Not exact matches
«Our findings may reflect a
temporal change in smoking patterns in which the proportion of adults with a 30 pack -
year smoking history and having quit within 15
years declined,» the authors write.
Several previous analyses of tide gauge records1, 2,3,4,5,6 — employing different methods to accommodate the spatial sparsity and
temporal incompleteness of the data and to constrain the geometry of long - term sea - level
change — have concluded that GMSL rose over the twentieth century at a mean rate of 1.6 to 1.9 millimetres per
year.
«This study will improve understanding of
temporal changes in body burden from pregnancy through the first few
years post-partum and provide uniquely high - quality data on the role of early PFC exposures in ASD.»
In that tale, a traveler to the past determined to hunt down a T - Rex strays from a carefully laid - out trail and crushes a butterfly, creating a ripple of
temporal change that becomes a mighty wave over the
years,
changing history in ways no one thought imaginable.
By analyzing 80 proxy records from around the globe (generally with resolutions better than 500
years) the authors are able to evaluate the
changes occurring during different time periods in order to characterize the spatial and
temporal structure of the deglacial evolution.
Mike's work, like that of previous award winners, is diverse, and includes pioneering and highly cited work in time series analysis (an elegant use of Thomson's multitaper spectral analysis approach to detect spatiotemporal oscillations in the climate record and methods for smoothing
temporal data), decadal climate variability (the term «Atlantic Multidecadal Oscillation» or «AMO» was coined by Mike in an interview with Science's Richard Kerr about a paper he had published with Tom Delworth of GFDL showing evidence in both climate model simulations and observational data for a 50 - 70
year oscillation in the climate system; significantly Mike also published work with Kerry Emanuel in 2006 showing that the AMO concept has been overstated as regards its role in 20th century tropical Atlantic SST
changes, a finding recently reaffirmed by a study published in Nature), in showing how
changes in radiative forcing from volcanoes can affect ENSO, in examining the role of solar variations in explaining the pattern of the Medieval Climate Anomaly and Little Ice Age, the relationship between the climate
changes of past centuries and phenomena such as Atlantic tropical cyclones and global sea level, and even a bit of work in atmospheric chemistry (an analysis of beryllium - 7 measurements).
Our study did not directly address this question because the paleotemperature records used in our study have a
temporal resolution of ~ 120
years on average, which precludes us from examining variations in rates of
change occurring within a century.
The
temporal lag is needed to account for the large mass of Neptune that would require
years to adjust to any
changes in solar output.
A: Our study did not directly address this question because the paleotemperature records used in our study have a
temporal resolution of ~ 120
years on average, which precludes us from examining variations in rates of
change occurring within a century.
The spatial and
temporal characteristics, of climatic
change and evidence for different causes, including human activity, from the beginning of the Quaternary period (2.6 million
years ago) to the present day.