Hawaii Extended Forecast Discussion NWS Weather Prediction Center College Park MD 818 AM EDT Sun Apr 29 2018 Valid 00Z Mon Apr 30 2018 - 00Z Mon May 07 2018 The large scale pattern across the central and north Pacific will remain relatively unchanged through the week. Models/ensemble show a strong signal for a broad area of negative height anomalies persisting in the vicinity of 35-40N/150-170W. The persistent large scale trough will be maintained by a series of mid/upper-level shortwaves that traverse the northern stream flow across the Pacific and then amplify as they encounter the existing large scale cyclonic flow in place north of Hawaii. Initially, satellite imagery this morning show a relatively deep upper-level low in place approximately 600 miles north of Hawai'i. South of the upper low, a weakening surface front was located just east of the Big Island, with deep tropical moisture (PWs > 2.00 inches) pooling along the front. As the initial upper low weakens and becomes absorbed in the higher latitude westerlies, and a second shortwave enters the large scale mean trough early next week, models show the surface front and the associated deep moisture gradually lifting back northward across Hawai'i over the next couple days, and lingering into next weekend as it gradually washes out. Guidance shows low-level winds remaining relatively light and variable in the vicinity of the surface front as it washes out through mid-week, thus the potential for sustained orographic rains appears fairly limited, despite the deeper moisture. By later in the week (Wed night onward), guidance suggests that low-level easterlies may begin to pick up into the 10-20 kt range (increasing flow perpendicular to any remaining weak surface boundary), while another trough amplifies just northwest of Hawaii (increasing upper-level support for precipitation). Both the ECMWF and the GFS show the potential for more widespread heavy rains across the western islands by Thu-Fri. The ECMWF would keep the heaviest rain potential confined to Kaua'i, while the GFS would also include O'ahu. Both models show the potential for multi-inch rainfall totals. The ECENS supports the operational ECMWF in showing the potential for heavy rains across Kaua'i later in the week. The GEFS probabilities also mirror the operational GFS, although the heavy rain probabilities are a bit lower than shown in the ECENS. Thus, at this time there is slight to moderate confidence in another round of potential heavy rains for the western Hawaiian Islands by late in the week. The exact timing/evolution of the late week upper trough, as well as the strength and position of any lingering surface boundary by that time will all play a role in the existence and placement of any heavy rain potential. Ryan