2014
DOI: 10.1080/02723646.2014.898126
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Spatial persistence and temporal patterns in vegetation cover across Florida, 1982–2006

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Cited by 12 publications
(13 citation statements)
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“…An increase in late autumn and winter NDVI was found by Tsai et al . () in the state of Florida over the period 1982–2006 and was suggested to be caused by changes in the Atlantic multi‐decadal oscillation (AMO), which switched from a cold to a warm phase after 1995 and is associated with increased winter precipitation.…”
Section: Discussionmentioning
confidence: 99%
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“…An increase in late autumn and winter NDVI was found by Tsai et al . () in the state of Florida over the period 1982–2006 and was suggested to be caused by changes in the Atlantic multi‐decadal oscillation (AMO), which switched from a cold to a warm phase after 1995 and is associated with increased winter precipitation.…”
Section: Discussionmentioning
confidence: 99%
“…Therefore, the relationship between winter greening and changes in LULCC in central and south-eastern USA based on FAO statistics is inconclusive. An increase in late autumn and winter NDVI was found by Tsai et al (2014) in the state of Florida over the period and was suggested to be caused by changes in the Atlantic multi-decadal oscillation (AMO), which switched from a cold to a warm phase after 1995 and is associated with increased winter precipitation.…”
Section: Diverging Trends and Changes In Agricultural Practicementioning
confidence: 99%
“…Specifically, we utilize a measure called directional persistence, which indicates the overall direction of landscape change (increasing/decreasing) relative to a fixed benchmark condition (which could be tied to a climatic event, policy change, etc.) on a per pixel basis [45][46][47]. This metric is based on the principal of the random walk process, such that at any point in time, the likelihood of an increase versus a decrease in a value is identical (i.e., 0.5 probability) as this is a Bernouli random process.…”
Section: Remote Sensingmentioning
confidence: 99%
“…Theoretically, as NDVI is a continuous variable bounded by −1 and +1, identical values of NDVI are impossible. Predetermined critical levels of statistical significance, based on a random walk statistic, highlight the nature and extent of changes across the landscape beyond which might be expected at random and which are possibly indicative of degradation or other changes (see [45][46][47] for more details). The directional persistence (D j ) in this case yields a maximum range of −23 to +23 with the critical value of (α = 0.025) ±11 [45].…”
Section: Remote Sensingmentioning
confidence: 99%
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