Not exact matches
Among the factors that could cause actual results to differ materially are the following: (1) worldwide economic, political, and capital markets conditions and
other factors beyond the Company's control, including natural and
other disasters or
climate change affecting the operations
of the Company or its customers and suppliers; (2) the Company's credit ratings and its cost
of capital; (3) competitive conditions and customer preferences; (4) foreign currency exchange rates and fluctuations in those rates; (5) the timing and market acceptance
of new product offerings; (6) the availability and cost
of purchased
components, compounds, raw materials and energy (including oil and natural gas and their derivatives) due to shortages, increased demand or supply interruptions (including those caused by natural and
other disasters and
other events); (7) the impact
of acquisitions, strategic alliances, divestitures, and
other unusual events resulting from portfolio management actions and
other evolving business strategies, and possible organizational restructuring; (8) generating fewer productivity improvements than estimated; (9) unanticipated problems or delays with the phased implementation
of a global enterprise resource planning (ERP)
system, or security breaches and
other disruptions to the Company's information technology infrastructure; (10) financial market risks that may affect the Company's funding obligations under defined benefit pension and postretirement plans; and (11) legal proceedings, including significant developments that could occur in the legal and regulatory proceedings described in the Company's Annual Report on Form 10 - K for the year ended Dec. 31, 2017, and any subsequent quarterly reports on Form 10 - Q (the «Reports»).
A large number
of additional observations are broadly consistent with the observed warming and reflect a flow
of heat from the atmosphere into
other components of the
climate system.
Similar to the model development process adopted for
other components of the
climate system, this strategy is composed
of four stages, each one building on the next.
[45]
Other features include a 42.4 kWh liquid cooled lithium - ion battery pack, a need - based energy management
system, LED technology used for all lighting units, independent cooling
system for each axle; doors, covers, sidewalls and roof in carbon fibre - reinforced plastic; 3 - mode flush gear selector (forward, reverse and neutral), instrument cluster with fold - out central display with integrated Audi MMI functions,
climate control unit located to the right above the steering wheel, racing - inspired lightweight bucket seats, snow white and cognac interior colours, heat pump,
climate control
system; triangular double wishbones at the front axle and trapezoidal wishbones made
of forged aluminum
components at the rear axle, direct rack - and - pinion steering with speed - sensitive electromechanical steering boost, 235 / 35R19 front and 295 / 30R19 rear tires with a new blade design and the prototype version
of an information processing
system (car - to - x communication).
It is, however, the variability on large scales influenced by interactions
of the atmosphere with
other components of the
climate system that is predictable.
Other nonradiative forcings modify the biological
components of the
climate system by changing the fluxes
of trace gases and heat between vegetation, soils, and the atmosphere and by modifying the amount and types
of vegetation.
In
other words, they fail the most basic type
of test imaginable; and in the words
of Li et al., this finding suggests that «global
climate models should better integrate the biological, chemical, and physical
components of the earth
system.»
A further unknown is exactly how the exchange
of heat and gases between the atmosphere and
other components of the
climate system takes place.
The new report further states that greenhouse gas emissions at or above current rates would induce changes in the oceans, ice caps, glaciers, the biosphere, and
other components of the
climate system.
Given the increased levels
of certainty regarding human - induced global warming (from 90 to 95 %), more robust projections on sea - level rise and data on melting
of ice sheets, and the «carbon budget» for staying below the 2 °C target, the WGI conclusions together with
other AR5
component reports are likely to put more pressure on the UNFCCC parties to deliver by 2015 an ambitious agreement that is capable
of preventing dangerous anthropogenic interference with the
climate system.
Requires such group, within a year and every four years thereafter, to submit to Congress a report that: identifies gaps in data and recommends actions to fill those gaps; proposes a coordinated strategy for funding and allocating responsibilities among federal agencies for
climate and
other global change data collection, management, and retention; recommends a federal capital investment strategy; and evaluates optimal design
of observation
system components to ensure a cost - effective, adequate set
of observations detecting and tracking global change.
It is for this reason that the scenario framework distinguishes between «pathways,» which describe one
component (such as RCPs or SSPs)
of integrated scenarios, and «scenarios» themselves, which combine pathways with
other information such as emissions,
climate projections and policy assumptions to produce integrated descriptions
of future
climate and human
system development.
The intent
of downscaling is to achieve accurate, higher spatial resolution
of weather and
other components of the
climate system than is achievable with the coarser spatial resolution global model.
And, even tho we may safely assume you are referring to radiative energy transport in the Earth's atmosphere, the interactions
of that energy with all
other components of the Earth's
climate system are the critically important aspects.
Water vapor and clouds, on the
other hand, are highly active
components of the
climate system that re-spond rapidly to changes in temperature and air pressure by evaporating, condensing, and precip - itating.»
Given the complexities
of the
climate system, I would say the chance
of any single
component of that
system having a long term warming impact all by itself, in a manner that effectively negates all
other components, is highly unlikely — especially when that one
component makes up a bare.04 %
of just one
of the subsystems making up the overall
climate system, and further, when human burning
of fossil fuels contributes a mere 3 - 4 %
of that.04 %.
And Nic and Lewis just said: «Heat uptake by
other components of the
climate system is ignored»
If observed warming is attributed to CO2 and there are
other, unknown,
components of the
climate system, the parameterisation will be incorrect.
However there is lots to play for in the individual
components of the
climate system and for that reason I am loth to criticise the work
of any
other climate sceptics.
Since the late 1970s,
other data from Earth - observation satellites have been used to provide a wide range
of global observations
of various
components of the
climate system.
Following the trend in global modelling, RCMs are increasingly coupled interactively with
other components of the
climate system, such as regional ocean and sea ice (e.g., Bailey and Lynch 2000; Döscher et al., 2002; Rinke et al., 2003; Bailey et al., 2004; Meier et al., 2004; Sasaki et al., 2006a), hydrology, and with interactive vegetation (Gao and Yu, 1998; Xue et al., 2000).
Such decadal temperature fluctuations in the SPNA are strongly correlated with
other components of the
climate system, for example, Atlantic hurricane activity, North American and European river flow, and rainfall over the African Sahel and northeast Brazil.
In the rest
of this analysis I deal with the question
of to what extent the model simulations used by Shindell can be regarded as providing reliable information about how the real
climate system responds to forcing from aerosols, ozone and
other forcing
components.
The workshop was organized to allow participants to take a global perspective and consider the influence
of the Arctic in the context
of forcing from
other components of the
climate system, such as changes in the tropics, ocean circulation, and mid-latitude sea surface temperature.
But just as «The appropriate uncertainty that exists in one area
of climate modeling doe not automatically translate to all
other components of the
climate system.»
What about
other component's
of the Earth's
climate system?
; What about
other components of the Earth's
climate system?
The interactions between a recovering ozone hole, increasing greenhouse gases, ocean currents, and
other components of the
climate system must still be explored in order to better understand how the Earth's
climate will change in the future.
Other components of the
climate system, such as the ocean and the large ice sheets, tend to operate on longer time scales.
The Introduction to Levitus et al (2005) begins: Based on the physical properties and mass
of the world ocean as compared to
other components of Earth's
climate system, Rossby [1959]...