Sentences with phrase «rind et»

Special Projects include examination of controversial meta - analysis by Rind et al., and examination of the use of «parental alienation syndrome» by the courts.

AR4 2007 — Ch 10.3.5.6 «A plausible explanation for the cause of the upward NAM trend simulated by the models is an intensifi cation of the polar vortex resulting from both tropospheric warming and stratospheric cooling mainly due to the increase in greenhouse gases (Shindell et al., 2001; Sigmond et al., 2004; Rind et al., 2005 a).»

Anomalies in the volcanic - aerosol induced global radiative heating distribution can force signifi cant changes in atmospheric circulation, for example, perturbing the equator - to - pole heating gradient (Stenchikov et al., 2002; Ramaswamy et al., 2006a; see Section 9.2) and forcing a positive phase of the Arctic Oscillation that in turn causes a counterintuitive boreal winter warming at middle and high latitudes over Eurasia and North America (Perlwitz and Graf, 2001; Stenchikov et al., 2002,2004, 2006; Shindell et al., 2003b, 2004; Perlwitz and Harnik, 2003; Rind et al., 2005; Miller et al., 2006).

This assumption has been questioned on the basis of both observational and model - simulated data suggesting that tropical to extratropical climate variability can be decoupled (Rind et al., 2005), and also that extratropical teleconnections associated with ENSO may vary through time (see Section 6.5.6).

Corrections: Del Genio et al. (1991); Raval and Ramanathan (1989) found that satellite infrared measurements gave «compelling evidence for the positive feedback between surface temperature, water vapour and the greenhouse effect; the magnitude of the feedback is consistent with that predicted by climate models;» similarly, Rind et al. (1991), p. 500; Sun and Held (1996); and the final nail in the coffin, Soden et.

A computer model by Bryan (1986) supported this, but another model found that a cold North Atlantic surface sufficed to bring a Younger Dryas - like climate, Rind et al. (1986).

Convection is expected to intensify as climate warms (Rind et al., 2001), although this might not be the case in the tropics (Stevenson et al., 2005).

Anomalies in the volcanic - aerosol induced global radiative heating distribution can force significant changes in atmospheric circulation, for example, perturbing the equator - to - pole heating gradient (Stenchikov et al., 2002; Ramaswamy et al., 2006a; see Section 9.2) and forcing a positive phase of the Arctic Oscillation that in turn causes a counterintuitive boreal winter warming at middle and high latitudes over Eurasia and North America (Perlwitz and Graf, 2001; Stenchikov et al., 2002, 2004, 2006; Shindell et al., 2003b, 2004; Perlwitz and Harnik, 2003; Rind et al., 2005; Miller et al., 2006).

NASA group: Hansen et al. (1989); Rind et al. (1990).

Not exact matches

Store bought pork rinds are an acceptable substitute if you can't fry your own (Baken - Ets or Mac's are easy to find).

The Humour award for Monckton et al mentioned @ 147 actually involves a paper co-authored by one of our hosts — Lacis, Schmidt, Rind & Ruedy (2010) «Atmospheric CO2: Principal Control Knob Governing Earth's Temperature.»

The studies are Meehl et al. 2004 (M04, blue), Stone et al. 2007 (S07, red), Lean and Rind 2008 (LR08, green), and Huber and Knutti 2011 (HK11, purple).

Rind, D.G., et al., 2001: Effects of glacial meltwater in the GISS Coupled Atmosphere - Ocean model: Part II.

The mid-Holocene (6000 years ago) and Last Glacial Maximum (~ 20,000 years ago) are also attractive targets of model validation, and while some successes have been noted (i.e. Joussaume et al, 1999, Rind and Peteet, 1985) there is still some uncertainty in the forcings and response.

The Humour award for Monckton et al mentioned @ 147 actually involves a paper co-authored by one of our hosts — Lacis, Schmidt, Rind & Ruedy (2010) «Atmospheric CO2: Principal Control Knob Governing Earth's Temperature.»

Rind, D., et al. (1986).

Figure 3: Percent contributions of various effects to the observed global surface warming over the past 50 - 65 years according to Tett et al. 2000 (T00, dark blue), Meehl et al. 2004 (M04, red), Stone et al. 2007 (S07, green), Lean and Rind 2008 (LR08, purple), Huber and Knutti 2011 (HK11, light blue), Gillett et al. 2012 (G12, orange), and Wigley and Santer 2012 (WS12, dark green).

On the attribution question, the results of Gillett et al. are consistent with the many other attribution studies we've looked at (i.e. Lean and Rind 2008, Huber and Knutti 2011, and Foster and Rahmstorf 2011)- namely that humans have been the dominant cause of the global warming over the past 25 - 150 years (Figure 1).

Percent contributions of various effects to the observed global surface warming over the past 50 - 65 years according to Tett et al. 2000 (T00, dark blue), Meehl et al. 2004 (M04, red), Stone et al. 2007 (S07, green), Lean and Rind 2008 (LR08, purple), Huber and Knutti 2011 (HK11, light blue), and Gillett et al. 2012 (G12, orange).

Figure 5: Net human and natural percent contributions to the observed global surface warming over the past 50 - 65 years according to Tett et al. 2000 (T00, dark blue), Meehl et al. 2004 (M04, red), Stone et al. 2007 (S07, green), Lean and Rind 2008 (LR08, purple), Huber and Knutti 2011 (HK11, light blue), and Gillett et al. 2012 (G12, orange).

Figure 1: Net human and natural percent contributions to the observed global surface warming over the past 50 - 65 years according to Tett et al. 2000 (T00, dark blue), Meehl et al. 2004 (M04, red), Stone et al. 2007 (S07, light green), Lean and Rind 2008 (LR08, purple), Huber and Knutti 2011 (HK11, light blue), Gillett et al. 2012 (G12, orange), Wigley and Santer 2012 (WS12, dark green), and Jones et al. 2013 (J12, pink).

Alternatively, it may be the result of increased ocean heat transports due to either an enhanced thermohaline circulation (Raymo et al., 1989; Rind and Chandler, 1991) or increased flow of surface ocean currents due to greater wind stresses (Ravelo et al., 1997; Haywood et al., 2000), or associated with the reduced extent of land and sea ice (Jansen et al., 2000; Knies et al., 2002; Haywood et al., 2005).

The studies are Tett et al. 2000 (T00, dark blue), Meehl et al. 2004 (M04, red), Stone et al. 2007 (S07, green), Lean and Rind 2008 (LR08, purple), Huber and Knutti 2011 (HK11, light blue), Gillett et al. 2012 (G12, orange), Wigley and Santer 2012 (WG12, dark green), Jones et al. 2013 (J13, pink), IPCC AR5 (IPCC, light green), and Ribes et al. 2016 (R16, light purple).

Stratosphere and ultraviolet: Haigh (1994); Rind and Balachandran (1995); Haigh (1996); McCormack et al. (1997); Shindell et al. (1999); Labitzke and van Loon (1999); for discussion, see Wallace and Thompson (2002); more recently, White (2006).

Studies such as Tett et al. 2000, Lean and Rind 2008, Jones et al. 2013, and more prove that human contribution to climate change is ore than minimal.

Figure 1: Percent contributions of greenhouse gases (GHGs), sulfur dioxide (SO2), the sun, volcanoes, and El Niño Southern Oscillation (ENSO) to the observed global surface warming over the past 50 - 65 years according to Tett et al. 2000 (T00, dark blue), Meehl et al. 2004 (M04, red), Stone et al. 2007 (S07, green), Lean and Rind 2008 (LR08, purple), Huber and Knutti 2011 (HK11, light blue), Gillett et al. 2012 (G12, orange), and Wigley and Santer 2012 (WS12, dark green).

1986 D. Rind, et al., «The Impact of Cold North Atlantic Sea Surface Temperatures on Climate: Implications for the Younger Dryas.»