13 results were found for 김천리얼폰팅《모든톡@secs4》모든톡@secs4 김천결혼 김천대학생•김천야한대화㉹김천교제 ヾ劒 surprisingly.

Results:

• 1. Increased glacial melt due to volcanic ash

  /hydrology/articles/nr/2110

• 2. Group5-Draft_report

  process. Although the time frame given in the task refers to 20 years in the foreseeable future, we--- as a compulsory part of the competent authority (leading agency), who is entitled the legal mandate to facilitate implementation of stakeholder involvement and ultimate performance of the outcome of the adaptation plan--- will not confine ourselves to the predefined time frame due /media/loftslag/Group5-Draft_report.pdf

• 3. CES_D2.4_solar_CMIP3

  for a more distant period, 2070-2099. Maps for that period are presented in the appendix (Figs. A1-A6). Qualitatively, the geographical distributions are similar to those for the period 2020-2049 but the amplitude of the response is stronger, the A2 scenario producing the strongest, the B1 scenario the weakest response. 4 UNCERTAINTY ANALYSIS Probability distributions for the insolation change /media/ces/CES_D2.4_solar_CMIP3.pdf

• 4. Adalgeirsdottir-etal-tc-5-961-2011

  Av. Ed. Belin, 31400 Toulouse, France Received: 21 March 2011 – Published in The Cryosphere Discuss.: 6 April 2011 Revised: 5 October 2011 – Accepted: 20 October 2011 – Published: 2 November 2011 Abstract. The Little Ice Age maximum extent of glaciers in Iceland was reached about 1890 AD and most glaciers in the country have retreated during the 20th century. A model for the surface mass balance /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 5. CES_D2.4_task1

  about 20-25% in 2010 to about 50% in 2050. Perhaps surprisingly, a particularly high probability is found in Iceland, most likely as a result of the small 12 interannual variability there. As expected, the probability of very warn years rises even faster than that of warm months – in northern Europe from typically 30-40% in 2010 to about 60- 80% in 2030 and to 85-95% or even more in 2050 /media/ces/CES_D2.4_task1.pdf

• 6. Eriksson_Garvill_Nordlund_2006

  (see e.g. Steg, 2003). In studies from several countries, push measures are perceived as less acceptable compared to pull measures (e.g. Ho¨lzer, 2003; Rienstra, Rietveld, & Verhoef, 1999; Steg & Vlek, 1997). For example, in a European study, over 90% of the car users supported improved public transport and park-and-ride schemes, while less than 20% approved of reduced parking space and cordon /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 7. Kok_JGEC658_2009

  it will be one of the main aspects of this paper. 2.3. Properties The elements of a Fuzzy Cognitive Map are as follows:  Concepts: C1, C2, . . ., Cn. These represent the drivers and constraints that are considered of importance to the issue under consideration.  State vector: A = (a1, a2, . . ., an), where ai denotes the state of the node Ci. The state vector represents the value of the concepts /media/loftslag/Kok_JGEC658_2009.pdf

• 8. Lorenzoni_Pidgeon_2006

  their lifestyles for this purpose. Of those who would be prepared to change their way of living, most (92% to 96%) favoured options that could be easily undertaken in the home, and that would cost almost nothing, like recycling and using less energy. Fewer favoured reducing their private transport (68% would use the car less; 62% would take fewer flights), whilst price increases were not popular (only 37 /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 9. 2010_012rs

  thus enabling the delineation of active faults in near-real time. Foreshocks preceding a large earthquake by more than 20 minutes will already have been located with high precision before the main shock occurs, and may already have delineated the fault plane of the coming main shock, thus allowing its faulting mechanism to be immediately inferred. Due to its size, the main shock /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 10. VI_2014_001

  6 0 20 40 60 80 10 0 12 0 14 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm51 heM 95?bh ??Obs 95?bh ??W aSiM 95?bh heM Annual max. Q : GEV Distributions for vhm51 Index flood model no. 6 l l l l l l l l l l l l l l l l l l −2 0 2 4 6 0 50 10 0 15 0 −ln(−ln(1−1/T)) Q( T) (m ?s) 1 2 5 10 20 50 100 T (years) l Obs. WaSiM vhm52 heM 95?bh Obs 95?bh /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf