A regional evaluation of the influence of climate change on long term trends in chlorophyll-a in large Italian lakes from satellite data

G. Free, M. Bresciani, M. Pinardi, Nicola Ghirardi, G. Luciani, R. Caroni, C. Giardino
{"title":"A regional evaluation of the influence of climate change on long term\ntrends in chlorophyll-a in large Italian lakes from satellite data","authors":"G. Free, M. Bresciani, M. Pinardi, Nicola Ghirardi, G. Luciani, R. Caroni, C. Giardino","doi":"10.5194/esd-2020-56","DOIUrl":null,"url":null,"abstract":"Abstract. Climate change has increased the temperature and altered the mixing regime of high-value lakes in the sub-alpine region of Northern Italy. Remote sensing of chlorophyll-a can help provide a time-series to allow an assessment of the ecological implications of this. Non-parametric multiplicative regression (NPMR) was used to visualize and understand the changes that have occurred between 2003–2018 in lakes Garda, Como, Iseo and Maggiore. In all four deep sub-alpine lakes there has been a disruption from a traditional pattern of a significant spring chlorophyll-a peak followed by a clear water phase and summer/autumn peaks. This was replaced after 2010–2012, with lower spring peaks and a tendency for annual maxima to occur in summer. There was a tendency for this switch to be interspersed by a two-year period of low chlorophyll-a, which seemed to extend until 2018 for Lake Garda. Variables that were significant in NPMR included time, air temperature, wind speed, cloud cover, winter temperature and winter values for the North Atlantic Oscillation and Eastern Atlantic pattern. The change from spring to summer chlorophyll-a maxima, relatively sudden in an ecological context, could be interpreted as a regime shift. The cause is probably cascading effects from increased winter temperatures, reduced winter mixing and altered nutrient dynamics. Future trends will depend on climate change and inter-decadal climate drivers.\n","PeriodicalId":11466,"journal":{"name":"Earth System Dynamics Discussions","volume":"1 1","pages":"1-19"},"PeriodicalIF":0.0000,"publicationDate":"2020-07-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Earth System Dynamics Discussions","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5194/esd-2020-56","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 3

Abstract

Abstract. Climate change has increased the temperature and altered the mixing regime of high-value lakes in the sub-alpine region of Northern Italy. Remote sensing of chlorophyll-a can help provide a time-series to allow an assessment of the ecological implications of this. Non-parametric multiplicative regression (NPMR) was used to visualize and understand the changes that have occurred between 2003–2018 in lakes Garda, Como, Iseo and Maggiore. In all four deep sub-alpine lakes there has been a disruption from a traditional pattern of a significant spring chlorophyll-a peak followed by a clear water phase and summer/autumn peaks. This was replaced after 2010–2012, with lower spring peaks and a tendency for annual maxima to occur in summer. There was a tendency for this switch to be interspersed by a two-year period of low chlorophyll-a, which seemed to extend until 2018 for Lake Garda. Variables that were significant in NPMR included time, air temperature, wind speed, cloud cover, winter temperature and winter values for the North Atlantic Oscillation and Eastern Atlantic pattern. The change from spring to summer chlorophyll-a maxima, relatively sudden in an ecological context, could be interpreted as a regime shift. The cause is probably cascading effects from increased winter temperatures, reduced winter mixing and altered nutrient dynamics. Future trends will depend on climate change and inter-decadal climate drivers.
气候变化对意大利大型湖泊叶绿素- A长期趋势影响的区域评估(卫星数据)
摘要气候变化增加了温度,改变了意大利北部亚高山地区高价值湖泊的混合状态。叶绿素-a的遥感可以帮助提供一个时间序列,以便对这种情况的生态影响进行评估。采用非参数乘法回归(NPMR)对Garda、Como、Iseo和Maggiore湖2003-2018年的变化进行了可视化分析。在所有四个深亚高山湖泊中,传统的春季叶绿素峰值-随后是清澈的水阶段和夏季/秋季峰值的模式已经被打破。2010-2012年之后,春季峰值降低,年最大值出现在夏季。这种转变有一种被两年的低叶绿素a期所点缀的趋势,对加尔达湖来说,这一时期似乎一直延续到2018年。NPMR中显著的变量包括时间、气温、风速、云量、冬季温度以及北大西洋涛动和东大西洋模式的冬季值。从春季到夏季叶绿素a最大值的变化,在生态环境中相对突然,可以解释为一种制度转变。原因可能是冬季气温升高、冬季混合减少和营养动态改变的级联效应。未来趋势将取决于气候变化和年代际气候驱动因素。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信