Not exact matches
Realistic large -
scale solar panel coverage could cause less than half a degree
of local warming, far less than the several degrees in global temperature rise predicted over the
next century if we keep burning fossil fuels.
Newman appears again in Twice Hammered (2011), where one finds the reproduction
of Diao's earlier Barnett Newman: The Paintings (1990; for which Diao presents all
of Newman's paintings at small
scale and reduced to the shapes
of their canvases)
next to that work's accompanying catalogue entry from a May 2005 Christie's Hong Kong 20th
Century Chinese and Asian Contemporary Art sale.
[Response: Here's a simple back -
of - envelope consideration for the future: if the Greenland ice sheet melts completely over the
next ~ 1,000 years (Jim Hansen argues in the current Climatic Change that the time
scale could be
centuries), this would contribute an average flux
of ~ 0.1 Sv
of freshwater to the surrounding ocean.
For those curious about the pronounced dips in the future scenarios here they are responses to Pinatubo -
scale volcanic eruptions that are assumed to occur at a reasonable frequency over the course
of the
next century.
Next point, changes in volcanic activity can affect decadal and
century -
scale temperatures due to the random occurence
of eruptions
of the right sort (though I don't think you dispute that).
A new international study is the first to use a high - resolution, large -
scale computer model to estimate how much ice the West Antarctic Ice Sheet could lose over the
next couple
of centuries, and how much that could add to sea - level rise.
Their work encompasses a range
of problems and time
scales: from five - day model predictions
of hurricane track and intensity, to understanding the causes
of changes in extremes over the past
century, to building new climate prediction models for seamless predictions out to the
next several years, to earth system model projections
of human - caused changes in various extremes (heat waves, hurricanes, droughts, etc.) over the coming
century.
(September 12, 2016)- A collaboration
of university researchers, government agencies, and private sector groups released today a
next - generation climate modeling dataset with improved local -
scale climate projections covering the 21st
century for a region from northern Mexico to southern Canada.
The relative magnitudes
of the climate impacts induced by the naturally - occurring NAO and by anthropogenic factors will depend on the time horizon (e.g.,
next few decades vs. end
of the twenty - first
century), time -
scale (interannual vs. multi-decadal), and parameter (temperature vs. precipitation)
of interest (e.g., Deser et al. 2012).
For however long this persists on the time
scale of decades to
centuries the
next deeper ocean layer will be slowly warmed by the warmed up top layer.
The close agreement
of warming for the early
century, with a range
of only 0.05 °C among the SRES cases, shows that no matter which
of these non-mitigation scenarios is followed, the warming is similar on the time
scale of the
next decade or two.
The story ranges from physics to chemistry, biology, geology, fluid mechanics, and quantum mechanics, to economics and social sciences.The class will consider evidence from the distant past and projections into the distant future, keeping the human time
scale of the
next several
centuries as the bottom line.The lectures follow a textbook, «Global Warming, Understanding the Forecast,» written for the course.
N.b. this diverges from the commonly used «Charney sensitivity» which describes temperature change over the
next century or so, and which is less than the change expected over the multi-millenial
scale of dwindling ice sheets and vegetation changes.
«Scientific and economic challenges still exist,» writes Harvard geoscientist Daniel Schrag, «but none are serious enough to suggest that carbon capture and storage will not work at the
scale required to offset trillions
of tons
of carbon dioxide emissions over the
next century.»
The early Eocene hyperthermals, a series
of transient global warming events (2 to 5 °C, provide a unique opportunity to assess the sensitivity
of the hydrologic cycle to the
scale of greenhouse forcing expected over the
next several
centuries.