2018
DOI: 10.1002/ecs2.2451
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A long‐term perspective on microclimate and spring plant phenology in the Western Cascades

Abstract: Phenology-recurring seasonal events in an organism's life cycle-is largely driven by local climates <1 km 2 (microclimates), and changes in phenology are frequently used to indicate a species' or community response to climate change. Phenological shifts can result in trophic asynchrony, population declines of higher-level consumers, and reduction of plant fitness. While timing of phenological events is often correlated with elevation, studies have shown that microclimates created by areas of heterogeneous topo… Show more

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Cited by 26 publications
(24 citation statements)
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“…Our data show that such climatic differences, and the associated very similar changes in phenology, can also occur on much smaller scales. However, microclimatic patterns can differ substantially from regional climate patterns (Hwang et al, 2011;Ward et al, 2018), and we therefore need to take them into account when projecting effects of climate change on phenology (De Frenne et al, 2013;Franklin et al 2013). Especially in forests, these microclimate dynamics have a stronger impact than macroclimate warming on plant responses to climate change (Zellweger et al 2020).…”
Section: Impact Of Microclimate On Phenologymentioning
confidence: 99%
“…Our data show that such climatic differences, and the associated very similar changes in phenology, can also occur on much smaller scales. However, microclimatic patterns can differ substantially from regional climate patterns (Hwang et al, 2011;Ward et al, 2018), and we therefore need to take them into account when projecting effects of climate change on phenology (De Frenne et al, 2013;Franklin et al 2013). Especially in forests, these microclimate dynamics have a stronger impact than macroclimate warming on plant responses to climate change (Zellweger et al 2020).…”
Section: Impact Of Microclimate On Phenologymentioning
confidence: 99%
“…We calculated early‐ and late‐season GDD at each plot based on when snow melted at that location, defining GDDearly as the daily temperature sum above 0°C during the first 25 d post‐SDD, and GDDlate as a parallel metric for days 25–50 post‐SDD. The use of a rolling window after snowmelt for calculating degree days rather than fixed calendar period/s is common in studies of high‐altitude meadows (e.g., Sedlacek et al 2015, Semenchuk et al 2016), because air temperature can only exert an influence on herbaceous plant reproduction after the insulation of snow has melted (Ward et al 2018). This does mean that SDD and GDD are related, because early snowmelt is associated with cooler early‐season temperatures and late snowmelt with cooler late‐season temperatures (Appendix : Fig.…”
Section: Methodsmentioning
confidence: 99%
“…Factors such as microclimate (Ward 2018) and elevation (Ziello 2009) can greatly influence local plant phenology. As such, it is essential to understand the environmental conditions where data sampling occurs, in order to decouple these effects from larger climate trends.…”
Section: Invasive Species As a Driver Of Ecological Changementioning
confidence: 99%