Download e-book for iPad: High Performance Drupal: Fast and Scalable Designs by Jeff Sheltren, Narayan Newton, Nathaniel Catchpole

By Jeff Sheltren, Narayan Newton, Nathaniel Catchpole

How are you able to aid your Drupal site proceed to accomplish on the maximum point because it grows to fulfill call for? This accomplished consultant presents top practices, examples, and in-depth reasons for fixing a number of functionality and scalability concerns. You’ll how to follow coding and infrastructure concepts to Drupal internals, software functionality, databases, internet servers, and function analysis.

overlaying Drupal models 7 and eight, this publication is the appropriate reference for every thing from web site deployment to enforcing particular applied sciences reminiscent of Varnish, memcache, or Solr. in case you have a easy realizing of Drupal and the Linux-Apache-MySQL-PHP (LAMP) stack, you’re able to get started.
• identify a functionality baseline and outline objectives for development
• Optimize your website’s code and front-end functionality
• Get most sensible and worst practices for customizing Drupal middle performance
• practice infrastructure layout options to release or extend a website
• Use instruments to configure, visual display unit, and optimize MySQL functionality
• hire replacement garage and backend seek thoughts as your web site grows
• song your internet servers via httpd and Hypertext Preprocessor configuration
• video display providers and practice load checks to capture difficulties prior to they turn into serious

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Extra info for High Performance Drupal: Fast and Scalable Designs

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The thermocline is dynamically active during the ENSO cycle and is key to its evolution. Upwelling: Upward movement of cold ocean water from depth, which in the equatorial Pacific is driven by the easterly from the east trade winds. Upwelling acts to cool the surface and supply nutrients to surface ecosystems. Surface zonal current: The mean easterly trade winds drive a surface easterly current that pushes warm surface waters into the west Pacific. When the trades weaken during El Niño, the warm west Pacific water sloshes eastward, weakening the zonal SST contrast across the Pacific and thus further weakening the trades—a positive feedback for the ENSO cycle.

The atmosphere. In: K. , Climate Systems Modeling. Sponsored Jointly by UCAR and the Electric Power Research Institute (EPRI). : Cambridge University Press, pp. 53–115. V. 2000. An Introduction to Thermal Physics. San Francisco, CA: AddisonWesley, pp. 305–307. , Tsushima, Y. et al. 2010a. Relative humidity changes in a warmer climate. Journal of Geophysical Research 115: D09104. G. 2010b. Tropospheric water vapor, convection, and climate. Reviews of Geophysics 48: RG2001. Smil, V. 2003. The Earth’s Biosphere: Evolution, Dynamics, and Change.

15 The long-term mean global hydrological cycle. , surface flow) are given in 103 km3/year. E. , J. ) 22 Climate Change and Water Resources Water in oceans and lakes is, of course liquid; but it is solid ice in glaciers, and gaseous water vapor in the atmosphere. Flows or pathways are the routes water takes between reservoirs. Evaporation moves water from the oceans to the atmosphere. Precipitation moves liquid (rain) or solid (snow) water from the sky back to the Earth’s surface. Snowmelt runoff turns solid water into a liquid that flows down rivers to the sea.

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High Performance Drupal: Fast and Scalable Designs by Jeff Sheltren, Narayan Newton, Nathaniel Catchpole


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