Sentences with phrase «other basins by»

In separate calculations, I obtain similar results by optimizing the pattern in distinct basins individually and then estimating the pattern in other basins by regression, suggesting that the global, same - sign character of the pattern is not an artifact of the EOF truncation used in the analysis.

Not exact matches

The agency alleges in court papers and internal memos obtained through the Freedom of Information Law that shoddy work by architect Rogers Marvel, lead contractor Commodore Construction Corp. and other parties left the Robert Moses - era Olympic - size pool plagued with «broken» piping, extensive cracking throughout the pool's basin and deck area, and other problems.

A final victory by the plaintiffs could prompt landowners in other river basins, such as the Klamath River in Oregon and California to claim similar damages from restoration efforts, Echeverria says.

In California 42 percent of the water comes from the Sacramento and San Joaquin river basins, which are fed by runoff from the Sierra Nevada and other mountain ranges.

The researchers studied water samples taken during cruises by Chinese ice breaker XueLong, (meaning «snow dragon») in summer 2008 and 2010 from the upper ocean of the Arctic's marginal seas to the basins as far north as 88 degrees latitude, just below the North Pole, as well as data from three other cruises.

Amazonian soils, in turn, are short on phosphorus and other critical nutrients that get washed away by the basin's frequent and heavy rainfall.

During the Last Glacial Maximum when the Earth was much colder, closed - basin lakes in currently dry parts of western North America, the Middle East and South America were much larger than they are now, as evidenced by radiocarbon dating and other testing of their ancient shorelines.

Dad will spend four nights at a lodge near the Chimán Indian village, fishing in rivers inhabited by two different Dorado species and other fish from the Amazon basin, such as the Pirapitinga or Amazon Pacu and the Yatorana.

Further examination of the bed topography by Vaughan and others (2006) indicates that most of the bed of the drainage basin of PIG is more than 500 meters below sea level, and there is a particularly deep basin in the eastern section of the upper basin.

It would be easy enough to test whether the storms in other basins had different characteristics by also performing an EOF analysis for each region.

The argument is then that the reason trends outside the Atlantic are weak is that they aren't being influenced by the AMO; the other explanation is that the other regions are already over the threshold, so that the Atlantic basin is more sensitive to changes in SSTs and atmospheric moisture than the other regions... or the data may be poor.

Focusing on the Permian - Triassic boundary, Gregory Ryskin [1] explores the possibility that mass extinction can be caused by an extremely fast, explosive release of dissolved methane (and other dissolved gases such as carbon dioxide and hydrogen sulfide) that accumulated in the oceanic water masses prone to stagnation and anoxia (e.g., in silled basins).

The Humboldt Current Large Marine Ecosystem (off Chile and Peru), the Benguelan Current LME (Namibia and South Africa), the Canary Current LME (Morocco), are the other main upwelling ecosystems, all driven by similar oceanographic and atmospheric processes, all on the eastern sides of ocean basins (western sides of continents).

Other studies of the Amazon climate tipping point The existence of an Amazonian climate tipping point is confirmed by other model studies, including the above - mentioned Climatic Change publication from 2008 — that suggests a large - scale die - back (70 percent) from about 3 degrees onwards, starting in the South of the bOther studies of the Amazon climate tipping point The existence of an Amazonian climate tipping point is confirmed by other model studies, including the above - mentioned Climatic Change publication from 2008 — that suggests a large - scale die - back (70 percent) from about 3 degrees onwards, starting in the South of the bother model studies, including the above - mentioned Climatic Change publication from 2008 — that suggests a large - scale die - back (70 percent) from about 3 degrees onwards, starting in the South of the basin.

If temperature of the basin goes up 1C in a hundred years it will keep the atmosphere warmer by 0.1 C for a thousand years in other words.

ii) The 60 year PDO Oscillation appears to be internal to the ocean system as the initial ENSO effects carry into the other ocean basins and then feed back to the Pacific by way of what you call a stadium wave but which I previously called he net interaction between the various ocean oscillations.

SLR satellite data includes things such as the «GIA Adjustment» — which is the amount of SLR that there would have been if the ocean basin hadn't increased in volume and in the case of this new study, how much higher the sea surface would have been if it had not been suppressed by the Mount Pinatubo volcanic eruption, another correction for ENSO / PDO «computed via a joint cyclostationary empirical orthogonal function (CSEOF) analysis of altimeter GMSL, GRACE land water storage, and Argo - based thermosteric sea level from 2005 to present», as well as other additions and adjustments — NONE OF WHICH can actually be found manifested in any change to the physical Sea Surface Height.»

See how global warming is undermining the stability of the MacKenzie River basin in Canada — and find other hot spots threatened by higher ground temperature on the Climate Hot Map.

It found that Brazil's protection of a core zone of rainforest would be enough to maintain precipitation across the basin and avoid the catastrophic «die - off» projected by other models, notably the Hadley model produced by the UK Meteorological Office.

These and other observations can be integrated into a model with feedbacks and having two unstable end ‐ points that is consistent both with classical studies of past climate states, and also with recent analysis of ice dynamics in the Arctic basin by Zhakarov, whose oscillatory model identifies feedback mechanisms in atmosphere and ocean, both positive and negative, that interact in such a manner as to prevent long ‐ term trends in either ice ‐ loss or ice ‐ gain on the Arctic Ocean to proceed to an ultimate state.

Only in the Kara Sea is ice cover dominated by thermodynamic factors, while ice cover in the other basins is dominated by the effects of wind and currents.

Even with warming of 2 °C, we can expect to see adverse effects on water availability in critical river basins, a more than doubling of forest fires in Amazonia by 2050, impacted coral reef recovery from bleaching events, among other effects.

The other end of the home a natures head composting toilet, basin and shower make up the bathroom area and are surrounded by beautiful lath art - work which is made from wood from old demolished homes in the Portland area.

Another general legacy of agricultural land use has been the creation of anthropogenic soils (anthrosols)(85), including the manure - enriched «plaggen» soils of Northwestern Europe, which may date to 4000 B.C. (86), the «terra preta» of the Amazon basin enriched with charcoal dating perhaps to 500 B.C. (87) and potentially in Africa (88), together with a wide range of anthrosols altered by sustained tillage, irrigation, manuring, and other land - use practices (83, 89).

And with the TOA imbalance, the energy that maintains the basins changes, restructuring the climate kinetics of regions, for instance the jet stream shifts documented by Dr. Jennifer Francis and others.

Variations in tropical cyclones, hurricanes and typhoons are dominated by ENSO and decadal variability, which result in a redistribution of tropical storm numbers and their tracks, so that increases in one basin are often compensated by decreases over other oceans.

Declared a Biosphere Preserve by UNESCO in 1989, the region is home to an estimated 40 % of all of the mammal species found in the Amazon basin — among many other plant and animal species.

While one of our modeling studies projects a large (~ 100 %) increase in Atlantic category 4 - 5 hurricanes over the 21st century, we estimate that such an increase would not be detectable until the latter half of the century, and we still have only low confidence that such an increase will occur in the Atlantic basin, based on an updated survey of subsequent modeling studies by our and other groups.

Another hitch arose when the wrong basin taps were delivered, along with a few other parts for the shower, which set the project back by a few days.