, were analysed considering <strong>the</strong> observed short waveincident solar radi<strong>at</strong>ion flux and pluviommetric precipit<strong>at</strong>ion, <strong>at</strong> each site.At <strong>the</strong> depths studied, <strong>the</strong> soil temper<strong>at</strong>ures in general decreased in <strong>the</strong> sequence :pasture, mangrove and forest. On <strong>the</strong> o<strong>the</strong>r hand, <strong>the</strong> soil moisture bene<strong>at</strong>h <strong>the</strong> forest washigh throughout <strong>the</strong> dry season.The soils veget<strong>at</strong>ion coverage was found to be, <strong>the</strong> principal agent responsible for<strong>the</strong> wide range of soil temper<strong>at</strong>ures variability found among <strong>the</strong> studied sites.The w<strong>at</strong>erstorage recharging bene<strong>at</strong>h <strong>the</strong> pasture was intense and abrupt, just after <strong>the</strong> onset of <strong>the</strong>rainy season. A smooth soil moisture transition was observed bene<strong>at</strong>h <strong>the</strong> forest.Corresponding author address : Dr. José Ricardo S. de SOUZA.Departamento de Meteorologia - Centro de Geociências- UFPACP. 1611 , Belém Pará Brasil CEP 66075-900.