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Adaptive management implies a system in which policy and practice are constantly revised in a continuous circular process to accommodate new ecological knowledge. In the case of current fish stocking practices, there is an evident gap between science and practice indicating a lack of adaptability. While fish stocking is perceived as a solution to many problems of modern fishery management, scientific researchers warn that current practices, including introducing alien populations, seriously threaten the sustainability of fish stocks. The aim of this study was to address, explain the existence of and, finally, discuss the prospect of narrowing this gap. For this purpose, the characteristics of the policy subsystem were analyzed. The empirical findings highlight the wickedness of the policy problem. The substantial and institutional uncertainties surrounding the issue are proposed as the main reasons for the deficits in adaptability. Fish stocking decisions are made within a complex policy subsystem that involves multiple actors and policy-making institutions, conflicting goals and competing notions of the problem. Cross-coalition learning—learning between coalitions of actors with different problem definitions, forming a joint view—is a necessary and, in the case of fish stocking, lacking variable in the adaptive management process. 相似文献
2.
Bj?rn Sandstr?m Hans Annersten Eva-Lena Tullborg 《International Journal of Earth Sciences》2010,99(1):1-25
Red-staining of rocks due to fluid–rock interaction during hydrothermal circulation in fractures is a common feature in crystalline
sequences. In this study, red-stained metagranitic rock adjacent to fractures in Forsmark, central Sweden, has been studied
with emphasis on the mineral reactions and associated element mobility occurring during the alteration. The main mineral reactions
associated with the hydrothermal alteration are an almost complete saussuritization of plagioclase accompanied by total chloritization
of biotite. Magnetite has been partly replaced by hematite whereas quartz and K-feldspar were relatively unaffected by the
hydrothermal alteration. We show that redistribution of elements on the whole rock scale was very limited and is mainly manifested
by enrichment of Na2O and volatiles and depletion of CaO, FeO and SiO2 in the red-stained rock. However, on the microscale, element redistribution was more extensive, with both intragranular and
intergranular migration of e.g. Ca, K, Na, Al, Si, Fe, Ba, Cs, Rb, Sr, Ti and REEs. The altered rock shows a shift towards
higher total oxidation factors, but the change is smaller than 1σ and the red-staining of the rock is due to hematite dissemination
rather than a significant oxidation of the rock. An increase in the connected porosity is also observed in the altered rock. 相似文献
3.
The objective of this study was to investigate the possible links between regional climate, fire and vegetation at the small spatial scale during the early and mid Holocene in southern Sweden using pollen, plant macrofossil and charcoal records from a small bog. The fire history was compared with climate reconstructions inferred from various proxy records in the study region. High fire activity is related to dry and warm climate around 8550, 7600, 5500–5100 and 4500 cal. a BC. Low fire activity ca. 6500–6000 and 4750 BC may correspond to the widespread ‘8.2 k event’ (ca. 6200 BC) recorded across the North Atlantic region, and a later, brief period of increased precipitation, respectively. The decrease in broadleaved trees culminating ca. 6500–6000 BC correlates with the ‘8.2 k event’. A long mid Holocene period with low fire activity (ca. 4350–1000 BC) agrees with the pattern emerging for Europe from the global charcoal database, and may correspond to generally wetter and cooler conditions. High fire activity ca. 8550 BC probably triggered the local establishment of Corylus. Warmer and drier conditions (and high fire activity) ca. 7600 BC might have favoured the establishment of Alnus, Quercus and Tilia. The fire‐adapted Pinus maintained important populations throughout the early and mid Holocene. Copyright © 2008 John Wiley & Sons, Ltd. 相似文献
4.
Hyein Park Chul E. Chung Annica M. L. Ekman Jung-Ok Choi 《Asia-Pacific Journal of Atmospheric Sciences》2014,50(3):377-390
This study examines and evaluates simulated aerosol optical depth (AOD) and fine-mode AOD (fAOD) from the ACCMIP and CMIP5 global model archives. Satellite data nudged to AERONET data are used to construct reliable global observations of AOD and fAOD for validating the simulations. The difference in simulated global average AOD among models is of the order of a factor of 2, and the difference is even larger (～factor of 3) for fAOD. Compared to the observations, the models tend to underestimate AOD and fAOD significantly over eastern China. Another important discrepancy is that the models show larger fAOD over the Indus-Ganga Plain in summer than in winter, whereas the observations display an opposite feature. The models also overestimate the fAOD over the biomass burning regions of central Africa in DJF and underestimate the fAOD over the biomass burning regions of southern Africa in JJA. To evaluate the effect of the discrepancy between modeled and observed fAOD on aerosol direct radiative forcing, an offline radiation model is utilized. Comparing the model-fAODderived fine-mode forcing with the fine-mode forcing derived from the fAOD observation, the models tend to give too large (negative) value. This result implies that the calculated anthropogenic aerosol forcing in ACCMIP and CMIP5 models has a negative bias. 相似文献
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The coupled climate model EC-Earth2 is used to investigate the impact of direct radiative effects of aerosols on stationary waves in the northern hemisphere wintertime circulation. The direct effect of aerosols is simulated by introducing prescribed mixing ratios of different aerosol compounds representing pre-industrial and present-day conditions, no indirect effects are included. In the EC-Earth2 results, the surface temperature response is uncorrelated with the highly asymmetric aerosol radiative forcing pattern. Instead, the anomalous extratropical temperature field bears a strong resemblance to the aerosol-induced changes in the stationary-wave pattern. It is demonstrated that the main features of the wave pattern of EC-Earth2 can be replicated by a linear, baroclinic model forced with latent heat changes corresponding to the anomalous convective precipitation generated by EC-Earth2. The tropical latent heat release is an effective means of generating stationary wave trains that propagate into the extratropics. Hence, the results of the present study indicate that aerosol-induced convective precipitation anomalies govern the extratropical wave-field changes, and that the far-field temperature response dominates over local effects of aerosol radiative forcing. 相似文献
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Swedish fish stocking policy constitutes an example of the disparate challenges associated with adaptive management theory and the realization thereof. The vast substantial and institutional uncertainties of the policy subsystem have previously been identified as variables that complicate the realization of adaptive policy making. The aim of this paper is to address and tentatively explain differences in regards to how these uncertainties are handled. What regional variances in Swedish fish stocking policy can be distinguished and how can these variations be explained? The empirical analysis shows that Swedish fish stocking policy consists of a wide array of different regional policies. These regional variations are explained by differences in existing implementation resources, policy beliefs and readings of formal regulations. Policy makers can decrease these divergences in two ways; they can either change formal regulations or influence available implementation resources. Both management approaches might have positive as well as negative effects on the subsystem's adaptability. 相似文献
7.
Klas Sandström 《GeoJournal》1995,35(4):539-546
After several decades of catchment research, most forest hydrologists agree that deforestation leads to increased annual catchment yields and augment groundwater recharge and dry-season flow. Nevertheless, millions of people in the semi-arid tropics have good reasons — a deep knowledge of the land after using it for many generations — to state the very opposite, ie that deforestation implies dry springs and streams. In this paper a model is presented which attemps to show that both of the above views are correct, but only if the hydrological consequences of deforestation are related to the diversity in land management, hydroclimate and landscape characteristics. The possibility of closing the dichotomy of opinion between people and professionals is discussed. 相似文献
8.
Based on Norwegian and Swedish representative national samples, and samples from areas with large mammalian carnivores present, we investigated whether well-known predictors for approval of wolves may explain between-country differences. Swedes were in general more positive than Norwegians were, while respondents in large carnivore areas, regardless of nationality, were less positive. The profile of those who approved wolf presence was the same in all samples. The difference between the samples was greater in Sweden, indicating that the relationship between urbanized and rural areas is more polarized in Sweden compared to Norway. We suggest this to be an effect of the fact that Norway’s large carnivore and agriculture policies favor the rural population, and of a higher degree of urbanization in Sweden. We recommend future studies to look into the different power relations between people living in urban and rural areas, comparing countries with different degree of urbanization. 相似文献
9.
The radiative flux perturbations and subsequent temperature responses in relation to the eruption of Mount Pinatubo in 1991
are studied in the ten general circulation models incorporated in the Coupled Model Intercomparison Project, phase 3 (CMIP3),
that include a parameterization of volcanic aerosol. Models and observations show decreases in global mean temperature of
up to 0.5 K, in response to radiative perturbations of up to 10 W m−2, averaged over the tropics. The time scale representing the delay between radiative perturbation and temperature response
is determined by the slow ocean response, and is estimated to be centered around 4 months in the models. Although the magniude
of the temperature response to a volcanic eruption has previously been used as an indicator of equilibrium climate sensitivity
in models, we find these two quantities to be only weakly correlated. This may partly be due to the fact that the size of
the volcano-induced radiative perturbation varies among the models. It is found that the magnitude of the modelled radiative
perturbation increases with decreasing climate sensitivity, with the exception of one outlying model. Therefore, we scale
the temperature perturbation by the radiative perturbation in each model, and use the ratio between the integrated temperature
perturbation and the integrated radiative perturbation as a measure of sensitivity to volcanic forcing. This ratio is found
to be well correlated with the model climate sensitivity, more sensitive models having a larger ratio. Further, if this correspondence
between “volcanic sensitivity” and sensitivity to CO2 forcing is a feature not only among the models, but also of the real climate system, the alleged linear relation can be used
to estimate the real climate sensitivity. The observational value of the ratio signifying volcanic sensitivity is hereby estimated
to correspond to an equilibrium climate sensitivity, i.e. equilibrium temperature increase due to a doubling of the CO2 concentration, between 1.7 and 4.1 K. Several sources of uncertainty reside in the method applied, and it is pointed out
that additional model output, related to ocean heat storage and radiative forcing, could refine the analysis, as could reduced
uncertainty in the observational record, of temperature as well as forcing. 相似文献
10.
Katarina Hansson-Forman Elsa Reimerson Annelie Sjölander-Lindqvist Camilla Sandström 《社会与自然资源》2018,31(7):837-852
The governance of large carnivores is often surrounded by conflicts. Along with the difficulties of governing large carnivores through centralized, top-down governing and a general shift towards participatory approaches in natural resource governance, this has led many countries to establish various collaborative measures in large carnivore governance – often presented as a catch-all solution to problems of legitimacy, democratic deficit and effectiveness. However, the field of large carnivore governance currently lacks a coherent understanding of strengths and weaknesses of different kinds of collaborative arrangements. In this paper, we address this knowledge gap. Using the framework of modes of governance to categorize and compare the governance of large carnivores in Norway, Sweden and Finland, we discuss the potential and limitations of various governance modes and identify gaps in contemporary research literature. The main conclusion is that all three governance systems need to incorporate more interactive governance elements. 相似文献
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