Not exact matches
Modern electronic techniques make it relatively easy
to distinguish true
signals from
noise; in addition, computers make possible the performance of
significant experiments concerning the complex relationship between stimulus and action.
It's been argued a
significant trend is expected under a warming climate, but the
signal -
to -
noise ratio is still too low in most places in Antarctica, even where the warming trend (e.g. WAIS) is quite large.
But detectability is a function of the
signal to noise ratio — a small shift in the mean of a distribution can give a detectable
signal at the tail but not a
significant signal near the middle.
A tropical SST link would explain why the
signal is strongest with a 10
to 20 year lag of the long - term changes (Waple et al, 2001), but the
noise in the NAO record could mean that you only see
significant changes after long term averaging.
It is true that there has been no «statistically
significant» warming in the last 16 (or 15 years) only because when you deal with such short data sets the
signal to noise ratio decreases, meaning that the 95 % confidence level also increases.
«that no - one has measured a CO2
signal in any modern temperature / time graph, so by standard
signal -
to -
noise ratio physics, there is a strong indication that the climate sensitivity of CO2 is 0.0 C
to one place of decimals, or two
significant digits.»
But while there's a lot of verbiage there, there isn't anything that addresses the basic problem of attempting
to pretend that there's something
significant about a «flattening» that is far more likely
to be
noise than
signal.
Serious matter, trying
to measure a tiny,
significant signal in a sea of
noise.
Additionally, a longer time perspective is needed
to develop ways
to separate the ecological «
noise» from the
significant ecological
signals that would presage biodiversity collapse.
The trick is that past data aren't considered as «
noise», or only in limited amount, but rather as a
significant «
signal» that can be substracted from the observed data
to get a
significant trend.
The
signal to noise ratio for low level radiation is very low and the number of variables in the
noise is
significant.
The space - time structure of natural climate variability needed
to determine the optimal fingerprint pattern and the resultant
signal -
to -
noise ratio of the detection variable is estimated from several multi-century control simulations with different CGCMs and from instrumental data over the last 136 y. Applying the combined greenhouse gas - plus - aerosol fingerprint in the same way as the greenhouse gas only fingerprint in a previous work, the recent 30 - y trends (1966 — 1995) of annual mean near surface temperature are again found
to represent a
significant climate change at the 97.5 % confidence level.
We experienced
significant signal drop in our testing, the active
noise cancelling was minimal at best, and a sibilant sound quality made cymbal hits and «s» sounds fatiguing
to listen
to.