Hhhhhh
Bookcase mixed with display shelves - gives more visual interest than traditional
Choosing a noun well will allow you to cut adjectives. This tightens your sentences and clarifies the meaning:
a young tree -> sapling
a single-storey house -> a bungalow
a young female horse -> a filly
her long thick hair -> her mane
a prudish person -> a prude.
his bald scalp -> his pate
an unpleasant smell -> a stench
a small child -> a toddler
a brown-haired woman -> a brunette
Of course, the choice of noun depends on context, but if you can use one word, why use two?
Writing style. If you have a lush writing style, you would use more adjectives compared to a terse one. However, more than three adjectives in a sentence will slow down the story.
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Matching Storage / display in shower & toilet area.
Window bench adjacent to dining space. Built-in bench with wood siding to differentiate the window bench area.
How to be an adult
"How to Life" Masterlist
Make your bed in the morning. It takes seconds, and it's worth it.
Reset to zero each morning.
Use the UFYH 20/10 system for clearing your shit.
Have a 'drop-zone' box where you dump anything and everything. At the beginning/end of the day, clear it out and put that shit away.
Automate your chores. Have a cleaning schedule and assign 15mins daily to do whatever cleaning tasks are set for that day. Set a timer and do it once the timer is up, finish the task you're on and leave it for the day.
Fold your clothes straight out of the tumble dryer (if you use one), whilst they're still warm. This minimises creases and eliminates the need for ironing.
Clean your footwear regularly and you'll feel like a champ.
Learn from Eisenhower's Importance/Urgency matrix.
Try out the two-minute rule and the Pomodoro technique.
Use. A. Planner. (Or Google Calendar, if that's more your thing.)
Try bullet journalling.
Keep a notebook/journal/commonplace book to dump your brain contents in on the regular.
Set morning alarms at two-minute intervals rather than five, and stick your alarm on the other side of the room. It's brutal, but it works.
Set three main goals each day, with one of them being your #1 priority. Don't overload your to-do list or you'll hit overload paralysis and procrastinate.
If you're in a slump, however, don't be afraid to put things like "shower" on your to do list - that may be a big enough goal in itself, and that's okay.
Have a physical inbox - a tray, a folder, whatever. If you get a piece of paper, stick it in there and sort through it at the end of the week.
Consider utilising the GTD System, or a variation of it.
Try timeboxing.
Have a morning routine, and guard that quiet time ferociously.
Have a folder for all your important documents and letters, organised by topic (e.g. medical, bank, university, work, identification). At the front of this folder, have a sheet of paper with all the key information written on it, such as your GP's details, your passport details, driving licence details, bank account number, insurance number(s), and so on.
Schedule working time and down time alike, in the balance that works for you.
Have. A. God. Damn. Budget.
Use a money tracker like toshl, mint, or splitwise. Enter all expenses asap! (You will forget, otherwise.)
Have a 'money date' each week, where you sort through your finances from the past seven days and then add it to a spreadsheet. This will help you identify your spending patterns and whether your budget is actually working or not.
Pack your own frickin' lunch like a grown-up and stop buying so many takeaway coffees. Keep snacks in your bag.
Know how to cook the basics: a starch, a protein, a vegetable, and a sauce.
Simple, one-pot meals ("a grain, a green, and a bean") are a godsend.
Batch cook and freeze. Make your own 'microwave meals'.
Buy dried goods to save money - rice and beans are a pittance.
Consider Meatless Mondays; it's healthier, cheaper, and more environmentally friendly.
Learn which fruits and vegetables are cheapest at your store, and build a standard weekly menu around those. (Also remember that frozen vegetables are cheap and healthy.)
Learn seasoning combinations. Different seasoning, even with the exact same ingredients, can make a dish seem completely new.
Have a stock email-writing format.
Want to start running, but find it boring? Try Zombies, Run!.
Keep a goddamn first aid kit and learn how to use it.
Update your CV regularly.
Keep a selection of stamps and standard envelopes for unexpected posting needs. (It happens more regularly than you would think!)
The Cathedral, Storr - Isle of Skye
New limited edition print.
Photographed by Freddie Ardley
www.freddieardley.com/prints
You may have seen the news that 2023 was the hottest year in NASA’s record, continuing a trend of warming global temperatures. But have you ever wondered what in the world that actually means and how we know?
We talked to some of our climate scientists to get clarity on what a temperature record is, what happened in 2023, and what we can expect to happen in the future… so you don’t have to!
The short answer: Human activities. The release of greenhouse gases like carbon dioxide and methane into the atmosphere trap more heat near Earth’s surface, raising global temperatures. This is responsible for the decades-long warming trend we’re living through.
But this year’s record wasn’t just because of human activities. The last few years, we’ve been experiencing the cooler phase of a natural pattern of Pacific Ocean temperatures called the El Niño Southern Oscillation (ENSO). This phase, known as La Niña, tends to cool temperatures slightly around the world. In mid-2023, we started to shift into the warmer phase, known as El Niño. The shift ENSO brought, combined with overall human-driven warming and other factors we’re continuing to study, pushed 2023 to a new record high temperature.
Almost certainly not. Although the overall trend in annual temperatures is warmer, there’s some year-to-year variation, like ENSO we mentioned above.
Think about Texas and Minnesota. On the whole, Texas is warmer than Minnesota. But some days, stormy weather could bring cooler temperatures to Texas while Minnesota is suffering through a local heat wave. On those days, the weather in Minnesota could be warmer than the weather in Texas. That doesn’t mean Minnesota is warmer than Texas overall; we’re just experiencing a little short-term variation.
Something similar happens with global annual temperatures. The globe will naturally shift back to La Niña in the next few years, bringing a slight cooling effect. Because of human carbon emissions, current La Niña years will be warmer than La Niña years were in the past, but they’ll likely still be cooler than current El Niño years.
Technically, NASA’s global temperature record starts in 1880. NASA didn’t exist back then, but temperature data were being collected by sailing ships, weather stations, and scientists in enough places around the world to reconstruct a global average temperature. We use those data and our modern techniques to calculate the average.
We start in 1880, because that’s when thermometers and other instruments became technologically advanced and widespread enough to reliably measure and calculate a global average. Today, we make those calculations based on millions of measurements taken from weather stations and Antarctic research stations on land, and ships and ocean buoys at sea. So, we can confidently say 2023 is the warmest year in the last century and a half.
However, we actually have a really good idea of what global climate looked like for tens of thousands of years before 1880, relying on other, indirect ways of measuring temperature. We can look at tree rings or cores drilled from ice sheets to reconstruct Earth’s more ancient climate. These measurements affirm that current warming on Earth is happening at an unprecedented speed.
It’s literally our job! When NASA was formed in 1958, our original charter called for “the expansion of human knowledge of phenomena in the atmosphere and space.” Our very first space missions uncovered surprises about Earth, and we’ve been using the vantage point of space to study our home planet ever since. Right now, we have a fleet of more than 20 spacecraft monitoring Earth and its systems.
Why we created our specific surface temperature record – known as GISTEMP – actually starts about 25 million miles away on the planet Venus. In the 1960s and 70s, researchers discovered that a thick atmosphere of clouds and carbon dioxide was responsible for Venus’ scorchingly hot temperatures.
Dr. James Hansen was a scientist at the Goddard Institute for Space Studies in New York, studying Venus. He realized that the greenhouse effect cooking Venus’ surface could happen on Earth, too, especially as human activities were pumping carbon dioxide into our atmosphere.
He started creating computer models to see what would happen to Earth’s climate as more carbon dioxide entered the atmosphere. As he did, he needed a way to check his models – a record of temperatures at Earth’s surface over time, to see if the planet was indeed warming along with increased atmospheric carbon. It was, and is, and NASA’s temperature record was born.
The temperature record is a global average, so not everywhere on Earth experienced record heat. Local differences in weather patterns can influence individual locations to be hotter or colder than the globe overall, but when we average it out, 2023 was the hottest year.
Just because you didn’t feel record heat this year, doesn’t mean you didn’t experience the effects of a warming climate. 2023 saw a busy Atlantic hurricane season, low Arctic sea ice, raging wildfires in Canada, heat waves in the U.S. and Australia, and more.
And these effects don’t stay in one place. For example, unusually hot and intense fires in Canada sent smoke swirling across the entire North American continent, triggering some of the worst air quality in decades in many American cities. Melting ice at Earth’s poles drives rising sea levels on coasts thousands of miles away.
Our global temperature record doesn’t actually track absolute temperatures. Instead, we track temperature anomalies, which are basically just deviations from the norm. Our baseline is an average of the temperatures from 1951-1980, and we compare how much Earth’s temperature has changed since then.
Why focus on anomalies, rather than absolutes? Let’s say you want to track if apples these days are generally larger, smaller, or the same size as they were 20 years ago. In other words, you want to track the change over time.
Apples grown in Florida are generally larger than apples grown in Alaska. Like, in real life, how Floridian temperatures are generally much higher than Alaskan temperatures. So how do you track the change in apple sizes from apples grown all over the world while still accounting for their different baseline weights?
By focusing on the difference within each area rather than the absolute weights. So in our map, the Arctic isn’t red because it’s hotter than Bermuda. It’s red because it’s gotten relatively much warmer than Bermuda has in the same time frame.
Want to learn more about climate change? Dig into the data at climate.nasa.gov.
Make sure to follow us on Tumblr for your regular dose of space!