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The Client-Centered Perspective: The clientcentered perspective of Carl Rogers stands out as the most classic example of the humanistic approach. Rogers used nondirective techniques such as active listening, empathy, congruence, and unconditional positive regard to understand and help others. Rogers felt that sincere empathy was needed in order for people to feel accepted and understood, and ultimately to enable growth to occur. Unconditional positive regard refers to the belief that no one should be negatively judged or evaluated in the therapy experience or elsewhere. Rather, respect and acceptance should prevail. Unconditional positive regard can be a challenge for professionals working with individuals who have attitudes or behaviors that one finds offensive (e.g., sexual abuse of children, stealing, racist comments). Unconditional positive regard does not mean that these behaviors or attitudes are accepted as being okay. Rather, it is the person who is fully accepted. Therefore, respect and a nonjudgmental attitude are advocated. Congruence, or genuineness, refers to harmony between one s feelings and actions. Thus, the professional should strive toward emotional honesty in his or her relationship with others. Genuineness also implies that the professional will not try to hide his or her feelings from others, yet still present a professional attitude and demeanor. Rogers was also instrumental in developing ways to assess treatment process and outcome. This included an individualized assessment technique such as the Q-sort (sorting a variety of cards with descriptive feelings into several categories) to assess functioning and outcome. The client-centered approach maintains that people have an innate drive toward growth. Because the development of the self and attempts at growth are often met with various social consequences (such as praise or punishment), individuals may develop patterns of behavior that are inconsistent with growth. For example, a parent may wish that

In some cases, however, you may want to display one of Excel s built-in dialog boxes so the end user can make the choices. There are two ways to do this: Access the Dialogs collection of the Application object. Execute a menu item directly. I discuss each of these techniques in the sections that follow.

Domain Structure There are special servers on the Internet that provide guidance to all name servers. These are known as root name servers and, as of this writing, there are nine of them. They do not contain all information about every host on the Internet, but they do provide direction as to where domains are located (the IP address of the name server for the uppermost domain a server is requesting). The root name server is the starting point to find any domain on the Internet. If access to the root servers ceased, transmission over the Internet would eventually come to a halt.

15 Thomason, L and Peter, T, eds Assessment of Stratospheric Aerosol Properties (ASAP): Stratospheric Processes and Their Role in Climate SPARC Report No 4, WCRP-124, WMO/TD-No 1295, 2006 16 Steele, HM and Hamill, P Effects of temperature and humidity on the growth and opticalproperties of sulfuric acid-water droplets in the stratosphere Journal of Aerosol Science 1981; 12(6): 517 528 17 Carslaw, KS, Peter, T and Clegg, SL Modeling the composition of liquid stratospheric aerosols Reviews of Geophysics 1997; 35(2): 125 154 18 Curtius, J, Weigel, R, Vossing, HJ, Wernli, H, Werner, A, Volk, CM, Konopka, P, Krebsbach, M, Schiller, C, Roiger, A, Schlager, H, Dreiling, V and Borrmann, S Observations of meteoric material and implications for aerosol nucleation in the winter Arctic lower stratosphere derived from in situ particle measurements.

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Atmospheric Chemistry and Physics 2005; 5: 3053 3069 19 Brock, CA, Hamill, P, Wilson, JC, Jonsson, HH and Chan, KR Particle formation in the upper tropical troposphere: a source of nuclei for the stratospheric aerosol Science 1995; 270: 1650 1653 20 Brasseur, G and Solomon, S Aeronomy of the Middle Atmosphere, 3rd edn Springer, Dordrecht, The Netherlands: 2005 21 Weisenstein, D, Bekki, S, Pitari, G, Timmreck, C and MIlls, M Modeling of stratospheric aerosols In: L Thomason and T Peter, eds Assessment of Stratospheric Aerosol Properties (ASAP) WCRP-124, WMO/TD No 1295, SPARC Report No 4, Toronto, Canada: 2006 22 Wayne, RP Chemistry of Atmospheres, 3rd edn Oxford University Press, Oxford, UK: 2000 23 MacKenzie, AR Stratospheric chemistry and transport In: CN Hewitt and A Jackson, eds Handbook of Atmospheric Science Blackwell, Oxford, UK: 2003; pp 188 210.

24 Roscoe, HK, Jones, AE and Lee, AM Midwinter start to Antarctic ozone depletion: evidence from observations and models Science 1997; 278(5335): 93 96 25 Farman, JC, Gardiner, BG and Shanklin, JD Large losses of total ozone in Antarctica reveal seasonal Clox/Nox interaction Nature 1985; 315(6016): 207 210 26 Cox, RA, MacKenzie, AR, Muller, RH, Peter, T and Crutzen, PJ Activation of stratospheric chlorine by reactions in liquid sulfuric-acid Geophysical Research Letters 1994; 21(13): 1439 1442 27 Hanson, DR, Ravishankara, AR and Solomon, S Heterogeneous reactions in sulfuric-acid aerosols a framework for model-calculations Journal of Geophysical Research Atmospheres 1994; 99(D2): 3615 3629 28 MacKenzie, AR and Haynes, PH The in uence of surface kinetics on the growth of stratospheric ice crystals Journal of Geophysical Research Atmospheres 1992; 97(D8): 8057 8064.