The distributions of many terrestrial organisms are currently shifting in latitude or elevation in response to changing climate Using a meta-analysis, we estimated that the distributions of species have recently shifted to higher elevations at a median rate of 110 meters per decade, and to higher latitudes at a median rate of 169 kilometers per decade These rates are approximately two and three times faster than previously reported The distances moved by species are greatest in studies showing the highest levels of warming, with average latitudinal shifts being generally sufficient to track temperature changes However, individual species vary greatly in their rates of change, suggesting that the range shift of each species depends on multiple internal species traits and external drivers of change Rapid average shifts derive from a wide diversity of responses by individual species

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Rapid Range Shifts of Species Associated with High Levels of Climate Warming

Investigating soil moisture-climate interactions in a changing climate: A review

Plants are finely tuned to the seasonality of their environment, and shifts in the timing of plant activity (i.e. phenology) provide some of the most compelling evidence that species and ecosystems are being influenced by global environmental change. Researchers across disciplines have observed shifting phenology at multiple scales, including earlier spring flowering in individual plants and an earlier spring green-up' of the land surface revealed in satellite images. Experimental and modeling approaches have sought to identify the mechanisms causing these shifts, as well as to make predictions regarding the consequences. Here, we discuss recent advances in several fields that have enabled scaling between species responses to recent climatic changes and shifts in ecosystem productivity, with implications for global carbon cycling.

https://www.cell.com/trends/ecology-evolution/pdf/S0169-5347(07)00130-9.pdf

Shifting plant phenology in response to global change

Significant changes in physical and biological systems are occurring on all continents and in most oceans, with a concentration of available data in Europe and North America. Most of these changes are in the direction expected with warming temperature. Here we show that these changes in natural systems since at least 1970 are occurring in regions of observed temperature increases, and that these temperature increases at continental scales cannot be explained by natural climate variations alone. Given the conclusions from the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report that most of the observed increase in global average temperatures since the mid-twentieth century is very likely to be due to the observed increase in anthropogenic greenhouse gas concentrations, and furthermore that it is likely that there has been significant anthropogenic warming over the past 50 years averaged over each continent except Antarctica, we conclude that anthropogenic climate change is having a significant impact on physical and biological systems globally and in some continents.

Attributing physical and biological impacts to anthropogenic climate change

There is ample evidence for ecological responses to recent climate change. Most studies to date have concentrated on the effects of climate change on individuals and species, with particular emphasis on the effects on phenology and physiology of organisms as well as changes in the distribution and range shifts of species. However, responses by individual species to climate change are not isolated; they are connected through interactions with others at the same or adjacent trophic levels. Also from this more complex perspective, recent case studies have emphasized evidence on the effects of climate change on biotic interactions and ecosystem services. This review highlights the ‘knowns’ but also ‘unknowns’ resulting from recent climate impact studies and reveals limitations of (linear) extrapolations from recent climate-induced responses of species to expected trends and magnitudes of future climate change. Hence, there is need not only to continue to focus on the impacts of climate change on the actors in ecological networks but also and more intensively to focus on the linkages between them, and to acknowledge that biotic interactions and feedback processes lead to highly complex, nonlinear and sometimes abrupt responses.

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Community and ecosystem responses to recent climate change.

Global climate change impacts can already be tracked in many physical and biological systems; in particular, terrestrial ecosystems provide a consistent picture of observed changes. One of the preferred indicators is phenology, the science of natural recurring events, as their recorded dates provide a high-temporal resolution of ongoing changes. Thus, numerous analyses have demonstrated an earlier onset of spring events for mid and higher latitudes and a lengthening of the growing season. However, published single-site or single-species studies are particularly open to suspicion of being biased towards predominantly reporting climate change-induced impacts. No comprehensive study or meta-analysis has so far examined the possible lack of evidence for changes or shifts at sites where no temperature change is observed. We used an enormous systematic phenological network data set of more than 125 000 observational series of 542 plant and 19 animal species in 21 European countries (1971–2000). Our results showed that 78% of all leafing, flowering and fruiting records advanced (30% significantly) and only 3% were significantly delayed, whereas the signal of leaf colouring/fall is ambiguous. We conclude that previously published results of phenological changes were not biased by reporting or publication predisposition: the average advance of spring/summer was 2.5 days decade � 1 in Europe. Our analysis of 254 mean national time series undoubtedly demonstrates that species’ phenology is responsive to temperature of the preceding

/pdf/european-phenological-response-to-climate-change-matches-the-3dr30qvjfp.pdf

European phenological response to climate change matches the warming pattern

Within a bilateral project of the meteorological services in Germany and Slovakia, time series of phenological phases in both countries have been analysed and compared for the time period 1951-2000. Phases of plants from all seasons which are available in both countries have been selected for a sample of eight representative stations from the observation networks of the meteorological services. The investigation comprises trend analysis, comparison of medians of the phase onset date and its year-to-year variability, their changes between the subperiods 1951-1985 and 1986-2000 and correlation with monthly averaged air temperature near surface. Differences between the phase onset dates in Germany and Slovakia can be found especially for early spring, when the onset dates are sooner and the year-to-year variability is higher in Germany compared to Slovakia. Later on in the year, differences between maritime and more continental regions within Germany become more important than differences between the two countries. The trend analysis shows that trends to sooner onset dates in spring and summer for the period 1951-2000 can be detected in general clearly in Germany, while in Slovakia trends of different sign and weaker trends can more often be found. Since the correlation between phenological phases and temperature is strong in both countries and also certain patterns of variability appear in both countries, the variability of phenological phases reflects large-scale climate change and its impact on vegetation. A future international action on a European basis is suggested to create a phenological reference data set for the area of Europe, providing a data base for climate monitoring applications and climate change impact research.

Viera Remisová

Papers

European phenological response to climate change matches the warming pattern

50-year time series of phenological phases in Germany and Slovakia: a statistical comparison