Figure 2 shows the time series of the weekly KWI and KCI computed by using the AVISO data from 1993 to 2013. The KWI has significant seasonal variations and its minimum (maximum) values mainly occur in the winter (summer), with values less than -4.0× 105 m2 s-1 in the winters of 1995/1996, 1996/1997, and 2011/2012. The KCI is characterized by intraseasonal variations. Power spectral analysis also indicates that significant intraseasonal and seasonal signals principally exist for the KWI, but only intraseasonal signals exist for the KCI (not shown).
The mean (μ) and standard deviation (σ) values of the KWI are -1.50× 105 and 0.75× 105 m2 s-1, and those of the KCI are 1.93× 105 and 0.55× 105 m2 s-1, respectively. The pink dashed lines in Fig. 2 denote the μσ. Based on the classification method mentioned in section 2, the red and blue dots represent KWEP and KCEP events, while the rest represent leaking path events. The occurrence proportions for these three types of paths, KWEP, KCEP and the leaking paths, are 14.1%, 14.8% and 71.1%, respectively, which are similar to the results of the KSI in magnitude (Nan et al., 2011a).
Figures 3a-f show the composites of the ADT, the surface geostrophic currents, and the SLA for the three types of paths based on the DI. The corresponding GV composites and eddy kinetic energy (EKE) are shown in Figs. 3g-l. When KWEP events occur, the main Kuroshio path enters the SCS in the middle portion of the LS and flows outward in an anticyclonic pattern in the northern part (Figs. 3a and g) to form a "Kuroshio loop" (Li and Wu, 1989; Xue et al., 2004; Nan et al., 2011a). The center of the Kuroshio loop is located southwest of Taiwan Island and has a minimum negative GV value (Fig. 3g) with SLA and EKE values larger than 15 cm and 0.15 m2 s-2 (Figs. 3b and h). Therefore, a KWEP event is mainly characterized by a warm eddy in the center of the Kuroshio loop. The warm eddy may be detached from the Kuroshio loop, based on in-situ and satellite altimeter observations (Li et al., 1998; Caruso et al., 2006; Yuan et al., 2006).
When a KCEP event occurs, the main Kuroshio path flows across the LS, and a branch of the Kuroshio enters the SCS in the northern part of the LS (Figs. 3c and i). Maximum positive GV values exist left of the main Kuroshio path (Fig. 3i), with a minimum SLA value of less than -5 cm (Fig. 3d) and a maximum EKE value of approximately 0.09 m2 s-2 (Fig. 3j). These results demonstrate that the KCEP is mainly characterized as a cold eddy, which occurs west of the LS, when the main Kuroshio path leaps the LS. A branch of the Kuroshio water enters the SCS in a cyclonic pattern in the northern region of the LS. Parts of this branch may return to the main Kuroshio path (Fig. 3c), which corresponds with the cyclonic intrusion presented by (Caruso et al., 2006). It is worth noting that there are two warm eddies with maximum SLA values larger than 5 cm on both sides of the cold eddy. One eddy is in the SCS and the other is just outside the LS (Fig. 3d). The relationships between the warm and cold eddies in the SCS are consistent with the conceptual model of eddy-Kuroshio interaction during the summer proposed by (Nan et al., 2011b). Their results show that a cold eddy often forms when the main Kuroshio path leaps the LS during the summer, which induces the formation of a warm eddy in the SCS and west of the cold eddy. Several studies have revealed that the warm eddy east of the LS will allow the main Kuroshio path to overcome the β effect more easily and leap the LS (Sheremet, 2001; Zhao and Luo, 2010; Yuan and Wang, 2011).
Because the leaking path accounts for more than 70%, the composite ADT and surface geostrophic currents of the leaking path are similar to those of the mean state (Figs. 1 and 3e). According to the ADT maps, there is no significant distinction between the leaking path and KCEP because both paths have a branch of Kuroshio flowing into the SCS. The branch of Kuroshio in the KCEP is northward relative to that in the leaking path. However, the difference between the leaking path and KCEP is clear when looking at the SLA maps, in which no eddy is in the leaking path (Fig. 3f). For the leaking path, the intensities of negative and positive GVs are relatively weak north and south of the integrated area (Fig. 3k), and the EKE values are smaller than those of the KWEP or KCEP in the SCS (Fig. 3l). Therefore, weaker mesoscale eddy activities in the northeastern SCS are the main features of the leaking path.
As shown above, the newly defined DI method can be used to identify three typical Kuroshio intrusion paths: the KWEP, KCEP, and leaking path. These three paths not only focus on the main Kuroshio path, but also on the typical spatial patterns of both the Kuroshio path and mesoscale eddies west of the LS. The ratios between the standard deviations and ensemble mean of each category——KWEP, KCWP and leaping path——have also been computed (not shown). The values are around 10% in the study domain. The small ratio suggests that the patterns of each event in each category are close to each other.
To compare the DI with the KSI, we calculate two KSIs (KSI1 and KSI2), as discussed in section 2. The integral area and the calculation method of KSI1 are the same as the KSI proposed by (Nan et al., 2011a). The calculation method of KSI2 is the same as that of KSI1, but uses the integral area of the DI, which is smaller than that of KSI1 (Fig. 1). Therefore, the impacts of the integral area can be determined by comparing KSI1 and KSI2, and the impacts of the calculation methods can be evaluated by comparing KSI2 with the DI. In the present sub-section, we present the primary features of KSI1 and KSI2, including the indices themselves, the occurrence proportions of different paths, and the spatial patterns of composited flows and eddies.
Figures 4a and b show the time series of the weekly KSI1 and KSI2 from 1993 to 2013. Overall, KSI1 is consistent with the KSI calculated by (Nan et al., 2011a), with only small differences resulting from different dataset versions. Nevertheless, large differences occur between KSI2 and KSI1 (Figs. 4a and b), and KSI2 is similar to KWI (Fig. 2). Figures 4a and b also indicate that KSI1 has a significant intraseasonal signal, while KSI2 has both intraseasonal and seasonal signals.
Using the standard deviations as thresholds, the red and blue points represent the looping and leaping path events and the remaining points represent the leaking path events. The occurrence proportions of the three patterns are approximately 15%, 15% and 70% for the looping, leaping and leaking paths, respectively (Table 1), which are close to those of the DI shown above.
Figures 4c and e show the composite of the ADT and the corresponding surface geostrophic currents for the looping and leaping paths for KSI1. Figures 4d and f are the same as Figs. 4c and e, respectively, but for KSI2. Because the patterns of the leaking paths are similar to those in Fig. 3e, the figures are not shown here. The distributions of the ADT and the surface geostrophic currents for the looping path and leaping path identified by KSI1 (Figs. 4c and e) are consistent with the results of (Nan et al., 2011a), but different from the paths identified by KSI2. The greatest distinction between KSI2 and KSI1 is that the ADT value in the center of the looping path identified by KSI2 is approximately 10 cm larger than that identified by KSI1 (Figs. 4c and d), which suggests that the events for the looping path classified by KSI2 are stronger than those classified by KSI1. For the leaping path, a cold eddy exists west of the LS, which is identified by KSI2 and is smaller than the Luzon cold eddy northwest of Luzon Island identified by KSI1 (Figs. 4e and f).
According to a preliminary comparison between KSI1 and KSI2, the integral area will significantly affect events and flow features; however, the occurrence proportions of the three patterns for KSI1 and KSI2 are close. These results also indicate that the paths of Kuroshio intrusion are more sensitive to changes in the integral area.
3.3.1. Monthly proportions of the looping/KWEP and leaping/KCEP paths
The Kuroshio intrusion has seasonal signals that are strong in winter and weak in summer (e.g., Wyrtki, 1961). Thus, investigating the seasonal variations of the three indices can highlight the distinctions among them. Figure 5 shows the monthly proportions of the looping/KWEP and leaping/ KCEP paths identified by the three indices. Hereafter, for simplicity, we simply refer to the looping and leaping paths. Overall, the values of the proportions show that the differences between KSI1 and KSI2 are much larger than those between KSI2 and DI, especially for the looping path.
For the looping path, both KSI2 and the DI indicate that the maximum proportion occurs during winter, with approximately 40% in December and 30% in November, and that the minimum proportion (less than 10%) appears during summer. Compared with KSI2 (or the DI), the proportion of KSI1 has semi-annual variations, with two peaks exceeding 20% in both July and November. These peaks suggest that the seasonal variations of the looping path identified by KSI1 are not consistent with observations (e.g., Wyrtki, 1961; Lan et al., 2004).
The seasonal proportion of the leaping path is generally higher in the winter and lower in the summer for KSI1, which obviously conflicts with observations (e.g., Wyrtki, 1961; Qu, 2000; Lan et al., 2004). The differences between KSI1 and KSI2 for the leaping path occur mainly in February and August, with KSI1 yielding a 20% higher (10% lower) result than KSI2 in February (August). The differences (over 5%) between KSI2 and the DI for the leaping path occur in April, May, June, July and October, with the largest occurring (over 10%) in April. This indicates that the consistency of KSI2 and the DI for the leaping path is less than that for the looping path.
According to the seasonal proportion of the looping and leaping paths, KSI2 and the DI appear closer to the observations than KSI1. These results indicate that the indices are sensitive to the integral area. Furthermore, the major differences between KSI2 and the DI are the proportions of the leaping path in spring and summer. The following analysis will focus on what causes these differences and also on which index is more reasonable.
3.3.2. Impacts of the integral area
Figure 6 presents the scatter diagrams for the normalized KSI2-KSI1, KSI2-KWI, and KSI2-KCI. According to the definition, the looping (leaping) events are identified by values smaller (greater) than -1 (+1), and the leaking pathevents are the black dots in the center area identified by the two indices. In Fig. 6a, the events in the A2 and A6 zones are identified as the looping and leaping paths, respectively, by both KSI1 and KSI2; events in the A1 and A5 zones are identified as leaking paths by KSI2 and as looping and leaping paths by KSI1; and events in the A3 and A5 zones are identified as the looping and leaping paths by KSI2 and as leaking paths by KSI1. The largest difference occurs in the A4 and A8 zones. Events in the A4 zone are identified as the leaping path by KSI1, as the looping path by KSI2, and vice versa in the A8 zone. Figures 6b and c are similar to Fig. 6a, but for KSI2-KWI and KSI2-KCI. The key zones for looping paths are B1, B2, B3 and B8, and those for leaping paths are C4, C5, C6 and C7.
Based on the significant differences between the monthly variations of the proportions for Kuroshio intrusion types (Fig. 5), we use colored dots and triangles to highlight the looping and leaping events that occur during particular months (Fig. 6). When comparing KSI1 with KSI2, we choose July, August, September and December for the looping path, and February, March and April for the leaping path (Fig. 6a). Additionally, to compare KSI2 and the DI, May, June and December are selected for the looping paths (Fig. 6b), and April, May, July and October are selected for the leaping paths (Fig. 6c). The analysis of the following composite and single case maps according to scatter diagrams will demonstrate the causes of the differences in the monthly occurrence proportions shown in Fig. 5.
First, we analyze the impacts of the integral area based on the scatter diagram of KSI1-KSI2 (Fig. 6a). To determine the main differences between KSI1 and KSI2, we focus on the A1, A2, A5 and A7 zones. Figure 7a presents the composite ADT and corresponding surface geostrophic currents according to the 21 cases in July in the A1 zone (red dots in Fig. 6a; Table 2). These cases are the looping paths for KSI1 and leaking paths for KSI2. The classification for KSI2 is obviously more reasonable. Figure 7b is the same as Fig. 7a, but for 26 cases in the A3 zone in December (purple dots in Fig. 6a; Table 2) that are identified as leaking paths by KSI1 and looping paths by KSI2. The composite ADT and current pattern are obviously a looping path and not a leaking path, which also indicates that KSI2 is more reasonable.
For the situation shown in Fig. 7a, no evident positive or negative GV center occurs in the integration area. A weak negative GV center in the northern part of Box 1 causes the integration to be more negative and is mistakenly classified as the looping path by KSI1. According to Fig. 7b, although a strong negative GV center occurs in the northern part of Box 1, the positive GV center in the south will cancel out the negative value. Thus, there is no peak for KSI1. These results can also explain the causes of the relatively high (low) occurrence proportion of the looping path in July (December) by KSI1.
Figure 7c shows the composite ADT and surface geostrophic currents of 19 events in the A5 zone in February (red triangles in Fig. 6a; Table 2), and Fig. 7d is similar to Fig. 7c, except for 20 events in the A7 zone in April (blue triangles in Fig. 6a; Table 2). In Fig. 7c, the events are identified as the leaping path by KSI1 and as the leaking path by KSI2; however, the opposite situation is shown in Fig. 7d. For the leaping path, a strong cold eddy with larger positive GV exists west of the LS, based on both KSI1 and KSI2. However, the center of the cold eddy identified by KSI1 is more southwestward than that of KSI2. The strong cold eddy cannot prevent the Kuroshio from entering into the SCS completely, because a branch of the Kuroshio extends into the SCS in the leaping path, which is identified by KSI1 and KSI2 (Figs. 4e and f). Moreover, the intrusion branch of the Kuroshio for the leaping path appears stronger than that for the leaking path. Therefore, it is difficult to determine which index is more reasonable for the leaping path. In addition, this finding suggests that it is improper to call this path the "leaping path". The ADT distribution in Fig. 7c is closer to that in Figs. 3e and 4e, while the ADT distribution in Fig. 7d is similar to that in Figs. 3c and 4f. Therefore, we infer that KSI2 better depicts the spatial pattern of mesoscale eddies and mean flow.
Figure 8 is similar to that of Fig. 7, except for the A4 and A8 zones, which have relatively fewer events (only 4 events in the A4 zone and 12 events in the A8 zone). These also suggest that both KSI1 and KSI2 are reasonable to some extent. Figure 8a is the same as Fig. 7d, except for 4 events in April and 4 events in September in the A8 zone (green and blue dots in Fig. 6a; Table 2). A cold eddy is located just west of the main Kuroshio path, and a warm eddy is located just west of the cold eddy. Because the entire area integration of GV is negative, the paths are classified as looping paths for KSI1. However, it is clear that this path is not a looping path. Figure 8b shows the same situation, but with only one case on 31 August 2011 when compared with the composite map shown in Fig. 8a.
Because only 4 cases occur in the A4 zone, a single case map is shown here instead of a composite one. Figures 8c-f present the distributions of the ADT for the 4 cases, which are identified as leaping paths by KSI1 and looping paths by KSI2. Although the flow pattern details vary, the main features clearly indicate looping paths in Figs. 8c, d and f, which indicate that KSI2 is more reasonable than KSI1. The situation shown in Fig. 8e is special. Although a negative GV occurs in the north part of the area, the value is small. Based on its definition, this path should not be classified as a leaping or looping path. Thus, both KSI1 and KSI2 misjudged this case.
The causes of missed or misjudged events when comparing KSI1 and KSI2 are shown above. Furthermore, we confirm that indices are sensitive to the integral area, and KSI2 calculated in a relatively small region seems more reasonable. The integral area for KSI1 is larger than the circulation structure and mesoscale eddy scales. Thus, the offset of positive and negative GVs possibly results in the reduction of the absolute value of the integrated GV for the looping path (e.g., Fig. 7a) and the criterion for the leaping path (e.g., Fig. 7c). However, KSI2 also results in misjudgment, as shown in Fig. 8e.
3.3.3. Impacts of calculation methods
A comparison of the Kuroshio intrusion paths between KSI2 and the DI will further reflect the difference caused by the algorithm of the indices, which considers whether to compute the positive and negative GVs separately. Figures 6b and c present scatter diagrams for the normalized KSI2-KWI and KSI2-KCI. From the distribution of the scatter dots, the consistency between KSI2 and KWI is better than that between KSI2 and KCI, which can also be seen in Fig. 5. Similar to the analysis of the impacts of the integral area, we also apply the composite method to investigate the causes of the differences between KSI2 and the DI.
Figure 9a shows the composite ADT and surface geostrophic currents of 11 events in the B1 zone in December (purple dots in Fig. 6b; Table 2). Figure 9b is similar to Fig. 9a, except for 7 events in the B3 zone in July (blue dots in Fig. 6b; Table 2). The former is identified as a leaking path by KSI2 and as the KWEP by the DI, while the latter is classified as a looping path by KSI2 and as the KCEP by the DI. These two situations reflect the main problems of KSI2. In Fig. 9a, it is clear that the judgment of the DI is correct. The misjudgment of KSI2 occurs because of the offset of the positive and negative GVs south and north of the integrated area. Although no strong negative GV center is shown in Fig. 9b, most of the integrated area is covered by relatively weak and negative GV. Therefore, the absolute values of the integrated GV of these cases are much more evident when using KSI2 than in the real looping path in which the large positive and negative values are offset. Thus, the misjudgment of KSI2 occurs.
Figures 9c and d are similar to Fig. 9a, except for 10 events in the C5 zone in July (blue triangles in Fig. 6c; Table 2) and 17 events in the C7 zone in April (red triangles in Fig. 6c; Table 2). The former is classified as the leaking path by KSI2 and as the KCEP by the DI, and the latter situation is classified as the leaping path by KSI2 and as the leaking path by the DI. As shown in Figs. 9c and d, it is difficult to determine which index is better. For the cases shown in Fig. 9c, two cores of positive and negative GVs are located in the integrated area west of the LS. For KSI2, the offset of positive and negative GVs results in a leaking path. However, for the DI, the positive GV is stronger than the negative GV. Thus, a KCEP occurs according to the DI. For the cases in Fig. 9d, weak positive GV anomalies occur throughout the study region. Because the absolute value of the positive GV is larger than that of negative GV for KSI2, the path is classified as a leaping path. The KCIs of these cases are smaller than those with strong cold eddies for the DI, and these cases are classified as leaking paths. In addition, the cases shown in Figs. 9c and d occur in July and April, respectively. The above two examples can also explain the differences in the occurrence proportion of the leaping path between KSI2 and the DI in Fig. 5b.
Figure 10 shows the ADT and surface geostrophic currents for the three events in the C4 and B8 zones. It is interesting that both the KWI and KCI values satisfy the criterion (Fig. 2). In Figs. 10a and b, two centers are shown in this study area: one has a large positive GV, and the other has a negative GV. The two events described above are both identified as looping paths by KSI2 because the absolute value of the negative GV in the north is larger than that of the positive GV in the south. For the DI, the KWEP and KCEP criteria are both satisfied. As mentioned in section 2, when this situation occurs, we classify the path based on the normalized deviations of the KWI and KCI from their mean values. That is, when the normalized deviation of KWI is larger than that of KCI, we define this as a KWEP case, and vice versa. The case in Fig. 10c is similar to the above two cases, except that the positive GV value in the south is relatively large. Therefore, the flow type is identified as the leaping path by KSI2. For the DI, the case is identified as a KCEP case because the KCI has a larger deviation from the mean value than the KWI. The above three cases indicate that the DI can address the special cases well when the KWI and KCI both satisfy the criteria.
Generally, the separated positive and negative GVs in the DI overcome the shortcomings of KSI2 and result in a large reduction in the probability of the error. The DI can further highlight the anticyclonic pattern of the main Kuroshio path entering the SCS, while the positive and negative GVs are cancelled out in KSI2.