Comparison of change detection techniques for the Yucatan peninsula using Landsat image time series

Author(s):  
Rene R. Colditz ◽  
Ricardo M. Llamas ◽  
Steffen Gebhardt ◽  
Thilo Wehrmann ◽  
Julian Equihua
2018 ◽  
Vol 11 ◽  
pp. 117862211775160 ◽  
Author(s):  
Gebiaw T Ayele ◽  
Aschalew K Tebeje ◽  
Solomon S Demissie ◽  
Mulugeta A Belete ◽  
Mengistu A Jemberrie ◽  
...  

Land use planners require up-to-date and spatially accurate time series land resources information and changing pattern for future management. As a result, assessing the status of land cover change due to population growth and arable expansion, land degradation and poor resource management, partial implementation of policy strategies, and poorly planned infrastructural development is essential. Thus, the objective of the study was to quantify the spatiotemporal dynamics of land use land cover change between 1995 and 2014 using 5 multi-temporal cloud-free Landsat Thematic Mapper images. The maximum likelihood (ML)-supervised classification technique was applied to create signature classes for significant land cover categories using means and variances of the training data to estimate the probability that a pixel is a member of a class. The final Bayesian ML classification resulted in 12 major land cover units, and the spatiotemporal change was quantified using post-classification and statistical change detection techniques. For a period of 20 years, there was a continuously increasing demand for arable areas, which can be represented by an exponential growth model. Excepting the year 2009, the built-up area has shown a steady increase due to population growth and its need for infrastructure development. There was nearly a constant trend for water bodies with a change in slope significantly less than +0.01%. The 2014 land cover change statistics revealed that the area was mainly covered by cultivated, wood, bush, shrub, grass, and forest land mapping units accounting nearly 63%, 12%, 8%, 6%, 4%, and 2% of the total, respectively. Land cover change with agro-climatic zones, soil types, and slope classes was common in most part of the area and the conversion of grazing land into plantation trees and closure area development were major changes in the past 20 years.


2013 ◽  
Vol 2013 ◽  
pp. 1-10 ◽  
Author(s):  
Constantinos S. Hilas ◽  
Ioannis T. Rekanos ◽  
Paris Ast. Mastorocostas

Changes in the level of a time series are usually attributed to an intervention that affects its temporal evolution. The resulting time series are referred to as interrupted time series and may be used to identify the events that caused the intervention and to quantify their impact. In the present paper, a heuristic method for level change detection in time series is presented. The method uses higher-order statistics, namely, the skewness and the kurtosis, and can identify both the existence of a change in the level of the time series and the time instance when it has happened. The technique is straightforwardly applicable to the detection of outliers in time series and promises to have several applications. The method is tested with both simulated and real-world data and is compared to other popular change detection techniques.


2011 ◽  
Vol 3 (5) ◽  
pp. 433-442 ◽  
Author(s):  
Neeti Neeti ◽  
John Rogan ◽  
Zachary Christman ◽  
J. Ronald Eastman ◽  
Marco Millones ◽  
...  

2019 ◽  
Author(s):  
Stephanie C. Hunter ◽  
Diana M. Allen ◽  
Karen E. Kohfeld

Abstract. The Terminal Classic Period (TCP, 800–1000 A.D.) coincides with the collapse of the Maya Civilization on the Yucatan Peninsula, a period of rapid population decline that has been attributed to extended and widespread droughts. This study uses multiple proxy records from the Yucatan Peninsula to collectively analyze drought occurrence across the region during this time. We use a changepoint analysis to identify periods of significant changes in the statistical properties (mean and variance) of 23 proxy records and classify evidence of drought based on four criteria: (1) a changepoint in mean and variance during the TCP, (2) a change towards more arid conditions during the TCP, (3) a change greater than 20 % from the time-series mean, and (4) having a mean during the TCP that is significantly different from the time-series mean. Our analysis shows that five records met all inclusion criteria for showing definitive evidence of drought during the TCP, and these are located in the northwest, northeast, and north-central regions of the Yucatan Peninsula. Many of these records showed some evidence of drought (meeting some but not all criteria), but some showed evidence of drought occurring earlier than the TCP (in the northeast of the Yucatan Peninsula) and later than the TCP (in the south of the Yucatan Peninsula). We also conducted a changepoint analysis on reconstructions of three modes of climate variability known to affect the movement of the Intertropical Convergence Zone (ITCZ). Our comparison suggests that during the first half of the TCP, the Pacific Decadal Oscillation (PDO), El Niño Southern Oscillation (ENSO), and Atlantic Multidecadal Oscillation (AMO) were all in positive phase, which may have pushed the ITCZ southward during the winter months and enhanced aridity during the dry season. However, our analysis suggests that the position of the ITCZ was not the sole driver of the TCP droughts, as these conditions existed over the Yucatan Peninsula prior to the TCP as well. This study highlights the complexity of the spatial and temporal variability of these droughts, and points to the need for further study to identify the mechanisms responsible for the TCP droughts.


Author(s):  
J. Chen ◽  
J. Chen ◽  
J. Zhang

Global, timely, accurate and cost-effective cropland monitoring with a fine spatial resolution will dramatically improve our understanding of the effects of agriculture on greenhouse gases emissions, food safety, and human health. Time-series remote sensing imagery have been shown particularly potential to describe land cover dynamics. The traditional change detection techniques are often not capable of detecting land cover changes within time series that are severely influenced by seasonal difference, which are more likely to generate pseuso changes. Here,we introduced and tested LTSM ( Landsat time-series stacks model), an improved Continuous Change Detection and Classification (CCDC) proposed previously approach to extract spectral trajectories of land surface change using a dense Landsat time-series stacks (LTS). The method is expected to eliminate pseudo changes caused by phenology driven by seasonal patterns. The main idea of the method is that using all available Landsat 8 images within a year, LTSM consisting of two term harmonic function are estimated iteratively for each pixel in each spectral band .LTSM can defines change area by differencing the predicted and observed Landsat images. The LTSM approach was compared with change vector analysis (CVA) method. The results indicated that the LTSM method correctly detected the “true change” without overestimating the “false” one, while CVA pointed out “true change” pixels with a large number of “false changes”. The detection of change areas achieved an overall accuracy of 92.37 %, with a kappa coefficient of 0.676.


2018 ◽  
Vol 130 (1) ◽  
pp. 45-50 ◽  
Author(s):  
S Guillén-Hernández ◽  
C González-Salas ◽  
D Pech-Puch ◽  
H Villegas-Hernández

2019 ◽  
Author(s):  
Jonathan B. Martin ◽  
◽  
Andrea J. Pain ◽  
Caitlin Young ◽  
Arnoldo Valle-Levinson

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