The difference waves were calculated for RC − congruent, SC − con

The difference waves were calculated for RC − congruent, SC − congruent and RC − SC. A repeated measures ANOVA was performed for group (3) × difference wave (3). A topographical analysis was also performed to further quantify the

differences between the three groups. Based on observations of the topographical differences between the three groups a series of electrode pools were used to capture this difference. The mean amplitude of the difference waves between 400 and 500 msec was examined at three central and parietal pools (central: 129, 31, 54, 55, 80, 79; left parietal: 58, 59, 65; right parietal: 91, 90, 96) (see Fig. 1B). A repeated measures ANOVA was performed for group (3) × congruency (3) × pool (3). The LRP was calculated according to convention (Coles, 1989): [(ER − EL) left hand response + (EL − ER) right hand response]/2. ER represents www.selleckchem.com/products/s-gsk1349572.html the amplitude of the ERP at the electrode over the right motor cortex, whereas EL represents the

amplitude of the ERP at the electrode over the left motor cortex. The left and right motor cortex electrodes were electrodes 36 and 104 respectively. These have the equivalent of positions C3 and C4 in the traditional 10–20 electrode system. The raw LRP waveforms were smoothed using a 50 msec moving average window to improve signal to noise ratio. The peak latency and peak amplitude of stimulus locked LRPs were calculated from 250 to 600 msec. Response locked LRPs’ peak amplitude, latency and mean amplitude were examined between −300 msec

and 0 msec relative to response. A repeated measures ANOVA of congruency (3) × group (3) was buy Lumacaftor done on the peak latencies and peak amplitudes. As the peak amplitude of the LRP can be variable particularly in developmental studies (Bryce et al., 2011) the mean amplitude of the LRP was also calculated with separate time periods for each group based on group differences in the mean RT data. In order to accurately detect the initiation of response selection the stimulus locked LRP peak latency was matched with Calpain the proportional change in RT in the three age groups. As the stimulus locked LRP tends to peak between 400 and 600 msec after stimulus onset young adults were examined between this time point. Adolescents RT was 45 msec faster than young adults therefore the LRP was examined 45 sec earlier than in young adults (355–555 msec). Middle age adults were 34 sec slower than young adults therefore the LRP was examined from 434 to 634 msec relative to stimulus onset. EEG data were processed using Brain Vision Analyzer (Brain Products, Munich), Matlab 7.9, SPSS 17.0 and Statistica 9. LRP jackknifing is a procedure commonly used in the LRP literature as it is thought to provide a more accurate estimate of LRP onset latencies (Lansbergen et al., 2007 and Miller et al., 1998; Wild-Wall, Falkenstein, & Hohnsbein, 2008).

However, our comprehensive predictions were different in some

However, our comprehensive predictions were different in some

respects from those previously reported [23]. Firstly, our results demonstrated that the content of β-strands in α-gliadins was relatively PD0325901 low and that only 67.68% of α-gliadins contained a β-strand (S) or two β-strands (S, SE) in the C-terminal unique domain II; moreover, in general, only 2 to 4 amino acid residues were involved in each β-strand. Secondly, our comparative analysis revealed that more α-helices usually occurred in the unique domain I (H2, H3, H4 and HE2) rather than the C-terminal unique domain II (H5, HE4). Finally, though our results also indicated that the secondary structure was seldom present in the N-terminal repetitive domain, a conserved α-helix or even two α-helices were invariably present in the glutamine repeat I (H1) in all 198 predicted genes. Because the older version was not available, to our knowledge, the only explanation for these discrepancies appears to be the difference in PSIPRED versions used in the respective studies. Generally, it has been suggested that, for the α-gliadins, a long repetitive domain, a high proportion of glutamine residues

and an extra cysteine residue in the primary structure, and more α-helices and β-strands in the secondary structure, exert a positive effect on gluten quality [37], [38], [39] and [40]. Our results also support this view, not only for the above-mentioned three genes (protein IDs ABQ96115, IPI-145 concentration ABQ96118 and ABQ96119) that harbor an extremely large glutamine repeat I and could Florfenicol form one or even two significant longer α-helices H1 in this region, but also for some of the genes with an extra cysteine residue in the C-terminal unique domain II, which also probably formed an extra α-helix HE4 or β-strand SE involving the peptides precisely around the sites where an extra cysteine residue most likely occurred. Accordingly,

on the basis of our comprehensive prediction, we propose that the two unique domains were the most important regions for the function of α-gliadins, whereas in some cases the glutamine repeats would also contribute. In addition, the marked influence on gluten quality of protein subunit ACX71610 identified in vitro and the marked similarity of Z4A-14 to ACX71610 in primary and secondary structure strongly suggest that Z4A-14 is closely associated with the high quality of common wheat cultivar Zhengmai 004. The marked genomic differences in the occurrence of the four major T-cell immunogenic peptides and the average lengths of the two polyglutamine domains, combined with the complete amino acid sequences, make the reliable determination of chromosomal location of the α-gliadin genes feasible [23].

However, since these bands are significantly more intense in the

However, since these bands are significantly more intense in the spectra for roasted corn and barley than they are in the spectra for roasted coffee and husks and for spent coffee, they will probably contribute to the discrimination between coffee and

its respective adulterants. Thus, more attention should be given to this region of the spectra. With a prior knowledge that starch is present in both corn and barley and is not present in coffee and its by-products (husks and spent find more grounds) we have studied FTIR spectra for commercial corn starch (not shown) and noticed that these bands are clearly observed in those spectra and are more intense than those present in spectra for coffee, coffee husks and spent coffee grounds. The presence of these bands in the spectra for commercial corn starch may be attributed to the absorption combination bands of bound phenolics (Lopez-Martinez et al., 2009; Omwamba & Hu, 2010), such as ferulic and coumaric acids and their derivatives, or to absorption in the C–O stretching region due to the interaction of starch and the residual gluten in the presence of water. Also, in this same wavenumber range, the water association band (2400–2000 cm−1), attributed to a combination of the bending mode of water molecules with intermolecular vibration modes due to hydrogen bonding between water molecules and between water

and other molecules, may be responsible for part Trichostatin A in vivo of the absorption. In the spectra we obtained for hydrated corn starch (not shown), the absorption in this region was significantly more intense than it was in the spectra for commercial corn starch. Hence, Celastrol in our study, the absorption in the range of 2250–1850 cm−1 may be partially associated with a large presence of phenolics bound to non-degraded starch in roasted corn and roasted barley and partially with the hydration water effect on the non-degraded starch in roasted corn and

roasted barley. Low hydration of starch granules stabilizes the starch structure and allows some of the starch granules present in corn and in barley to stay intact during roasting and thus be found in the roasted product, as detected by Amboni, Francisco, and Teixeira (1999) by scanning electronic microscopy. Sharp bands at 1745–1742 cm−1 are evident in coffee, corn and spent coffee grounds spectra. Such bands have been previously identified in FTIR spectra of roasted coffee (Kemsley et al., 1995; Lyman et al., 2003; Reis et al., 2013) and attributed to carbonyl (C O) vibration in esters (triglycerides) and aldehydes. Such literature reports and the fact that these bands are rather weak in the spectra obtained for roasted coffee husks and barley (low lipid content) corroborate our previous assessment (Reis et al., 2013) regarding its association to lipid concentration.

In contrast, for A549 lung cancer cells (FR −ve), the uptake was

In contrast, for A549 lung cancer cells (FR −ve), the uptake was independent

on the sequence of loading. The FR-nanogel-CDDP displayed superior antitumour activity towards A2780 xenografts in contrast to free CDDP [ 24]. The intracellular delivery of carboplatin has been investigated by coupling i.p. Wnt cancer administration with a folate-receptor-targeted liposomal system. The cytotoxicity is enhanced (twofold) in comparison to carboplatin itself towards human ovarian IGROV-I (FR +ve) cancer cells. Mice bearing the i.p.-grown human IGROV-1 ovarian tumour xenografts treated with FRT-carboplatin liposomes had an 83% survival rate [25]. EGF is another potential targeting ligand due to the overexpression of the EGF receptor in human tumours, in particular NSCLC non-small cell lung cancer. Bhirde et al. have attached cisplatin (dissolved in DMSO) and EGF to oxidised SWCNTs to target squamous cancer. In vivo studies revealed SWCNT–CDDP–EGF (19) were selective towards HNSCC head and neck squamous cell carcinoma. Tumour growth regression was significant in mice treated with SWCNT–CDDP–EGF bearing HNSCC xenografts in contrast to mice treated with SWCNT–CDDP [ 26•]. Biotinylated BMS-754807 in vitro epidermal growth factor (bEGF)

conjugated to a Pt(NH3)22+-gelatin nanocomplex (GP-Pt-bEGF, 20) gives rise to a twofold higher Pt concentration in A549 human adenocarcinoma (EGF +ve) compared to HFL1 lung fibroblasts (EGF −ve). Immunodeficient mice injected with an A549 cell suspension treated with GP-Pt-bEGF nanoparticles displayed a reduction in tumour volume compared to mice treated with free CDDP which the tumour volume grew rapidly [ 27••]. The high molecular weight of full length EGFR monoclonal antibody if used as a targeting ligand may hinder its penetration into tumour cells; furthermore interaction with the Fc receptor on normal tissues may disturb its specific targeting. Therefore, single-chain antibodies against the EGFR (ScFvEGFR) lacking the Fc receptor have been conjugated onto the surface of ScFvEGFR-heparin-CDDP nanoparticles

(with Pt(NH3)22+ bound to carboxylates, 21). Nanoparticle Adenosine conjugate 21 was most potent towards H292 (EGF +ve) human lung cancer cells with an IC50 of 1.1 μm. Kidneys from mice treated with 21 showed no change in either blood urea nitrogen (BUN) or creatine (CRE) levels, in contrast to CDDP which gave significant changes consistent with impaired renal function [28••]. Xu et al. have coupled a Pt(NH3)2-herceptin (L2, Figure 2g) dicarboxylato binding ligand onto dumbbell-like Au-Fe3O4 nanoparticles (22) to act as nanocarriers to deliver the platinum pharamacophore into SK-Br3 breast cancer (HER2 +ve) cells. Without the targeting agent, the platin-Au-Fe3O4-NPs were still active, but less than CDDP. Thus, herceptin enhances Pt uptake in SK-Br3 cells giving greater cytotoxicity owing to the specific targeting.

5 presents some of the drying curves for different fruit:solution

5 presents some of the drying curves for different fruit:solution rations. The equilibrium moisture

content of the dried cherries was calculated based on the changes in their weight. The calculated Sunitinib in vivo equilibrium moisture content was 1.089 ± 0.150 kg moisture/kg dry matter. The equilibrium moisture was determined from three samples for each ration studied. These samples were dehydrated for 12 h, then oven-dried until they reached a constant weight, following the 2002 AOAC method. In all the conditions, there was a period of declining moisture content characterized by a rapid drop in the drying rate. This indicates that the main mechanism of water transport was diffusion and that the diffusion equation can be employed to analyze drying data. The moisture content of West Indian cherry decreased exponentially over time, from 11.05 to 3.10 kg moisture/kg find more dry matter after 12 h, which is in agreement with previous research (Derossi et al., 2008 and Spiazzi and Mascheroni, 1997) on other fruits. Exponential changes were also observed in weight reduction, solid gain and water loss of West Indian cherry, as shown in Fig. 1, Fig. 2 and Fig. 3.

Table 2 shows a statistical analysis of water loss, solid gain and weight loss at the fruit:solution rations under study. As can be seen in this table, the fruit:solution ratio of 1:10 showed the lowest standard deviation (SD) values, except for the solid gain, whose lowest SD occurred with the 1:4 ratio. This can be explained by the effect of solution dilution at the 1:4 ratio. The profiles presented in Fig. 1, Fig. 2, Fig. 3 and Fig. 4 reflect the above described patterns. The high coefficients of determination Liothyronine Sodium obtained by the Levenberg–Marquardt method and Differential Evolution method (R2 > 0.958) indicated the goodness of fit of experimental data to Eq. (4), see Table 3. The Def values varied from approximately 1.558 × 10−10–1.771 × 10−10 m2 s−1 for West Indian cherry. These values are within the range of Def (10−12–10−8 m2 s−1) normally expected for dehydrated foods ( Azoubel and Murr, 2004, Corrêa et al., 2006 and Gely and Santalla, 2007). This variability in diffusion

coefficient depends on the experimental conditions and procedures used for the determination of the moisture diffusivity, as well as on the data treatment methods, the product’s properties, composition, physiological state, and heterogeneity of its structure. For instance, Corrêa et al. (2006) obtained Def values between 2.78 × 10−10 and 8.42 × 10−10 m2s−1 for West Indian cherry samples osmotically dehydrated at a solution:sample ratio of 3:1 for 60°Brix of sucrose solution, during 24 h of osmotic dehydration. Fig. 6 show experimental moisture distribution during the osmotic treatment for the fruit:solution ratio 1:15 studied here, similar results for the other cases were obtained. The distribution behavior corresponds to the model calculated with diffusion values estimated by two methods: Levenberg–Marquardt and Differential evolution.

After his internship, Larry became an instructor in Homer Smith’s

After his internship, Larry became an instructor in Homer Smith’s physiology department at NYU and worked with him at the Mount Desert Island Biological Laboratory in Maine, studying electrolyte regulation in animals and translating the www.selleckchem.com/products/ipi-145-ink1197.html findings to humans. After further training in clinical nephrology, Larry became Chief of the Renal Section at the Boston VA 1954-1956, and then Assistant Professor of Medicine, SUNY College of Medicine, Syracuse. In 1960–1961 he took the first of his several highly productive

sabbaticals, this time to the Strangeways Research Laboratory in Cambridge, UK, where he learned bone rudiment organ culture from Dame Honor Fell and developed it into a quantitative method to study effects of agents on bone by labelling the fetal bones in vivo with 45Ca. Larry became fully dedicated Selleckchem DZNeP to bone upon taking a position at the University of Rochester as Associate Professor of Clinical Pharmacology and Medicine. Larry spent 13 years at Rochester, and was part of a visionary group of “boneheads” that included Bill Neuman and Bill Peck. Larry

used the bone organ cultures to demonstrate that parathyroid hormone stimulated bone resorption by direct effects on bone. He guided studies in his laboratory that showed the role of cAMP in resorption, the direct effects of calcitonin to inhibit resorption, and the secretion of bone-resorbing activity from cultured parathyroid glands. Other studies addressed effects of steroid hormones, including the newly discovered vitamin D metabolites. Discoveries that he was to pursue extensively with his students and Inositol oxygenase colleagues throughout his career were the effects of newly recognized factors, prostaglandins, growth factors and cytokines. To expand his experience to the anabolic side

of bone, Larry took a sabbatical at the National Institutes of Dental Research with George Martin and Karl Piez to learn collagen chemistry, and as a side interest worked with John Horton and Joel Oppenheim in the immunology group at NIDR and discovered that the active inflammatory material from periodontal disease contained a bone resorbing factor that they named Osteoclast Activating Factor. Larry’s further work in what was eventually named “osteoimmunology” was stimulated by the collaboration with the late Greg Mundy, inspiring and leading research on myeloma bone disease when they showed that OAF was produced by supernatants of both lymphoid and myeloma cell cultures. Subsequent work over many years showed that OAF was a composite of several bone-resorbing cytokines. Larry moved to Connecticut in 1974 as Chief of Endocrinology at the University of Connecticut Health Centre and was a major force in developing that institution as a center for bone research.

, 2005) To this day existence of a circadian clock has been demo

, 2005). To this day existence of a circadian clock has been demonstrated for Plants, Animals and, among the Prokarya, exclusively in Cyanobacteria. However, there is evidence for circadian rhythms also in other Bacteria (Min et al., 2005) and in Archaea (Edgar et al., 2012). One of the first circadian rhythms in a unicellular prokaryotic

organism was reported for cell division in the marine Synechococcus sp. strain WH 7803 ( Sweeney and Borgese, 1989). This astonishing observation contradicted a former hypothesis stating that intracellular compartments are absolutely necessary for circadian timing. In 1993 the Sunitinib nmr freshwater cyanobacterium Synechococcus elongatus PCC 7942 (hereafter S. elongatus) emerged as a prokaryotic model organism Nutlin-3 chemical structure for circadian research because it was amenable to genetic manipulations and

molecular tools were available for this species ( Golden et al., 1987, Golden, 1988 and Kondo et al., 1993). After 20 years of investigations the molecular mechanism underlying the functioning of the prokaryotic core clock is well understood, though many processes, especially those involved in input and output pathways in the cyanobacterial cell await further elucidation. The core oscillator of S. elongatus consists solely of three proteins, KaiA, KaiB

and KaiC ( Ishiura et al., 1998). KaiC is the core component of this unique post-translational oscillator. Due to inverse modulation by KaiA and KaiB it intrinsically phosphorylates and dephosphorylates, which leads to phosphorylation cycles that display a period of about 24 h ( Iwasaki et al., 2002, Kitayama et al., 2003, Nishiwaki et al., 2004 and Xu et filipin al., 2003). All three kai genes together are found in Cyanobacteria exclusively. Thus, the KaiABC system cannot represent a general prokaryotic clock mechanism. However, sequences similar to KaiC, sometimes in combination with KaiB, were identified also outside the cyanobacterial phylum, in Proteobacteria, Chloroflexi and Archaea ( Aoki and Onai, 2009 and Dvornyk et al., 2003). Regarding other cyanobacterial species and particularly marine Cyanobacteria, the knowledge about circadian rhythms is very limited. One of the reasons for the rare studies on clock systems in marine Cyanobacteria is founded mainly by the lack of effective genetic manipulation systems. Our purpose for this review is to compare the well-studied S. elongatus clock system with information we have on circadian rhythms in other, particularly marine Cyanobacteria.

, 2012) Although surface rainwater runoff has frequently been in

, 2012). Although surface rainwater runoff has frequently been investigated in many countries, little attention has been

paid to urban snowmelt runoff (Buttle 1988). In countries with a moderate continental climate, winter surface runoff quality is influenced primarily by litter and rubbish from streets, soil and pavement erosion, emissions from vehicles and industry, road de-icing composites, street cleaning, salting and snow removal etc., as well as the weather conditions (Sujkova et al. 2012, Shhukin et al. 2012). Up to 60% of the annual pollutant load related to surface runoff originates from the winter period, because pollutants selleck chemicals llc are accumulated in the snowpack and then released during intermittent and final snowmelt (Marsalek 2003). In cities where the surface runoff drainage system was designed in the mid-20th century, the common practice has been to discharge the runoff directly into watercourses, since for a long time urban surface runoff was not considered harmful to the environment. In the city of Brest, the surface runoff from the majority of drainage collectors is discharged directly into the River Mukhavets. The Mukhavets is the main river of Brest Polesye, a watercourse important for the socio-economic development of the region. Four towns are situated on the banks

of the Mukhavets, and the river provides a water supply, shipping, fishing and recreation for their populations.

The river MDV3100 clinical trial is also the main recipient of wastewaters (Volchek et al. 2005). Furthermore, the Mukhavets is a tributary of the trans-boundary Western Bug, a river belonging to the Baltic Unoprostone Sea catchment area. This means that the contaminants entering the Mukhavets contribute to the total amount of pollutants carried to the Baltic Sea by river systems. The aim of this paper was to study the inorganic constituents of snow and snowmelt runoff in urban areas as exemplified by the city of Brest, and to indicate the components that could pose a potential environmental threat. Accordingly, the concentrations of inorganic ions such as chloride, phosphate, nitrate and ammonium, heavy metals (HM) – Pb, Cu, Mn, Zn, Fe, Ni, Cr – as well as total suspended solids (TSS) and pH were determined in samples of snow and snowmelt runoff collected from December 2012 to April 2013. To evaluate the impact on surface waters, all the results were compared with the national regulations for surface waters – the maximum permissible concentrations (MPC) for fish breeding waters (Regulation No. 43/42). TSS concentrations were compared with the national regulation for urban surface runoff discharges (TCGP, 2012 – Technical Code 17.06-08-2012 (02120)), because the regulation for fish breeding waters does not limit the concentration of TSS, but only states its maximum permissible increase after wastewater discharges.

Nonetheless, co-management has been particularly useful in small-

Nonetheless, co-management has been particularly useful in small-scale fisheries [1] and [20]. Operationalising an EAF can, however, be arduous for managers in low-income and island countries. The process involves the diagnosis of the fishery, defining and prioritising management objectives, setting of regulatory measures to achieve the objectives and actions by the manager to implement and monitor those measures [11] and [21]. Ideally, all of these steps should be undertaken jointly with stakeholders selleck chemicals in the fishery.

A consultative process allows for discussion of key uncertainties, logistic constraints and practicality of implementing various management measures [11] and [22]. The management solutions must concurrently arise within the technical and human resource capacity of management http://www.selleckchem.com/products/ch5424802.html institutions. Small-scale coastal fisheries in Pacific Islands contribute to food security, livelihoods and culture [9] and [23]. While finfish contribute significantly to food security in coastal communities, invertebrate fisheries such as sea cucumbers provide community-level income streams and contribute to national export revenue. Sea cucumbers are a key resource, contributing to poverty alleviation for probably more than three million fishers globally [24]. They are fished, either for subsistence consumption or export, in every Pacific Island Country (PIC)

[25] and are a vital marine export commodity for numerous countries elsewhere [24], [26] and [27]. Exportation

of the processed product, called beche-de-mer, from Pacific Islands to Asian markets has occurred intermittently for at least 160 years [25]. Sea cucumbers are the third-most economically important marine export from Pacific islands, after tunas and pearls, and are probably worth much more than officially reported [28]. Sea before cucumber production from Fiji, Solomon Islands and New Caledonia, when converted to wet weight equivalents, compare to 19–32% of tuna catches in their exclusive economic zones [29]. Globally, sea cucumber fisheries have often lacked comprehensive management plans and enforcement capacity to deal with intense exploitation rates [24]. Soaring market demand, lack of alternative income streams for fishers and ineffective management have led to recent over-exploitation of resources across the Pacific [25] and [28]. Over-exploitation of wild stocks has prompted national fishery closures in Papua New Guinea, Solomon Islands and Vanuatu within the past 5 years [24]. The closures herald failures in past management systems but, at the same time, give hope to the future as they demonstrate a political will to take drastic measures to protect these resources. A few fisheries in the Pacific Islands have remained as subsistence fisheries (domestic consumption only) (Fig. 1) but have come under recent pressure to open harvests for export.

2007) Hierarchical CA was used on standardized data, applying Wa

2007). Hierarchical CA was used on standardized data, applying Ward’s method with correlation. The low and high nutrient stations were determined from hierarchical CA using linkage

distance. PCA extracted eigenvalues and eigenvectors from the covariance matrix of the original variables, then produced new GS-7340 nmr orthogonal variables known as PCs through VARIMAX rotation, which are linear combinations of the original variables. PCs provide information on the most meaningful parameters that describe a whole data set, allowing data reduction with minimum loss of original information. They are unobservable, hypothetical, latent variables (Vega et al. 1998, Helena et al. 2000, Pekey et al. 2004, Singh et al. 2004, Wu & Wang 2007, Zhou et al. 2007). All the mathematical and statistical computations were performed using MATLAB R2008b (Mathworks Inc., USA) and ArcGIS 9.3 (ESRI Inc., USA). MODIS-Aqua satellite images (4-km Level 3 HDF) covering the SCS were obtained from NASA. Weekly (8-day) composite sea surface temperature (SST) data from 14 to 21 September were used owing to the heavy cloud coverage around this region during the cruise. The SeaDAS package was used to process the SST imagery. The horizontal distributions of parameter concentrations at the surface are shown in Figure 2. The horizontal distributions of surface NO2-N reveal that there are two

high concentration regions: one is near the Pearl River Estuary in signaling pathway the north-west, the other is near the Luzon Strait in the

south-east (Figure 2a). The NO3-N distribution shows four high nutrient regions: near the Pearl River, in the south-west, south-east Histamine H2 receptor and north-east of the PIS (Figure 2b). The NH4-N concentration is high in the north-west, north-east and south-east of the PIS (Figure 2c). SiO3-Si is distributed in three regions: (1) around and to the north-east of the PIS, (2) in the west of the PIS and (3) near the perennial cold cyclonic eddy (Figure 2d). The PO4-P distribution shows horizontal variations with increases from the southern to the northern regions; it is also found in the same three regions where silicate is distributed (Figure 2e). The distributions of DO and Chl a are similar: high near the coast and low in offshore waters. The offshore DO concentration is equal to 6.64 m ol dm−3. In contrast, Chl a shows three small, high-concentration regions in the Pearl River Estuary, the locations of which are similar to those of silicate ( Figures 2f–g). The temperature distribution is significantly low in the north-east and the west of the PIS, and low at 114°E–115°E in the south ( Figure 2h). The horizontal distributions of SiO3-Si and temperature show three upwelling regions: (1) the north-east of the PIS, (2) the west of the PIS and (3) the regions of the perennial cold cyclonic eddy.