Characterizing ecosystem phenological diversity and its macroecology with snow cover phenology

Abstract One critical challenge of exploring flora phenology is on characterizing ecosystem phenological diversity (EPD), and thus how EPD’s performance is influenced by climate changes has also been an open macro-ecological question. To fill these two gaps, we proposed an innovative method for refl...

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Published in:Scientific Reports
Main Authors: Lin, Yi, Hyyppä, Juha
Other Authors: National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Springer Science and Business Media LLC 2019
Subjects:
Online Access:http://dx.doi.org/10.1038/s41598-019-51602-1
http://www.nature.com/articles/s41598-019-51602-1.pdf
http://www.nature.com/articles/s41598-019-51602-1
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author Lin, Yi
Hyyppä, Juha
author2 National Natural Science Foundation of China
author_facet Lin, Yi
Hyyppä, Juha
author_sort Lin, Yi
collection Springer Nature
container_issue 1
container_title Scientific Reports
container_volume 9
description Abstract One critical challenge of exploring flora phenology is on characterizing ecosystem phenological diversity (EPD), and thus how EPD’s performance is influenced by climate changes has also been an open macro-ecological question. To fill these two gaps, we proposed an innovative method for reflecting EPD, by taking the advantage of the often-classified inverse factor of spatial resolution discrepancy between the used remote sensing datasets of vegetation phenological dates (green-up and brown-up) and snow cover phenological dates (SPDs) (onset and end) around the Arctic, and further, we examined the cross response/feedbacks of the two kinds of EPDs to the two categories of SPDs. We found that the circumpolar green-up and brown-up EPDs both were shrinking, driven more by the delaying of the onset SPDs than the advancing of the end SPDs; North America and North Eurasia performed with inconsistent EPD response/feedbacks to the related SPD anomalies; and further, the EPD-SPD response/feedbacks in some locations exhibited the time-lag effect, e.g., the green-up EPDs made the strongest response to the onset SPDs of two years earlier. Overall, the validated method and the new findings are of implications for improving the phenology modules in Earth system models, and the contributions of the present study have enlightening significance for kicking off the new EPD branch in macrosystem phenological ecology.
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genre_facet Arctic
geographic Arctic
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spelling crspringernat:10.1038/s41598-019-51602-1 2025-01-16T20:41:08+00:00 Characterizing ecosystem phenological diversity and its macroecology with snow cover phenology Lin, Yi Hyyppä, Juha National Natural Science Foundation of China 2019 http://dx.doi.org/10.1038/s41598-019-51602-1 http://www.nature.com/articles/s41598-019-51602-1.pdf http://www.nature.com/articles/s41598-019-51602-1 en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Scientific Reports volume 9, issue 1 ISSN 2045-2322 Multidisciplinary journal-article 2019 crspringernat https://doi.org/10.1038/s41598-019-51602-1 2022-01-04T16:43:14Z Abstract One critical challenge of exploring flora phenology is on characterizing ecosystem phenological diversity (EPD), and thus how EPD’s performance is influenced by climate changes has also been an open macro-ecological question. To fill these two gaps, we proposed an innovative method for reflecting EPD, by taking the advantage of the often-classified inverse factor of spatial resolution discrepancy between the used remote sensing datasets of vegetation phenological dates (green-up and brown-up) and snow cover phenological dates (SPDs) (onset and end) around the Arctic, and further, we examined the cross response/feedbacks of the two kinds of EPDs to the two categories of SPDs. We found that the circumpolar green-up and brown-up EPDs both were shrinking, driven more by the delaying of the onset SPDs than the advancing of the end SPDs; North America and North Eurasia performed with inconsistent EPD response/feedbacks to the related SPD anomalies; and further, the EPD-SPD response/feedbacks in some locations exhibited the time-lag effect, e.g., the green-up EPDs made the strongest response to the onset SPDs of two years earlier. Overall, the validated method and the new findings are of implications for improving the phenology modules in Earth system models, and the contributions of the present study have enlightening significance for kicking off the new EPD branch in macrosystem phenological ecology. Article in Journal/Newspaper Arctic Springer Nature Arctic Scientific Reports 9 1
spellingShingle Multidisciplinary
Lin, Yi
Hyyppä, Juha
Characterizing ecosystem phenological diversity and its macroecology with snow cover phenology
title Characterizing ecosystem phenological diversity and its macroecology with snow cover phenology
title_full Characterizing ecosystem phenological diversity and its macroecology with snow cover phenology
title_fullStr Characterizing ecosystem phenological diversity and its macroecology with snow cover phenology
title_full_unstemmed Characterizing ecosystem phenological diversity and its macroecology with snow cover phenology
title_short Characterizing ecosystem phenological diversity and its macroecology with snow cover phenology
title_sort characterizing ecosystem phenological diversity and its macroecology with snow cover phenology
topic Multidisciplinary
topic_facet Multidisciplinary
url http://dx.doi.org/10.1038/s41598-019-51602-1
http://www.nature.com/articles/s41598-019-51602-1.pdf
http://www.nature.com/articles/s41598-019-51602-1