Francis Dube

Francis Dube

orcid

Research Focus & Metrics

Academic Career Length

16Years (2011-Present)

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

Representative Publications

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6 July 2011
Verified
Book Chapter
Closed access
PDF file
FDFrancis Dube
Francis Dube
NTNaresh V. Thevathasan
Naresh V. Thevathasan
EZErick Zagal
Erick Zagal
AGAndrew M. Gordon
Andrew M. Gordon
NSNeal B. Stolpe
Neal B. Stolpe
MEMiguel Espinosa
Miguel Espinosa

13 January 2012 in Agroforestry Systems
Verified
Journal Article
Closed access
PDF file
FDFrancis Dube
Francis Dube
MEMiguel Espinosa
Miguel Espinosa
NSNeal B. Stolpe
Neal B. Stolpe
EZErick Zagal
Erick Zagal
NTNaresh V. Thevathasan
Naresh V. Thevathasan
AGAndrew M. Gordon
Andrew M. Gordon

6 August 2020 in Remote Sensing
Verified
Journal Article
Open access
PDF file
Efrain DuarteEfrain Duarte
Efrain Duarte
JBJuan A. Barrera
Juan A. Barrera
FDFrancis Dube
Francis Dube
FCFabio Casco
Fabio Casco
AHAlexander Hernandez
Alexander Hernandez
EZErick Zagal
Erick Zagal
Current estimates of CO2 emissions from forest degradation are generally based on insufficient information and are characterized by high uncertainty, while a global definition of ‘forest degradation’ is currently being discussed in the scientific arena. This study proposes an automated approach to monitor degradation using a Landsat time series. The methodology was developed using the Google Earth Engine (GEE) and applied in a pine forest area of the Dominican Republic. Land cover change mapping was conducted using the random forest (RF) algorithm and resulted in a cumulative overall accuracy of 92.8%. Forest degradation was mapped with a 70.7% user accuracy and a 91.3% producer accuracy. Estimates of the degraded area had a margin of error of 10.8%. A number of 344 Landsat collections, corresponding to the period from 1990 to 2018, were used in the analysis. Additionally, 51 sample plots from a forest inventory were used. The carbon stocks and emissions from forest degradation were estimated using the RF algorithm with an R2 of 0.78. GEE proved to be an appropriate tool to monitor the degradation of tropical forests, and the methodology developed herein is a robust, reliable, and replicable tool that could be used to estimate forest degradation and improve monitoring, reporting, and verification (MRV) systems under the reducing emissions from deforestation and forest degradation (REDD+) mechanism.

22 August 2020 in Sustainability
Verified
Journal Article
Open access
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JOJuan Ortiz
Juan Ortiz
FDFrancis Dube
Francis Dube
PVPablo Neira Vidal
Pablo Neira Vidal
MPMarcelo Panichini
Marcelo Panichini
NSNeal Stolpe
Neal Stolpe
PMPedro A. Martínez-Hernández
Pedro A. Martínez-Hernández
In Chile, 49.1% of the national territory is affected by soil degradation (including erosion and loss of soil organic matter), whereby of the 51.7 Mha that have been historically associated with agricultural-livestock and forestry activities, only 35.5 Mha are being used at the present. Consequently, soil degradation has resulted in the release of about 11.8 Gg yr−1 of carbon (C) equivalent (CO2eq) to the atmosphere. Silvopastoral systems (SPS), however, can increase soil organic C (SOC) through sequestration (C→SOC), improve ecosystem services, and have been internationally recommended for sustainable land use. Therefore, it was proposed to determine the effects of SPS on soils, over five years, in degraded sites that were located in the Ranchillo Alto (SPS-RA) (37°04′52″ S, 71°39′14″ W), Ñuble region. The sites were rated according to previous canopy disturbance levels (+) as follows: open (Op)+++, semi open (SOp)++, and semi closed (SC)+. The analysis was performed on different physical and chemical soil properties (0–5 and 5–20 cm depths), that were expressed as soil indicators (SIND) for chemical and physical properties, which were used to calculate a soil quality (SQ) index (SQI). The results indicated overall SQI values of 37.6 (SC) > 29.8 (Op) > 28.8 (SOp), but there were no significant variations (p < 0.05) in physical SQ, whereas chemical SQ varied in all conditions, mostly at 0–5 cm in Op and SOp. Increases of SOC were also observed (2015–2018 period) of 22.5, 14.5, and 4.8 Mg ha−1 for SOp, Op, and SC, respectively, showing that SPS promote the reclamation of Ranchillo Alto soils.

31 October 2012 in Agroforestry Systems
Verified
Journal Article
Closed access
PDF file
FDFrancis Dube
Francis Dube
NTNaresh V. Thevathasan
Naresh V. Thevathasan
NSNeal B. Stolpe
Neal B. Stolpe
EZErick Zagal
Erick Zagal
AGAndrew M. Gordon
Andrew M. Gordon
KSKatia Sáez
Katia Sáez

3 March 2016
Verified
Book Chapter
Closed access
PDF file
FDFrancis Dube
Francis Dube
ASAlvaro Sotomayor
Alvaro Sotomayor
VLVeronica Loewe
Veronica Loewe
BMBurkhard Müller-Using
Burkhard Müller-Using
NSNeal Stolpe
Neal Stolpe
MDMarcelo Doussoulin
Marcelo Doussoulin