1 00:00:05,559 --> 00:00:08,720 Speaker 1: Kioda. I'm Chelsea Daniels and this is the Front Page, 2 00:00:09,200 --> 00:00:16,160 Speaker 1: a daily podcast presented by the New Zealand Herald. New 3 00:00:16,239 --> 00:00:21,440 Speaker 1: Zealand has been experiencing some wild weather this week. Red 4 00:00:21,480 --> 00:00:25,640 Speaker 1: wind warnings were issued for much of Canterbury, Marlborough, Wellington 5 00:00:25,800 --> 00:00:29,840 Speaker 1: and southern Wadded Upper As it yesterday afternoon, flights and 6 00:00:29,920 --> 00:00:33,479 Speaker 1: fairies were canceled and tens of thousands of households have 7 00:00:33,560 --> 00:00:38,600 Speaker 1: been without power. Meanwhile, strong winds have been hampering firefighting 8 00:00:38,640 --> 00:00:42,680 Speaker 1: efforts in several parts of the country. So is this 9 00:00:43,000 --> 00:00:46,520 Speaker 1: usual for this time of year? And how long will 10 00:00:46,560 --> 00:00:50,040 Speaker 1: we have to wait for some sunny days ahead? Today 11 00:00:50,080 --> 00:00:54,520 Speaker 1: on the Front Page, Newer Principal scientist Chris Brandolino is 12 00:00:54,560 --> 00:00:57,880 Speaker 1: with us to take us through what's causing this stormy 13 00:00:57,960 --> 00:01:01,000 Speaker 1: weather and whether there is in fact a lot at 14 00:01:01,040 --> 00:01:07,120 Speaker 1: the end of the tunnel. First off, Chris tell us 15 00:01:07,400 --> 00:01:11,680 Speaker 1: why this is happening, what's causing these high winds across 16 00:01:11,720 --> 00:01:12,720 Speaker 1: the country. 17 00:01:12,760 --> 00:01:17,080 Speaker 2: Two words pressure gradient, So you may be wondering what 18 00:01:17,160 --> 00:01:21,240 Speaker 2: the heck is that. Basically, yeah, it describes the change 19 00:01:21,240 --> 00:01:24,800 Speaker 2: of air pressure over distance. So think of it this way. 20 00:01:24,959 --> 00:01:30,800 Speaker 2: Replace the term pressure gradient with elevation change. Imagine, if 21 00:01:30,880 --> 00:01:34,039 Speaker 2: you're a cyclist, you're at the top of a hill, 22 00:01:34,560 --> 00:01:37,839 Speaker 2: right and you're gonna go down the hill. You're gonna 23 00:01:37,840 --> 00:01:40,360 Speaker 2: go a lot faster if the hill is steep, right, 24 00:01:41,120 --> 00:01:42,959 Speaker 2: going from the top of the hill to the bottom 25 00:01:43,040 --> 00:01:45,320 Speaker 2: of the hill, you'll go maybe not as fast. If 26 00:01:45,319 --> 00:01:48,480 Speaker 2: that hill is more gentle or not as steep, that 27 00:01:48,600 --> 00:01:53,600 Speaker 2: elevation change isn't as dramatic. Think of high pressure in 28 00:01:53,600 --> 00:01:55,760 Speaker 2: the atmosphere, like the top of the hill. High pressure 29 00:01:55,800 --> 00:01:58,640 Speaker 2: brings nice weather. And for those listening or watching from 30 00:01:58,680 --> 00:02:03,520 Speaker 2: the upper North Island, Auckland and Hamilton and toward Northland, 31 00:02:03,560 --> 00:02:05,680 Speaker 2: we had some beautiful weather on Sunday, going back to 32 00:02:05,720 --> 00:02:09,079 Speaker 2: the weekend, even better weather on Monday, not so bad 33 00:02:09,120 --> 00:02:13,640 Speaker 2: on Tuesday. That was because of high pressure. Now that's 34 00:02:14,080 --> 00:02:15,920 Speaker 2: one end of the spectrum. On the other end of 35 00:02:15,919 --> 00:02:18,120 Speaker 2: the spectrum, low pressure is like a hole in the 36 00:02:18,160 --> 00:02:21,000 Speaker 2: atmosphere and Mother Nature is trying to fill that hole 37 00:02:21,600 --> 00:02:23,960 Speaker 2: with the fluid called air. And so when you have 38 00:02:24,080 --> 00:02:26,560 Speaker 2: high pressure top of the hill, low pressure kind of 39 00:02:26,560 --> 00:02:30,200 Speaker 2: bottom of the hill, or a hole a valley. If 40 00:02:30,240 --> 00:02:33,000 Speaker 2: they're quite distinct in terms of one being high, one 41 00:02:33,040 --> 00:02:37,639 Speaker 2: being quite lower deep, then your elevation change or your 42 00:02:37,680 --> 00:02:41,560 Speaker 2: pressure gradient could be quite dramatic. And that is what 43 00:02:41,720 --> 00:02:44,840 Speaker 2: causes wind, is pressure gradient, the change in air pressure 44 00:02:44,880 --> 00:02:46,680 Speaker 2: over distance. If you think of it like a mountain 45 00:02:46,720 --> 00:02:48,120 Speaker 2: in a hill, if that makes sense. 46 00:02:48,880 --> 00:02:51,920 Speaker 1: Yeah, when we hear about wind warnings of you know, 47 00:02:51,960 --> 00:02:54,880 Speaker 1: one hundred and thirty one hundred and fifty two hundred 48 00:02:54,960 --> 00:02:58,400 Speaker 1: kilometers an hour, what does that actually look like in 49 00:02:58,520 --> 00:02:59,520 Speaker 1: real terms? 50 00:03:00,040 --> 00:03:02,120 Speaker 2: I think you just go on media right now, social 51 00:03:02,120 --> 00:03:05,239 Speaker 2: media to see the impact. You know, when you see 52 00:03:05,280 --> 00:03:08,960 Speaker 2: wing gusts of you know, one hundred and seventy one 53 00:03:09,040 --> 00:03:11,080 Speaker 2: hundred and eighty two hundred k you're getting to like, 54 00:03:11,600 --> 00:03:15,720 Speaker 2: you know, category two, category three tropical cyclone intensity. I mean, 55 00:03:15,720 --> 00:03:18,680 Speaker 2: this is not a tropical cyclone, but it's the intensity. 56 00:03:18,720 --> 00:03:20,160 Speaker 2: You know, you're trying to wrap your head around this, 57 00:03:20,880 --> 00:03:23,280 Speaker 2: and that is what can cause you know, these bursts 58 00:03:23,280 --> 00:03:25,760 Speaker 2: of wind which are wing gusts to three second bursts 59 00:03:25,760 --> 00:03:28,560 Speaker 2: of win That is what generally causes a lot of 60 00:03:28,560 --> 00:03:30,760 Speaker 2: the damage. And we've seen that play out. We've seen 61 00:03:30,800 --> 00:03:33,840 Speaker 2: wing gusts. I was just looking Invercargo. I had a 62 00:03:33,840 --> 00:03:35,880 Speaker 2: win gus to think of one hundred I'm looking off 63 00:03:35,960 --> 00:03:38,560 Speaker 2: screen here one hundred and thirty seven k and over 64 00:03:38,600 --> 00:03:41,440 Speaker 2: toward Gore a wing gust of one hundred and twenty 65 00:03:41,480 --> 00:03:46,600 Speaker 2: four k I believe, one hundred Yeah, and at Wellington 66 00:03:46,800 --> 00:03:50,400 Speaker 2: at the airport one hundred and twenty six and Cayle 67 00:03:50,480 --> 00:03:54,800 Speaker 2: Cow and Wellington Kyalkou the mountain there one hundred and 68 00:03:54,880 --> 00:03:58,160 Speaker 2: fifty five kilometers per hour. So that type of wing gust. 69 00:03:58,600 --> 00:04:00,440 Speaker 2: If you can't wrap your head around, just go to 70 00:04:00,520 --> 00:04:03,720 Speaker 2: social media and you see like the pine trees leaning down, 71 00:04:03,760 --> 00:04:06,280 Speaker 2: and like a whole row of pine trees over toward 72 00:04:06,360 --> 00:04:10,200 Speaker 2: Hamner Forest leaning down on power lines, you know, or 73 00:04:10,320 --> 00:04:13,160 Speaker 2: roofs being lifted, you know, obviously the trampolines and you 74 00:04:13,200 --> 00:04:15,880 Speaker 2: know any deck furniture things like that that'll be you know, 75 00:04:15,920 --> 00:04:17,479 Speaker 2: that could be k's down the road or you know, 76 00:04:17,520 --> 00:04:19,920 Speaker 2: half k hundreds of meters anyway, Yeah, is. 77 00:04:19,880 --> 00:04:21,520 Speaker 1: This usual for this time of year? 78 00:04:22,120 --> 00:04:24,279 Speaker 2: Uh? Not to this degree. I mean this is what 79 00:04:24,320 --> 00:04:26,440 Speaker 2: the red warning, you know, the red warning kind of 80 00:04:26,520 --> 00:04:29,040 Speaker 2: you know, reflects the unusual nature. We don't see those 81 00:04:29,080 --> 00:04:32,000 Speaker 2: every day, that's for sure. Look, spring is always a 82 00:04:32,080 --> 00:04:35,359 Speaker 2: changeable season. And with that change that that that variety. 83 00:04:35,400 --> 00:04:37,719 Speaker 2: I like to call spring the teenager of season because 84 00:04:37,960 --> 00:04:40,440 Speaker 2: a lot of mood swings ups and downs, and with 85 00:04:40,600 --> 00:04:43,400 Speaker 2: that moodiness comes win. So you know, it's not unusual 86 00:04:43,400 --> 00:04:45,719 Speaker 2: to have windy PIDs in spring. That's part of spring. 87 00:04:46,320 --> 00:04:49,839 Speaker 2: But this is like, this is next level, and what's 88 00:04:49,960 --> 00:04:52,440 Speaker 2: driving that is kind of nerdy. We've had a lot 89 00:04:52,480 --> 00:04:56,000 Speaker 2: of low pressure that whole in the atmosphere I've talked about, right, 90 00:04:56,080 --> 00:04:58,239 Speaker 2: we had a over the subn Ocean, so the Suthern 91 00:04:58,240 --> 00:05:01,599 Speaker 2: Ocean is that big body of water separating New Zealand 92 00:05:01,640 --> 00:05:04,960 Speaker 2: and Antarctica, you know, down to the ice and we've 93 00:05:04,960 --> 00:05:09,080 Speaker 2: had low pressure just favoring and continuously moving through the 94 00:05:09,160 --> 00:05:13,280 Speaker 2: Southern Ocean, brushing against the South Island at times, and 95 00:05:13,320 --> 00:05:16,480 Speaker 2: that has been a big reason for our wind, our 96 00:05:16,560 --> 00:05:20,400 Speaker 2: strong westerly wind. Why is that low pressure in the 97 00:05:20,440 --> 00:05:23,960 Speaker 2: Southern Ocean? Why is it there a lot? Well, believed 98 00:05:23,960 --> 00:05:27,000 Speaker 2: it or not, We can trace that back to Antarctica 99 00:05:27,040 --> 00:05:29,560 Speaker 2: of all places. So at the very top of the atmosphere, 100 00:05:29,600 --> 00:05:32,320 Speaker 2: like way at the very top over the South Pole 101 00:05:32,640 --> 00:05:36,080 Speaker 2: back in September, the temperatures got really warm, really fast, 102 00:05:36,240 --> 00:05:39,600 Speaker 2: at least for that part of the atmosphere. And when 103 00:05:39,680 --> 00:05:42,880 Speaker 2: that happened, kind of jumping to the chase, if you will. 104 00:05:43,400 --> 00:05:46,960 Speaker 2: What that did is that that kind of displaced all 105 00:05:47,000 --> 00:05:50,520 Speaker 2: that low pressure that typically favors the Antarctic region, what 106 00:05:50,640 --> 00:05:54,520 Speaker 2: we call the polar vortex. It basically allowed for that 107 00:05:54,560 --> 00:05:59,200 Speaker 2: low pressure to be displaced into the Southern Ocean, and 108 00:05:59,240 --> 00:06:03,599 Speaker 2: because of that, we now have these strong westerly winds, 109 00:06:04,160 --> 00:06:06,359 Speaker 2: big hole in the atmosphere, if you will, over the 110 00:06:06,400 --> 00:06:09,839 Speaker 2: southern ocean, kind of a decent sized mountain near northern 111 00:06:09,880 --> 00:06:14,200 Speaker 2: New Zealand, and that those two features are creating that 112 00:06:14,279 --> 00:06:18,279 Speaker 2: pressure gradient, that change in pressure or as we said before, 113 00:06:18,320 --> 00:06:21,400 Speaker 2: that change in elevation. And this is why we've seen 114 00:06:21,440 --> 00:06:25,200 Speaker 2: these persistent episodes of high wind. We saw them earlier 115 00:06:25,200 --> 00:06:26,720 Speaker 2: in their week, we see we're seeing them now and 116 00:06:26,760 --> 00:06:29,320 Speaker 2: guess what, we're probably gonna see it again next week 117 00:06:29,360 --> 00:06:31,320 Speaker 2: on Labor Day. So just the heads up for those 118 00:06:31,800 --> 00:06:34,080 Speaker 2: getting a headstart on the unofficial start to the I 119 00:06:34,080 --> 00:06:38,400 Speaker 2: guess summer season, be mindful that Monday of next week 120 00:06:38,480 --> 00:06:42,160 Speaker 2: things are still you know, crystallizing, but there will be 121 00:06:42,240 --> 00:06:45,360 Speaker 2: another low coming from the west and north, and that 122 00:06:45,440 --> 00:06:48,000 Speaker 2: will probably bring with it another round of active weather, 123 00:06:48,640 --> 00:06:51,800 Speaker 2: probably not to the degree we're seeing today, but still 124 00:06:51,839 --> 00:06:54,200 Speaker 2: could be quite impactful because it's a big travel day 125 00:06:54,680 --> 00:06:57,160 Speaker 2: and people will be you know, enjoying the public holiday. 126 00:06:57,680 --> 00:07:00,200 Speaker 2: So that is something we could see again. And we 127 00:07:00,200 --> 00:07:04,200 Speaker 2: could see some really cold temperatures, unusually cold temperatures behind 128 00:07:04,240 --> 00:07:08,839 Speaker 2: that on Tuesday, which could impact farmers and livestock because 129 00:07:09,040 --> 00:07:12,720 Speaker 2: we'renowned to the growing season. So because of these big swings, 130 00:07:12,760 --> 00:07:15,280 Speaker 2: like right now in kai Kota, it got to more 131 00:07:15,320 --> 00:07:20,960 Speaker 2: than thirty degrees today, thirty degrees but yeah, and then 132 00:07:20,960 --> 00:07:24,120 Speaker 2: we're talking about much cooler temperatures tomorrow. Then we're talking 133 00:07:24,120 --> 00:07:27,480 Speaker 2: about temperatures going up on Sunday and Monday, Labor Day, 134 00:07:27,520 --> 00:07:30,720 Speaker 2: then going back down on Tuesday. Those big temperature changes, 135 00:07:31,040 --> 00:07:34,520 Speaker 2: they are congruent with wind. Whenever you have these big 136 00:07:34,560 --> 00:07:38,920 Speaker 2: temperature changes, oftentimes a reflection of those temperature changes up 137 00:07:38,960 --> 00:07:42,560 Speaker 2: and down that roller coaster is strong wind. So what 138 00:07:42,560 --> 00:07:46,280 Speaker 2: we're seeing play out high wind, active weather, big temperature changes, 139 00:07:46,440 --> 00:07:47,600 Speaker 2: they're all kind of connected. 140 00:07:47,880 --> 00:07:51,440 Speaker 1: Have we any idea when things should stabilize? 141 00:07:51,560 --> 00:07:54,960 Speaker 2: That's a great question. Look, if you would have asked 142 00:07:55,000 --> 00:07:56,880 Speaker 2: me that, if we were talking like a month ago, 143 00:07:56,880 --> 00:07:58,760 Speaker 2: if you asked me that question, I would have said, 144 00:07:58,800 --> 00:08:02,320 Speaker 2: with a fair bit of confidence, Oh, it'll come right, 145 00:08:04,040 --> 00:08:07,960 Speaker 2: middle second half of October. Well, guess what. We're in 146 00:08:07,960 --> 00:08:10,280 Speaker 2: the second half of October and we're still talking about it. 147 00:08:11,200 --> 00:08:14,240 Speaker 2: What I talked about over Antarctica, that rapid warming at 148 00:08:14,240 --> 00:08:16,240 Speaker 2: the very tippy top of the atmosphere. That's called a 149 00:08:16,240 --> 00:08:19,720 Speaker 2: sudden stratospheric warming event. We just call it SSW. So 150 00:08:19,840 --> 00:08:22,720 Speaker 2: use an SSW drop that in your dinner time conversation. 151 00:08:22,760 --> 00:08:26,640 Speaker 2: You'll raise some eyebrows. That SSW that tends to have 152 00:08:27,120 --> 00:08:33,640 Speaker 2: lingering effects weeks several weeks after. So it looks like 153 00:08:34,160 --> 00:08:38,920 Speaker 2: this sort of pattern where we have active weather, strong westerlies, 154 00:08:38,960 --> 00:08:41,679 Speaker 2: things like that, up and down with temperature. It's probably 155 00:08:41,720 --> 00:08:44,120 Speaker 2: going to continue through at least the rest of October. 156 00:08:44,160 --> 00:08:46,360 Speaker 2: So we got another week or so, and if you 157 00:08:46,400 --> 00:08:48,920 Speaker 2: look at the long range guidance, it actually may go 158 00:08:49,040 --> 00:08:52,600 Speaker 2: into the first ten days of November, so we may 159 00:08:52,640 --> 00:08:55,920 Speaker 2: have to wait until the middle second week, third week 160 00:08:55,960 --> 00:09:00,160 Speaker 2: of November. Once that happens, it will happen eventually. It's 161 00:09:00,200 --> 00:09:03,719 Speaker 2: a matter of being delayed but not denied. But when 162 00:09:03,800 --> 00:09:07,080 Speaker 2: it does happen, the expectation as will have settled weather 163 00:09:07,200 --> 00:09:10,840 Speaker 2: kick in over the country, high pressure and we should 164 00:09:10,920 --> 00:09:14,120 Speaker 2: see a change in the rainfall patterns. So for the 165 00:09:14,200 --> 00:09:17,120 Speaker 2: past couple months, since the beginning of spring, it's the 166 00:09:17,120 --> 00:09:19,640 Speaker 2: west of the South Island that's been getting hammered with 167 00:09:19,760 --> 00:09:24,800 Speaker 2: a lot of rain, mountains, snow, high wind. That's probably 168 00:09:24,800 --> 00:09:27,400 Speaker 2: gonna and we have dry weather for the eastern part 169 00:09:27,440 --> 00:09:30,240 Speaker 2: of the islands, especially up toward Hawk's Bay where they 170 00:09:30,360 --> 00:09:33,880 Speaker 2: have some pretty dry conditions. Once we see that pattern shift, 171 00:09:34,000 --> 00:09:36,480 Speaker 2: our winds are going to shift. And when our wind shift, 172 00:09:37,120 --> 00:09:39,480 Speaker 2: so does the rainfall pattern. So as we work our 173 00:09:39,520 --> 00:09:41,880 Speaker 2: way into the second half of November and into summer 174 00:09:41,920 --> 00:09:48,280 Speaker 2: proper December, January, and February, odds are we should see 175 00:09:48,440 --> 00:09:50,880 Speaker 2: the areas that have been wet Western and lower South 176 00:09:50,920 --> 00:09:53,720 Speaker 2: Island they should become drier, and areas that have been 177 00:09:53,840 --> 00:09:58,600 Speaker 2: dry Hawk's Bay, Eastern Northland, their odds for rainfall should 178 00:09:58,640 --> 00:10:02,280 Speaker 2: start going up. It may take another two three four weeks. 179 00:10:02,320 --> 00:10:02,800 Speaker 2: That happened. 180 00:10:09,080 --> 00:10:10,880 Speaker 1: Our power has gone out in the big Pine Tree, 181 00:10:10,960 --> 00:10:17,880 Speaker 1: one of them has just gone over. There is flying everywhere, 182 00:10:19,040 --> 00:10:21,240 Speaker 1: plastic milk, things flying. 183 00:10:20,960 --> 00:10:24,400 Speaker 2: From god knows where. Stuff is just coming from everywhere 184 00:10:26,080 --> 00:10:28,440 Speaker 2: that the fences are also down. Those deer are going 185 00:10:28,480 --> 00:10:28,920 Speaker 2: to disappear. 186 00:10:29,000 --> 00:10:33,920 Speaker 1: Up that river, a roof ti up, we just lost 187 00:10:33,960 --> 00:10:34,640 Speaker 1: out of the roof. 188 00:10:34,880 --> 00:10:38,360 Speaker 2: But the pine tree shelter about of the neighbors. 189 00:10:37,840 --> 00:10:41,319 Speaker 1: And the trees are just going over like dominoes dog. 190 00:10:42,760 --> 00:10:44,199 Speaker 1: And we're only at one hundred and six k. 191 00:10:44,360 --> 00:10:46,959 Speaker 2: So if we get up to one fifty's going, oh 192 00:10:47,000 --> 00:10:49,640 Speaker 2: my god, turn the power off. 193 00:10:51,000 --> 00:10:51,839 Speaker 1: That roof's gone. 194 00:10:52,280 --> 00:10:54,160 Speaker 2: That's part of it there, and then the other part 195 00:10:54,160 --> 00:10:56,360 Speaker 2: of it is where over the other side of the road. 196 00:10:58,720 --> 00:11:01,320 Speaker 1: Now we all know that climate change has a huge 197 00:11:01,360 --> 00:11:04,720 Speaker 1: impact on weather patterns. I mean, surely by now everybody 198 00:11:04,840 --> 00:11:08,320 Speaker 1: must know this is that what's at play here? Are 199 00:11:08,320 --> 00:11:12,520 Speaker 1: we still within what's called normal weather patterns. 200 00:11:13,000 --> 00:11:19,640 Speaker 2: Look, climate change doesn't cause extreme weather, just like fertilizer 201 00:11:20,080 --> 00:11:24,800 Speaker 2: doesn't make grass grow. It makes it grow better, makes 202 00:11:24,800 --> 00:11:29,199 Speaker 2: it grow faster and overcome things. But climate change does. 203 00:11:29,360 --> 00:11:34,280 Speaker 2: It makes extreme weather a more extreme, b makes it 204 00:11:34,320 --> 00:11:38,280 Speaker 2: more likely to happen, and c makes it more frequent. 205 00:11:39,000 --> 00:11:43,400 Speaker 2: So climate change in itself isn't the culprit for extreme weather. 206 00:11:44,040 --> 00:11:47,360 Speaker 2: Extreme weather has always happened, as we know, but it 207 00:11:47,440 --> 00:11:52,559 Speaker 2: makes the extremes higher or more extreme, and the frequency 208 00:11:52,640 --> 00:11:55,880 Speaker 2: and the likelihood of them grow with climate change. So 209 00:11:56,360 --> 00:11:59,000 Speaker 2: to your you know, if people are wondering this weather 210 00:11:59,080 --> 00:12:02,560 Speaker 2: event that we're seeing now is that because of climate change. Look, 211 00:12:02,559 --> 00:12:05,040 Speaker 2: I'm not a climate change expert. My guess is that 212 00:12:05,240 --> 00:12:07,880 Speaker 2: it's not because of climate change, but there may be 213 00:12:07,920 --> 00:12:11,640 Speaker 2: some footprints of climate change, maybe because of warmer than 214 00:12:11,760 --> 00:12:14,760 Speaker 2: usual oceans around New Zealand the Tasman. See, if you 215 00:12:14,800 --> 00:12:19,080 Speaker 2: have a warmer ocean, warmer than usual, that puts more water, vapor, 216 00:12:19,160 --> 00:12:21,920 Speaker 2: more energy in the air, and that sort of energy 217 00:12:21,960 --> 00:12:26,880 Speaker 2: can help fuel storm. But it's a complex process. No 218 00:12:26,960 --> 00:12:29,439 Speaker 2: one event is caused by climate change, but as I say, 219 00:12:29,559 --> 00:12:33,040 Speaker 2: it makes these events more frequent, more likely, and more intense. 220 00:12:33,600 --> 00:12:36,480 Speaker 1: So easy to think about the damage in sensational terms. 221 00:12:36,559 --> 00:12:39,240 Speaker 1: You know, you've got trees falling on cars, roofs being 222 00:12:39,280 --> 00:12:42,320 Speaker 1: lifted off buildings, et cetera. But there's also things like 223 00:12:42,400 --> 00:12:46,480 Speaker 1: planes being grounded, power outages. I mean, Nelson Hospital suffered 224 00:12:46,480 --> 00:12:49,280 Speaker 1: a forty five minute power outage yesterday, and forty five 225 00:12:49,400 --> 00:12:51,400 Speaker 1: minutes might not seem like a lot, but when you've 226 00:12:51,400 --> 00:12:54,560 Speaker 1: got people hooked up to machines or breathing for them, 227 00:12:55,160 --> 00:12:57,600 Speaker 1: then it's really serious. What are some of the less 228 00:12:57,720 --> 00:13:02,959 Speaker 1: I suppose sensational but still very costly or dangerous risks 229 00:13:03,040 --> 00:13:04,680 Speaker 1: of severe weather well. 230 00:13:04,920 --> 00:13:07,800 Speaker 2: I think people's mental well being is one of them. 231 00:13:08,200 --> 00:13:12,520 Speaker 2: You know, just think about for those who experienced the 232 00:13:12,760 --> 00:13:16,319 Speaker 2: severe weather events back in early twenty twenty three, when 233 00:13:16,360 --> 00:13:19,080 Speaker 2: we had the Auckland Anniversary flooding, and then we had 234 00:13:19,160 --> 00:13:22,720 Speaker 2: cyclone Gabrielle, and then you know, there are other flooding 235 00:13:22,720 --> 00:13:25,760 Speaker 2: events after that, and you just you start to get 236 00:13:25,760 --> 00:13:28,040 Speaker 2: a bit jumpy. I mean I did, and I produce 237 00:13:28,160 --> 00:13:30,920 Speaker 2: is my living and every time there'd be a heavy downpour, 238 00:13:30,960 --> 00:13:33,120 Speaker 2: it kind of triggers you a little bit, you know. 239 00:13:33,240 --> 00:13:37,280 Speaker 2: So I think people's mental health and is one facet 240 00:13:37,400 --> 00:13:41,680 Speaker 2: of how people can be affected adversely by high impact 241 00:13:41,720 --> 00:13:45,440 Speaker 2: weather events. Obviously, your insurance claims, you know, when you 242 00:13:45,480 --> 00:13:47,520 Speaker 2: have to you know, if your house gets destroyed or 243 00:13:47,559 --> 00:13:49,720 Speaker 2: your roof gets torn off, or you have flooding to 244 00:13:49,760 --> 00:13:51,760 Speaker 2: deal with, you're gonna have to put a claim in 245 00:13:52,400 --> 00:13:55,120 Speaker 2: and you know, odds are your claim's gonna your insurance 246 00:13:55,120 --> 00:13:57,080 Speaker 2: premiums are gonna go up, even you know if the 247 00:13:57,080 --> 00:13:59,600 Speaker 2: claim is sorted, and you know, but it's dealing with 248 00:13:59,640 --> 00:14:01,960 Speaker 2: all the sort of those day to day you know, 249 00:14:01,960 --> 00:14:04,160 Speaker 2: your day to day life. I can only imagine, you know, 250 00:14:04,200 --> 00:14:06,199 Speaker 2: if my roof is blown off, you know, it's one 251 00:14:06,200 --> 00:14:08,080 Speaker 2: thing you got to make dinner and go about doing 252 00:14:08,120 --> 00:14:09,880 Speaker 2: your business day to day. But if you have no roof, 253 00:14:10,120 --> 00:14:12,440 Speaker 2: it just throws a complete spanner in the works. It 254 00:14:12,559 --> 00:14:14,720 Speaker 2: just and that goes back to the mental health component. 255 00:14:14,760 --> 00:14:17,520 Speaker 1: I suppose that weather fatigue. 256 00:14:17,679 --> 00:14:21,920 Speaker 2: Hey yeah, yeah, exactly, great, great term fatigue exactly. So 257 00:14:22,080 --> 00:14:24,360 Speaker 2: I mean it's things like that. It's things like maybe 258 00:14:24,800 --> 00:14:27,360 Speaker 2: you know, if you know, it could be if trucks 259 00:14:27,360 --> 00:14:29,920 Speaker 2: are driving and they're they're pushed over on the roadway. 260 00:14:30,400 --> 00:14:32,840 Speaker 2: You know, maybe that's a delivery that doesn't get somewhere, 261 00:14:32,880 --> 00:14:35,960 Speaker 2: so people's businesses, things have to shut down. So maybe 262 00:14:36,000 --> 00:14:38,400 Speaker 2: there's an impact of the economy. So there's a lot 263 00:14:38,440 --> 00:14:41,480 Speaker 2: of sort of I guess, long reaching things that we 264 00:14:41,520 --> 00:14:44,760 Speaker 2: could probably have a pretty long conversation about that it's 265 00:14:44,800 --> 00:14:47,600 Speaker 2: are hard to maybe quantify without you know, that's probably 266 00:14:47,760 --> 00:14:50,400 Speaker 2: kind of a research or a science questions like how 267 00:14:50,400 --> 00:14:53,600 Speaker 2: do you quantify the impacts of a significant weather event 268 00:14:53,680 --> 00:14:56,720 Speaker 2: or a multitude of significant weather events that are in succession, 269 00:14:56,840 --> 00:14:59,560 Speaker 2: you know, how, you know, beside the obvious of you know, 270 00:15:00,080 --> 00:15:03,920 Speaker 2: people's injury and property damage, And I imagine that would 271 00:15:03,920 --> 00:15:06,320 Speaker 2: be long reaching, and that would be kind of from 272 00:15:06,360 --> 00:15:08,920 Speaker 2: a science perspective, kind of fascinating in some ways. I 273 00:15:08,920 --> 00:15:09,920 Speaker 2: would think we're. 274 00:15:09,760 --> 00:15:13,680 Speaker 1: Talking to you on Thursday afternoon, of course, while the 275 00:15:13,680 --> 00:15:16,720 Speaker 1: warnings are still in place. But already there's been a 276 00:15:16,920 --> 00:15:19,320 Speaker 1: tragic death of a man in Willington who was struck 277 00:15:19,360 --> 00:15:22,080 Speaker 1: by a falling branch, and there could be more damage 278 00:15:22,120 --> 00:15:24,440 Speaker 1: and injuries by the time this episode is published. 279 00:15:25,240 --> 00:15:25,720 Speaker 2: But as a. 280 00:15:25,640 --> 00:15:29,960 Speaker 1: Stark reminder, I think of the power of these systems. 281 00:15:30,080 --> 00:15:33,040 Speaker 1: Do we take these things seriously enough? 282 00:15:34,680 --> 00:15:37,640 Speaker 2: Yeah, it's kind of a tough one because I mean, 283 00:15:37,680 --> 00:15:40,840 Speaker 2: the red warnings are really good, because what's built into 284 00:15:40,920 --> 00:15:43,160 Speaker 2: a red warning is like, oh, this is different. I 285 00:15:43,200 --> 00:15:45,760 Speaker 2: need to behave differently, I need to really think about 286 00:15:45,760 --> 00:15:48,000 Speaker 2: my decisions if I'm on if I'm in that red 287 00:15:48,040 --> 00:15:51,880 Speaker 2: warning area. But when you go to other warnings, potentially 288 00:15:53,440 --> 00:15:55,760 Speaker 2: there is an element of like, well, how does this 289 00:15:56,280 --> 00:15:59,400 Speaker 2: event different from another event that maybe isn't quite so severe. 290 00:16:00,120 --> 00:16:02,520 Speaker 2: I know MET Service, we're working with met Service. Obviously. 291 00:16:02,560 --> 00:16:05,520 Speaker 2: MET Service is becoming part of the Earth Sciences New 292 00:16:05,560 --> 00:16:08,160 Speaker 2: Zealand Fauna where you know GNS and NEILO they were separate. 293 00:16:08,200 --> 00:16:10,640 Speaker 2: Now we're one met Service coming into the fold, which 294 00:16:10,680 --> 00:16:13,280 Speaker 2: is great because we need this as a country in 295 00:16:13,360 --> 00:16:15,480 Speaker 2: order to deal with what mother nature throws our away. 296 00:16:15,840 --> 00:16:17,400 Speaker 2: So this is a really good thing. And one of 297 00:16:17,400 --> 00:16:19,480 Speaker 2: the things that I know met Service is doing and 298 00:16:19,480 --> 00:16:23,320 Speaker 2: they're keenon progressing, is kind of changing the warning system 299 00:16:23,640 --> 00:16:27,000 Speaker 2: and improving the warning system. So hopefully those changes will 300 00:16:27,040 --> 00:16:30,320 Speaker 2: will address some of the things that that what your 301 00:16:30,400 --> 00:16:33,360 Speaker 2: question is about. But I think I think at the 302 00:16:33,400 --> 00:16:35,560 Speaker 2: heart of it and any warning system. This could be 303 00:16:35,600 --> 00:16:37,520 Speaker 2: an Aussie, this could be in America, this could be 304 00:16:37,560 --> 00:16:40,720 Speaker 2: in the UK. Is you hear about a warning and 305 00:16:40,760 --> 00:16:42,880 Speaker 2: then oh, yeah, the weather is bad, but maybe you 306 00:16:42,880 --> 00:16:45,600 Speaker 2: didn't have a big impact. Maybe your house didn't get 307 00:16:45,720 --> 00:16:49,560 Speaker 2: you know, damaged, or maybe your property wasn't damaged by 308 00:16:49,600 --> 00:16:53,280 Speaker 2: falling trees, and so you hear there's another warning coming, 309 00:16:53,400 --> 00:16:55,920 Speaker 2: and you know you're gonna go by memory. Well, heck, 310 00:16:55,920 --> 00:16:58,400 Speaker 2: the last time there was a warning, nothing really happened 311 00:16:58,440 --> 00:17:00,400 Speaker 2: to me. So I don't really you know, I don't 312 00:17:00,400 --> 00:17:02,960 Speaker 2: really need to take any action, or oh yeah, there 313 00:17:02,880 --> 00:17:06,000 Speaker 2: a weather forecasters they get it wrong. You know they're 314 00:17:06,000 --> 00:17:08,639 Speaker 2: gonna say this and it doesn't really happen. And so 315 00:17:08,680 --> 00:17:10,840 Speaker 2: there's a bit of that that's a big social science 316 00:17:10,920 --> 00:17:13,919 Speaker 2: question actually, So this is where social sciences play a 317 00:17:14,000 --> 00:17:17,320 Speaker 2: key role into the development of say, weather warnings, and 318 00:17:17,359 --> 00:17:20,240 Speaker 2: how to communicate them and how to how to basically 319 00:17:20,320 --> 00:17:22,879 Speaker 2: frame them in a lot of ways. So there is 320 00:17:22,920 --> 00:17:25,199 Speaker 2: an element of and hopefully I'm answering your question. I 321 00:17:25,240 --> 00:17:27,119 Speaker 2: realize I'm talking a lot, but maybe not giving you 322 00:17:27,160 --> 00:17:29,480 Speaker 2: a useful answer because it's a hard one to articulate 323 00:17:30,359 --> 00:17:32,960 Speaker 2: and it's just not my specialty in terms of social science, 324 00:17:33,200 --> 00:17:35,680 Speaker 2: you know, obviously, but I think, you know, just from 325 00:17:35,680 --> 00:17:38,840 Speaker 2: being in the business for so long, people kind of like, ah, 326 00:17:39,040 --> 00:17:41,320 Speaker 2: she'll be right att itude. Well maybe she won't be, 327 00:17:41,480 --> 00:17:43,959 Speaker 2: you know, Like this is where I think there can 328 00:17:44,000 --> 00:17:47,600 Speaker 2: be some improvements from a science and weather provider perspective. 329 00:17:47,920 --> 00:17:50,080 Speaker 2: But I also think there can be some improvements with 330 00:17:50,200 --> 00:17:54,440 Speaker 2: people really taking you know, some education where people do 331 00:17:54,480 --> 00:17:57,240 Speaker 2: take the warnings more seriously because they often go by 332 00:17:57,280 --> 00:18:00,280 Speaker 2: what happened before, and just because something happened for it 333 00:18:00,320 --> 00:18:02,960 Speaker 2: and didn't result in a bad impact for you, you know, 334 00:18:03,000 --> 00:18:05,680 Speaker 2: your roof being torn off, your house being flooded or damaged, 335 00:18:06,040 --> 00:18:09,800 Speaker 2: it doesn't guarantee that will happen again. Unfortunately, weather forecasts 336 00:18:09,840 --> 00:18:12,639 Speaker 2: that can only be so precise. So when the weather 337 00:18:12,680 --> 00:18:15,720 Speaker 2: warning is issued, they're usually issued for a large area 338 00:18:15,840 --> 00:18:20,360 Speaker 2: like Canterbury. Canterbury is a huge area, but the impacts 339 00:18:20,840 --> 00:18:23,600 Speaker 2: can be quite variable in Canterbury, you know, unless it's 340 00:18:23,600 --> 00:18:26,760 Speaker 2: something has still worked, like Gabrielle, where there was really 341 00:18:26,920 --> 00:18:30,479 Speaker 2: widespread damage. But even then there were you know, not 342 00:18:30,680 --> 00:18:32,800 Speaker 2: you know, there were landslips in one place is but 343 00:18:32,840 --> 00:18:35,560 Speaker 2: not in the other. Some rivers had really really bad flooding, 344 00:18:35,680 --> 00:18:39,400 Speaker 2: some didn't. So part of it, too, is that warnings 345 00:18:39,400 --> 00:18:42,840 Speaker 2: are issued for broad areas, but there can be variable 346 00:18:42,960 --> 00:18:45,920 Speaker 2: impacts within that warning area. Some could have really really 347 00:18:45,960 --> 00:18:50,040 Speaker 2: high impacts and some areas the impacts would be quite pedestrian. 348 00:18:50,080 --> 00:19:03,800 Speaker 2: If at all this is hid, I'll get here. They're 349 00:19:03,800 --> 00:19:10,480 Speaker 2: gonna be paid for all, guys. WHOA. 350 00:19:12,280 --> 00:19:20,679 Speaker 1: Look, I've heard a lot of people wondering where is spring, 351 00:19:21,720 --> 00:19:23,560 Speaker 1: And I've heard a lot of talk people talk about 352 00:19:24,240 --> 00:19:28,720 Speaker 1: whether the seasons are changing. So at what point do 353 00:19:28,760 --> 00:19:33,280 Speaker 1: you think we scraped with the current season calendar altogether 354 00:19:33,400 --> 00:19:35,720 Speaker 1: and shift everything by a month and call it a day. 355 00:19:36,600 --> 00:19:42,520 Speaker 2: No, I can't do that. Look, seasons are a human construct, right, 356 00:19:42,600 --> 00:19:46,080 Speaker 2: The seasons are changing in the way and we had 357 00:19:46,119 --> 00:19:49,680 Speaker 2: a scientist who since passed on, but doctor Brett Mullen, 358 00:19:49,760 --> 00:19:51,920 Speaker 2: I remember when I first came to at the time NIWA. 359 00:19:53,320 --> 00:19:56,040 Speaker 2: He did a bit of, you know, I guess, a 360 00:19:56,040 --> 00:20:00,359 Speaker 2: bit of an investigation on have has the have the 361 00:20:00,359 --> 00:20:02,840 Speaker 2: seasons changed? And what he did is he looked at 362 00:20:02,880 --> 00:20:07,560 Speaker 2: when the first frost occurred and for select locations around 363 00:20:07,600 --> 00:20:10,280 Speaker 2: the country. And it turned out, and I'm going off 364 00:20:10,320 --> 00:20:14,280 Speaker 2: memory here, hopefully I don't, Butcher his his his findings 365 00:20:14,760 --> 00:20:20,520 Speaker 2: that basically frosts were happening later in autumn. So the 366 00:20:20,560 --> 00:20:23,760 Speaker 2: first frost, you know, it's happening later, deeper into the season, 367 00:20:24,600 --> 00:20:28,240 Speaker 2: and the last frost was happening in springtime was happening earlier. 368 00:20:28,800 --> 00:20:34,000 Speaker 2: So what happens is that the shoulder seasons are getting warmer, 369 00:20:34,119 --> 00:20:37,880 Speaker 2: the shoulder seasons being autumn and spring, right, So what 370 00:20:37,920 --> 00:20:41,359 Speaker 2: we're seeing is that the warmth is lingering longer. So 371 00:20:41,480 --> 00:20:44,840 Speaker 2: when summer ends, we enter autumn, and that warmth is 372 00:20:44,960 --> 00:20:47,479 Speaker 2: lingering a bit longer and longer, and it takes longer 373 00:20:47,480 --> 00:20:51,200 Speaker 2: for that first frost to occur. Also in springtime, we're 374 00:20:51,240 --> 00:20:54,359 Speaker 2: warming up a bit sooner, so the last frost happens 375 00:20:54,400 --> 00:20:57,440 Speaker 2: a bit earlier, so using that as a metric. Yeah, 376 00:20:57,840 --> 00:21:01,879 Speaker 2: the seasons are evolving, but looks people are probably like, 377 00:21:02,080 --> 00:21:05,320 Speaker 2: where a spring? This is spring, man, this is spring. Now, 378 00:21:05,359 --> 00:21:08,639 Speaker 2: I admittedly this is spring kind of next level with 379 00:21:08,800 --> 00:21:11,439 Speaker 2: the high wind and we've seen these damaging wind events. 380 00:21:11,440 --> 00:21:12,520 Speaker 2: We've seen a lot of rain. 381 00:21:14,040 --> 00:21:17,639 Speaker 1: This is spring heating puberty. 382 00:21:18,040 --> 00:21:21,520 Speaker 2: Well said, Yeah, but even even if this spring weren't 383 00:21:21,520 --> 00:21:25,000 Speaker 2: as volatile or as active, and it was maybe a 384 00:21:25,040 --> 00:21:29,159 Speaker 2: notch lower, this would be pretty typical. Acknowledging today and 385 00:21:29,200 --> 00:21:32,159 Speaker 2: Tuesday and other days have not been typical. Just that 386 00:21:32,200 --> 00:21:34,159 Speaker 2: if they were brought down a bit, you know, you 387 00:21:34,200 --> 00:21:37,280 Speaker 2: know that's normal. You know, spring has ups and downs. 388 00:21:37,280 --> 00:21:39,879 Speaker 2: It is the teenager of the seasons. 389 00:21:40,000 --> 00:21:42,760 Speaker 1: Very Moody, thanks for joining us, Chris. 390 00:21:42,840 --> 00:21:43,600 Speaker 2: Thanks for having me. 391 00:21:46,359 --> 00:21:49,480 Speaker 1: That's it for this episode of the Front Page. You 392 00:21:49,520 --> 00:21:53,280 Speaker 1: can read more about today's stories and extensive news coverage 393 00:21:53,320 --> 00:21:56,840 Speaker 1: at ends a Herald, dot co, dot enz. The Front 394 00:21:56,880 --> 00:21:59,960 Speaker 1: Page is produced by Jane Ye and Richard Martin, who 395 00:22:00,200 --> 00:22:04,800 Speaker 1: also our editor. I'm Chelsea Daniels. Subscribe to the Front 396 00:22:04,840 --> 00:22:08,359 Speaker 1: Page on iHeartRadio or wherever you get your podcasts, and 397 00:22:08,400 --> 00:22:11,760 Speaker 1: tune in on Monday for another look behind the headlines,