Exceptional 2023 marine heat wave reshapes North Atlantic coccolithophore blooms
Guinaldo T, Neukermans G.
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Challenges in modelling the impact of frost and heat stress on the yield of cool-season annual grain crops. [PDF]
Richetti J +12 more
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Retrospective entomological and eco-epidemiological survey of a leishmaniasis outbreak in southern Spain. [PDF]
González MA +11 more
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Impact of high temperature in 2023 and 2024 on spring leaf flush phenology in Japan derived by GCOM-C satellite. [PDF]
Mizuno Y +4 more
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Seasonal divergence in reproductive timing on the verge of spring: comparing hypothalamic transcriptome of two seasonally sympatric North American songbird populations. [PDF]
Singh D, Fudickar AM, Ketterson ED.
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Buying time – increasing yield potential in wheat by extending stem elongation duration
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Approximating Lake Ice Phenology with Satellite Surface Temperature Data
2021 IEEE International Geoscience and Remote Sensing Symposium IGARSS, 2021Studies of lake ice phenology have historically relied on limited in situ data. Satellite-derived temperature data provide an opportunity to better understand the climatological factors and trends behind ice phenology. Here we developed a model that uses daytime and nighttime surface temperature observations from the Moderate Resolution Imaging ...
Sophia Karina Skoglund +6 more
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Lake ice phenology changes in the northern hemisphere
2021<p>Lake-ice phenology is an essential indicator of climate change impact for different regions (Livingstone, 1997; Duguay, 2010), which helps understand the regional characters of synchrony and asynchrony. The observation of lake ice phenology includes ground observation and remote sensing inversion. Although some lakes have been observed
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Shortening ice seasons and changing phenology affect under-ice lake thermal dynamics
2023Temperate lakes worldwide are losing ice cover but the implications for under-ice thermal dynamics are poorly constrained. Using a 90-year record of ice phenology from a temperate lake, we examined trends, variability, and drivers of ice phenology. The onset of ice formation decreased by 23 days century-1 which can be largely attributed to warming air ...
Isabella Oleksy, David Richardson
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In Chapter 5 of this book, it is shown that the formation of ice on the surface of a lake (‘ice-on’) and its thawing and ultimate disappearance (‘ice-off’) are complex phenomena governed by mechanisms that involve many interacting meteorological (and some non-meteorological) forcing factors. Linking ice phenology – the timing of ice-on and ice-off – to
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