Adoption of reduced tillage management systems often leads to increased carbon content and increased percentage of WFPS in soils, which in turn may support higher rates and duration of denitrification . Also, different types of nitrogen fertilizers produce different amounts of N2O under the same reduced tillage management systems, so fertilizer-tillage interactions must also be considered . With respect to effects of water content, Dobbie and Smith found that N2O emissions from arable soils increased about 30-fold when the WFPS was increased from about 60% to 80%. Smith suggested that, contrary to expected decreases in N2O emissions with decreased precipitation, increased temperature might stimulate respiration and lead to oxygen depletion. This would, in turn, increase the anaerobic volume in soil pore spaces and consequently favor denitrification and N2O emissions. Based on these estimates, N2O emissions from both arable lands and natural ecosystems in California may be increased by rising temperature, even though it is difficult to predict the exact amount of increases of N2O emissions. Although studies indicate a positive relationship between temperature, precipitation and denitrification, the actual predictions of how N2O emissions will respond to global warming are complicated and varies between models. For example, in the Denitrification-Decomposition model and Land Use Emissions submodels , the underlying assumption is there is a positive relationship between temperature and precipitation. However,blueberry packing box the CarnegieAmes-Stanford model assumes a negative feedback on N2O emissions as a result of climate change. Since denitrification in soils is regulated by many factors, as described above, and given the paucity of data on N2O emissions, it is difficult to predict the effect of climate change on N2O emissions.
A small change of N2O concentration can lead to a large difference in global warming potential since the GWP of N2O is 300 times higher than that of CO2. Thus, studying the effect of changes in temperature and precipitation on N2O emissions is a high priority for the state . To support these efforts, more precise methods of measuring N2O emissions in the field are needed. Methane is produced by the process of methanogenesis, under strictly anaerobic conditions, by microorganisms that either using hydrogen gas as an energy source with CO2 as an electron acceptor or that ferment acetate . The process occurs in the digestive system of ruminant herbivores as well as in soils that are saturated with water and therefore depleted in oxygen. Soil with high amounts of organic matter , found in California wetlands and the Delta area, are a particular class of soil with high potential for methane production . The current estimate of wetland acreage in California, areas where Histosols are the common soil type, is approximately 450,000 acres; some of these soils are under agricultural production . Even though these soils represent 0.4% of the state’s area, the GHG emissions from these soils could surpass those of the mineral soils, due to emission rates and the high global warming potential of CH4 and N2O. Temperature, irrigation, fertilization, available carbon, and seasonal variations are among the factors that influence production of methane in soil . This section focuses on methane formation in soils. There has been little consideration of the effects of temperature and CO2 on CH4 emissions in flooded rice fields and wetlands in California. Studies from other parts of the world provide insights regarding how methane emissions may respond to climate change.Watanabe et al. reported that temperature is a major factor causing seasonal variation in CH4 emission rates during continuous flooding and that higher cumulative temperature leads to higher total CH4 emissions.
Allen et al. suggested that elevated CO2 and higher temperatures increase CH4 emissions in flooded rice soils due to greater root exudation or root sloughing mediated by increased seasonal total photosynthetic CO2 uptake. Other studies, however, have not observed positive correlations between temperature and methane emissions . Clearly, more extensive studies of gas fluxes from flooded ecosystems are needed to predict potential effects of elevated temperature and CO2 on CH4 emissions in California’s flooded rice fields and wetlands. The potential effects of climate change on GHG emissions are quite diverse and controlled by numerous factors . However, due to the longterm legacy of today’s GHG emissions, it is sensible to formulate alternatives to adapt to climate change. At present, formulating adaptation strategies for California agriculture to increasing GHGs concentrations in the atmosphere is based on theory and extrapolations from global scale assessments . Our aim should be to decrease negative impacts, promote any potential positive impacts that may result from these adaptive strategies, and reduce environmental and social pressures that increase vulnerability to climate variability . Wilkinson has identified a series of “no regret” adaptation strategies, i.e., increased water use efficiency; limiting the footprint of development on the landscape, particularly in vulnerable habitats such as wetlands and areas subject to fires, floods, and landslides; creating nature reserves designed to accommodate future climate changes and necessary range shifts and migrations of plants and animals; reducing urban heat island impacts; and using permeable pavements so that storm water runoff can be used to recharge groundwater systems . Agricultural, as well as forest and rangeland, soils have the potential to mitigate climate change by serving as sinks for GHGs due to their ability to store C in the form of organic matter. This section will now focus on agricultural management practices that can enhance the utilization of agroecosystems as GHG sinks. It will also consider how interactions among different GHG must be considered in developing management strategies.At present there is limited quantification of the mitigating effect of various agricultural practices in California . This quantification is an essential step that has to be taken towards planning, policy making and further implementation of GHG mitigation practices. A major source of uncertainty regarding GHG in California is associated with our incomplete understanding of the sources and mitigation potential of CH4 and N2O, both of which are GHG with high global warming potential. Our estimates of N2O fluxes from California agricultural soils are particularly poor and difficult to model, derived from the fact that so little data have been collected in California and that the environmental drivers of this process are not well understood. In addition, there is a need for specific research on GHG emissions from Histosols ,package of blueberries not only on current emission rates, but also on the potential that wetland restoration could have in reversing these negative impacts. The consequences of changes in management practices to achieve mitigation of GHG need to be better characterized in California soils; Table 3.2 summarizes some potential issues. This information is essential for evaluating the trade-offs of different mitigation strategies both with respect to GHG and, beyond that, with the system as a whole. This information is urgently needed to develop effective and efficacious management plans and policies. Research on some of these issues is ongoing as part of the research program of the Kearney Foundation of Soil Science.Air quality refers to the clarity, smell, and even taste of the air surrounding us. Atmospheric trace gases are involved in many interactions which determine air quality, as they are heated by solar radiation, transported by wind, and scrubbed out of the atmosphere by rain. Air quality affects climate change in two main ways: by altering the atmospheric greenhouse effect and by reducing the amount of solar radiation reaching the earth’s surface . In addition, aerosols can also have local effects , and ozone production that directly reduce crop productivity .
Air quality in California is impacted by emissions and their regulation both within and outside the state. Such regulations vary between states and regions, and countries, both in terms of their stringency and the types of emissions. Agriculture is impacted by climate change , air quality , and also by the interaction between these two phenomena . For instance, O3 formation is positively correlated to temperature, can directly interfere with plant metabolism , and can indirectly compromise symbiotic relationships within plant communities by reducing the diversity of mycorrhizal communities , and potentially their functionality. Agriculture also can be an important determinant of air quality. Recognizing agriculture’s impact on air quality, California has placed stringent regulations on agriculture, relative to the rest of the United States, to comply with the Clean Air Act of 1990. For instance, the California Air Resources Board recently tightened rules governing emissions from engine-powered irrigation pumps , to curb smog-forming constituents and GHG emissions. The direct effects of the two most prominent greenhouse gases on GWP and radiative forcing have been addressed above in Section 3. This section reviews the effects of O3, aerosols, and oxides of nitrogen on climate and agriculture in the California context.Ozone has potentially wide-ranging but only moderately well–understood effects on climate change due to the non-linear and multiplicative interactions involved in its formation. In the upper troposphere, O3 effectively reflects UV radiation, and in the lower atmosphere, in addition to being harmful to human health, O3 is a well documented phytotoxin . Ozone enters plants through stomata and disrupts biochemical functioning, leading to decreased productivity, lowered fertility, and accelerated senescence , all of which can cause significant economic losses within California croplands . Integration of agricultural crop production models and a motor-vehicle emissions model, revealed significant crop production losses in different commodities at regional and national levels. A complex series of reactions between VOCs and NOx gases , catalyzed by sunlight and heat, produce O3 . At low concentrations, tropospheric NOx causes a net destruction of O3, while at higher concentrations it causes a net production. However, global O3 production efficiency is greater at lower NOx concentrations, and anthropogenic NOx is known to contribute less than natural sources to global O3 budgets . Furthermore, background GHG concentrations, such as CO2 and CH4, could accelerate O3 formation through radiative forcing, and the ratio of NOx to VOCs can be more important in determining O3 production than absolute concentrations . This myriad of reactions can confound local air quality initiatives that do not account simultaneously for NOx and VOC concentrations as O3 precursors. Such local effects may be of particular significance to agriculture, given the phytotoxicity of O3 . The above interactions and their impacts upon agriculture are as yet poorly understood, however, it is apparent that an integrated approach to the regulation of these various atmospheric constituents affecting air quality is necessary.The preponderance of current research agrees that the overall impact of aerosols on climate change is a cooling effect, countering the warming effects of GHGs . Aerosols directly influence the climate system by absorbing and scattering solar radiation and indirectly by providing cloud condensation nuclei . An increase in cloud droplet concentrations and a reduction in cloud droplet size is often observed when clouds are fed by air with enhanced levels of CCN, creating the so called ”first indirect effect,” through which aerosols effect climate . As a result, the optical properties of clouds are rendered more reflective, and solar insolation is increased. However, the magnitude of aerosol cooling is poorly quantified; a recent study found increased solar insolation over the past 15 years, and attributed this result to improvements in air quality . Given the projected increases in the population of California and consequential aerosol production coincident with urbanization , the effects of increased CCN may be of particular significance to climate and California agriculture, especially in the Central Valley, where much of the urbanization is projected to take place. In addition to increased cloud reflectivity, an increase in CCN has been found to decrease the average radius of atmospheric liquid-water droplets, which hinders cloud droplet coalescence and retards precipitation, leading to the ‘second indirect effect’ through which aerosols effect climate . Thus, aerosols can decrease the precipitation efficiency of clouds, notably decreasing incidence and amounts of precipitation . Increased aerosol concentrations downwind of major urban centers in both California and Israel are suggested to have reduced precipitation by 15%-25% during the last several decades, based upon calculations of the orographic enhancement factor using a time course of precipitation data downwind and side wind of urbanized areas .