Sentences with phrase «land near the ocean»

A beach or other land near the ocean is great because it is super romantic and super free!

Orange County officials rescinded plans to establish three temporary shelters on county land near the ocean.

Not exact matches

Exploring those regions or landing near cracks on the moons Europa and Enceladus, which may harbor subsurface oceans, could require reinstituting the baking step, Conley says.

They interpreted the deposits were formed on land, not in the ocean, by identifying the presence of geyserite — a mineral deposit formed from near boiling - temperature, silica - rich, fluids that is only found in a terrestrial hot spring environment.

Fiber goes out in the ocean, and it's all over the land, so this technology increases the likelihood that a sensor is near the rupture when an earthquake happens, which translates into finding small events, improved earthquake locations, and extra time for early warning.»

This study also offers a slice of pterosaur life history that is out of reach of fossil evidence, suggesting that the reptiles lived within easy access of warm thermal wind currents near open spaces of land or near the ocean.

Land based and sea - going human activities are affecting the ocean in both near field and far field.

Since today's Earth has a continent over the South Pole and an almost land - locked ocean over the North Pole, geologists believe that Earth will continue to endure glacial periods in the geologically near future.

The Landings is conveniently located near the main resort and offers a magnificent tropical setting complete with ocean views, warm breezes, and palm trees overhead.

Heading west to east, you can travel back in history from the cutting - edge high tech of contemporary Silicon Valley, across the Wild West frontier of the mid-1800s, and through lands the likes of Daniel Boone and countless others pioneered in the 1700s, before arriving at the Atlantic Ocean near some of the oldest and best - preserved colonial - era landscapes in the United States.

Costa Rica Weather & Surfing — There's a new app specifically made for people planning of hanging ten in Costa Rica or if you just be safe near the oceans of the land of «Pura Vida».

Tocumen International is near the southern end of the Panama Canal, so once you've landed you will be traveling up the canal towards its southern end that opens onto the Pacific Ocean.

The land here is a few hundred meters above sea level so it attracts a very different set of birds than those that are found near the ocean.

Continuing to expand their brand under the vision of «unearthing the exceptional» this year has also seen Mantis embark on the development of a five star hotel on the island of St. Helena, in the South Atlantic Ocean, 2,000 km from the nearest major land mass.

For many of our early immigrants the coastline near the lighthouse would have been their very first land sighting after a very long, ocean voyage from Europe.

Depending on the time you have you can go as far or near as you want along the Great Ocean Road before returning either the same route or choosing the in land route for a bit of variety.

Exciting Cabrera Ocean View Land near Playa Grande on the evergreen North Coast of the DR.. This Cabrera Ocean View Land...

«The global annual temperature for combined land and ocean surfaces for 2007 is expected to be near 58.0 °F and would be the fifth warmest since records began in 1880.

The two longest ones are of temperature near the Earth's surface: a vast network of weather stations over land areas, and ship data from the oceans.

About half the solar energy reaching Earth is absorbed by the ocean and land, where it is temporarily stored near the surface.

Peter: I will concede that you could have very cold air blowing over the ocean from the land, but a) this tends to be localized near to the coast, and b) the air will warm, but as a result of the ocean being a lot warmer, not as a result of the ocean freezing In regards to a: I am not sure that it would always be «localized near to the coast».

Now land and ocean are both near records.

iv) The downward infrared flux from the atmosphere to land surface or ocean is primarily natural so that the near surface temperature already accommodates that natural component.

I will concede that you could have very cold air blowing over the ocean from the land, but a) this tends to be localized near to the coast, and b) the air will warm, but as a result of the ocean being a lot warmer, not as a result of the ocean freezing.

The land in turn creates warmer rivers which then enter the ocean and follow the bottom out to deep water so for diving buoys that don't come near shore the heat is not observed passing through the open ocean surface.

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 yearly avocean 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 avocean 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 avocean 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 avOcean 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 average

«If we ask models the questions they are capable of answering, they answer them reliably,» counters Professor Jim Kinter from the Center for Ocean - Land - Atmosphere Studies near Washington DC, who is attending the Reading meeting.

At the northwestern end of the vast, fire - marred range that now covers a land area larger than most countries, temperatures near the Arctic Ocean shore at 70.9 ° N, 81.4 ° E are 86 degrees F (30 C)-- about 40 degrees F (22 C) above average.

A note of caution: To avoid erroneous ice concentration along coasts (satellite signal mixed from land and ocean), near coastal - areas have to be excluded.

This includes maintaining Argo, the main system for monitoring ocean heat content, and the development of Deep Argo to monitor the lower half of the ocean; the use of ship - based subsurface ocean temperature monitoring programs; advancements in robotic technologies such as autonomous underwater vehicles to monitor waters adjacent to land (like islands or coastal regions); and further development of real - or near - real - time deep ocean remote sensing methods.

The cold waters near the poles and the deep oceans are far from saturated, but these have a limited exchange, neither are land plants near saturation, but they have other limits.

Non-ocean signals, such as in the Indian Ocean due to the 2004 Sumatran — Andean earthquake, and near Greenland and West Antarctica due to land signal leakage, can also corrupt the ocean trend estimocean signals, such as in the Indian Ocean due to the 2004 Sumatran — Andean earthquake, and near Greenland and West Antarctica due to land signal leakage, can also corrupt the ocean trend estimOcean due to the 2004 Sumatran — Andean earthquake, and near Greenland and West Antarctica due to land signal leakage, can also corrupt the ocean trend estimocean trend estimates.

@Myrrh You appear to have a belief that visible light (which includes near - IR) does not warm the land and oceans.

In tranquil, well - behaved parts of the ocean like near the Galapagos, it would be probably easier to document changes in the carbon content of the upper ocean than it would be on land.

To point out just a couple of things: — oceans warming slower (or cooling slower) than lands on long - time trends is absolutely normal, because water is more difficult both to warm or to cool (I mean, we require both a bigger heat flow and more time); at the contrary, I see as a non-sense theory (made by some serrist, but don't know who) that oceans are storing up heat, and that suddenly they will release such heat as a positive feedback: or the water warms than no heat can be considered ad «stored» (we have no phase change inside oceans, so no latent heat) or oceans begin to release heat but in the same time they have to cool (because they are losing heat); so, I don't feel strange that in last years land temperatures for some series (NCDC and GISS) can be heating up while oceans are slightly cooling, but I feel strange that they are heating up so much to reverse global trend from slightly negative / stable to slightly positive; but, in the end, all this is not an evidence that lands» warming is led by UHI (but, this effect, I would not exclude it from having a small part in temperature trends for some regional area, but just small); both because, as writtend, it is normal to have waters warming slower than lands, and because lands» temperatures are often measured in a not so precise way (despite they continue to give us a global uncertainity in TT values which is barely the instrumental's one)-- but, to point out, HadCRU and MSU of last years (I mean always 2002 - 2006) follow much better waters» temperatures trend; — metropolis and larger cities temperature trends actually show an increase in UHI effect, but I think the sites are few, and the covered area is very small worldwide, so the global effect is very poor (but it still can be sensible for regional effects); but I would not run out a small warming trend for airport measurements due mainly to three things: increasing jet planes traffic, enlarging airports (then more buildings and more asphalt — if you follow motor sports, or simply live in a town / city, you will know how easy they get very warmer than air during day, and how much it can slow night - time cooling) and overall having airports nearer to cities (if not becoming an area inside the city after some decade of hurban growth, e.g. Milan - Linate); — I found no point about UHI in towns and villages; you will tell me they are not large cities; but, in comparison with 20-40-60 years ago when they were «countryside», many small towns and villages have become part of larger hurban areas (at least in Europe and Asia) so examining just larger cities would not be enough in my opinion to get a full view of UHI effect (still remembering that it has a small global effect: we can say many matters are due to UHI instead of GW, maybe even that a small part of measured GW is due to UHI, and that GW measurements are not so precise to make us able to make good analisyses and predictions, but not that GW is due to UHI).

The standard deviation of the monthly MSU 2R anomalies has a much more zonally symmetric structure (Fig. 4 and Fig. 5) so that relative to the surface there is a much larger contribution from the northern oceans and a generally smaller contribution over land and near the equator to the hemispheric and global means.

These models predicted that the Northern Hemisphere Polar region would warm fastest and first, that the Southern Ocean would draw a greater portion of atmospheric heat into the ocean system, and that land ice melt near Greenland and West Antarctica would generate cold, fresh water flows into the nearby ocean zones and set off localized cooOcean would draw a greater portion of atmospheric heat into the ocean system, and that land ice melt near Greenland and West Antarctica would generate cold, fresh water flows into the nearby ocean zones and set off localized cooocean system, and that land ice melt near Greenland and West Antarctica would generate cold, fresh water flows into the nearby ocean zones and set off localized cooocean zones and set off localized cooling.

The AGW claim from the comic cartoon KT97 and kin The Greenhouse Effect says that Shortwave, (near UV, visible and near infrared, but mostly visible) heats up land and oceans, that no longwave infrared from the Sun gets through the invisible undefined and unexplained barrier said to be like the glass of a greenhouse, and then the Shortwave heated land and oceans radiate out longwave infrared, (which in real physics is heat, also called thermal infrared).

The ubiquitous character of certain events further confirms their importance: «the Younger Dryas and a large number of abrupt changes during the last ice age called Dansgaard / Oeschger events (23 abrupt changes into a climate of near - modern warmth and out again, during the last glacial period) have been corroborated in multiple ice cores from Greenland, Antarctica and tropical mountains, marine sediments from the North Atlantic Ocean, the tropical Atlantic, eastern Pacific, and Indian Oceans, and from various records on land.

In the 1960s, the United States began using satellites to observe its lands, oceans, atmosphere and the space environment near Earth.

Ocean waters near shore do not show depleted iron levels due to the interaction of the ocean with land, and water runoff that contains Ocean waters near shore do not show depleted iron levels due to the interaction of the ocean with land, and water runoff that contains ocean with land, and water runoff that contains iron.

The news of a few houses, foolishly built on fragile land too near the sea bluffs» edge, were indeed falling into the ocean and were now providing great photo - ops...

From my experience sailing offshore for almost 20 years, the mid oceans are generally pretty empty of life, while near land life is much more abundant.

Their analysis revealed that almost two - thirds of the listed impacts related specifically to the warming over land and near the surface of the ocean could confidently be attributed to human - generated emissions.

Land near currents is affected by the temp of the ocean currents.

This is reflected in the clarity of the water, which is clear mid ocean and murky near land, even where there are no people.

Only Land near or on the poles is required because ice - sheets build up on Land and not on the Ocean.

In truth, even if Christmas does bring warmth, it won't matter a whit, and not because the true measurements — based on comprehensive satellite readings rather than from a scattering of thermometers on land and ocean buoys — show 2014 to be nowhere near setting records.

Some examples from energy balance model calculations indicate that: (1) solar variability has a near - global response, with the amplitude of response slightly larger over land; (2) volcanism has a proportionately larger amplitude of response over land than over ocean; and (3) the most oft - cited mode of internal variability, changes in the North Atlantic thermohaline circulation, has a hemispheric asymmetry in response.

The ice stream's speed - up and near - doubling of ice flow from land into the ocean has increased the rate of sea level rise by about.06 millimeters (about.002 inches) per year, or roughly 4 percent of the 20th century rate of sea level increase.