We obtained meteorologic data for study locations specified by longitude and latitude (to three decimal degrees) from the Oregon Climate Service PRISM data explorer for monthly high-resolution precipitation and temperature climate data (Oregon Climate Service 2008).
To prepare for increasing temperatures, climate adaptation actors are prioritizing climate resilience- and transformation-based activities.
Furthermore, Ref. [24] indicated that except for temperature, some other climate parameters such as humidity and air movement were also important to passenger thermal comfort.
Findings of the present study contribute to the understanding of the effect of climate change on areas with various land use and provide baseline conditions for temperature projection of future climate change scenarios.
This paper addresses the problem of greenhouse crop growth through a hierarchical control architecture governed by a high-level multiobjective optimization approach, where the solution to this problem is to find reference trajectories for diurnal and nocturnal temperatures (climate-related setpoints) and electrical conductivity (fertirrigation-related setpoints).
Leung and Gustafson (2005) used regional climate simulations for temperature, solar radiation, precipitation, and stagnation/ventilation, and projected worse air quality in Texas and better air quality in the Midwest in 2045 2055 compared with 1995 2005.
regressing GR t for each locality on Ta, Ts, Tw or Pa, respectively, incorporating one year delayed autoregressing (GR t -1): GR t = α + yGR t -1 + x t β where x t is the mean climate parameter for temperature and precipitation and α, β and γ are regression constants.
Climate data for these GCM-projections were generated by downscaling the change rates of monthly mean temperatures and monthly precipitation to 0.5° resolution by bi-linear interpolation and superimposing these monthly climate anomalies (absolute for temperature, relative for precipitation and cloudiness) on the 1961 1990 average of the observed climate [78,79].
The climate change parameters for temperature and rainfall were determined separately for southern and northern Europe (Christensen et al. [2011]) (Table 1).
Data generated from previous studies reveal a complex interaction of climate factors especially for temperature and humidity [ 18– 218.
