Not exact matches
Currently, our robots are little more intelligent than
sea slugs, and even after decades of clever research, they can barely distinguish figures from a
background at the skill level of an infant.
Rising majestically from the
sea, a waterfall trickled gently in the
background and the only sound was the slight gurgle as a nearby turtle raised his wizened head to glance quizzically
at us.
Perched on the cliff on «Millionaires Row» in Wharf Street, Port Douglas, Queensland, Australia the 180 degree views are stunning as you look out
at the horizon and the Coral
Sea with the mountains of Cape Tribulation reaching up in the
background.
Get a selfie
at the breathtaking Henry Ross Lookout with the Coral
Sea and Cairns city in the
background
Guests can also dine
at nicely furnished dining room where taste fine local dishes and relax in the panoramic terrace, enjoying a drink or reading a book with the
background sound of the
sea.
The painting closest to Miró and Gorky already hints
at a landscape by the
sea, with a firm horizon line and blue
background above it.
Solo exhibitions include
Background 2
at Kristin Hjellegjerde Gallery, London (2015),
Background 1
at Lela Gallery, Addis Ababa (2014), and X Privacy
at the Alliance Ethio - Française, Addis Ababa (2012), while group exhibitions include Pangaea II: New Art from Africa and Latin America, Saatchi Gallery, London (2015), Concerning The Internal
at Circle Art Gallery, Nairobi (2015), Visibles / Invisibles
at Fondation Blachere, Apt (2015), the display of the Habesha Art Collection
at the National Museum in Addis Ababa (2014), and the touring exhibition Silver
Sea Cross-Ship (2013 - 14).
The resting giants
at the bottom of the
sea do not only form fascinating and unique
backgrounds for Andreas Franke's sceneries.
In her two «Beaufort Scale,» 2005 works (for use
at sea and for use on land) Floyer prints onto a white
background, the wind velocity classifications as described in the Beaufort Wind Scale invented by Sir Francis Beaufort in 1805.
Most interesting is that the about monthly variations correlate with the lunar phases (peak on full moon) The Helsinki
Background measurements 1935 The first background measurements in history; sampling data in vertical profile every 50 - 100m up to 1,5 km; 364 ppm underthe clouds and above Haldane measurements at the Scottish coast 370 ppmCO2 in winds from the sea; 355 ppm in air from the land Wattenberg measurements in the southern Atlantic ocean 1925-1927 310 sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm year
Background measurements 1935 The first
background measurements in history; sampling data in vertical profile every 50 - 100m up to 1,5 km; 364 ppm underthe clouds and above Haldane measurements at the Scottish coast 370 ppmCO2 in winds from the sea; 355 ppm in air from the land Wattenberg measurements in the southern Atlantic ocean 1925-1927 310 sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm year
background measurements in history; sampling data in vertical profile every 50 - 100m up to 1,5 km; 364 ppm underthe clouds and above Haldane measurements
at the Scottish coast 370 ppmCO2 in winds from the
sea; 355 ppm in air from the land Wattenberg measurements in the southern Atlantic ocean 1925-1927 310 sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aver
sea; 355 ppm in air from the land Wattenberg measurements in the southern Atlantic ocean 1925-1927 310 sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the
sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aver
sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over
sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aver
sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents
Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aver
Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over
sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly aver
sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly average
For
background on the decline of Arctic
sea ice, see my summary post
at Climate Dialogue (and Climate Etc. references therein).
b Trends surface temperature from the GOGA CAM3 simulations (
background colorscale; air temperature over
sea ice and SST elsewhere) along with the Z850 trend produced by the model simulations (black contours; negative dashed and positive solid; interval of 3 m / decade) and the simulated convective precipitation trends (positive green contours, negative red contours, contoured
at − 0.7, − 0.3, − 0.1, 0.1, 0.3, and 0.7 mm / day / decade, shown only for 45 ° S — 45 ° N. (c) As in (b) but for the TOGA CAM3 simulations.
For example, an analysis of the risks of
sea level rise for the State of California evaluated the economic value of property
at risk of flooding, as well as the size, economic status, and demographic
backgrounds of the population living in areas vulnerable to flooding, area of wetland likely to be lost, and other metrics related to threatened transportation, energy, and water infrastructure (Heberger et al 2011).
The oceans control the
background rate of energy flow from ocean to air via The Hot Water Bottle Effect and it is the energy flow from ocean to air (supplemented to a miniscule extent by the greenhouse effect) that drives the rate of evaporation by creating varying temperature differentials between
sea surface and air
at the surface.
The advocate scientists only want to focus on the bad effects of warming, some large percentage of which is naturally occurring
at a
background rate anyway (6mm / year
background rate of
sea level rise given 120 meters over 20,000 years — that is double the current rate of 3mm / year rise and how much of that is natural?).