lokalni.ailokalni.ai⁄Stejný vstup, stejný výstup⁄Qwen3-4B · vLLM · greedy on L40S · L40S

helloHello! Who are you?

reference: A100, E1 greedy, r0 · 50 tokens · r0–9 identical
Hello! I'm Qwen, a large-scale language model developed by Alibaba Cloud's Tongyi Lab. I can assist you with answering questions, writing stories, creating documents, coding, and more. How can I help you today? 😊

factExplain why the sky is blue during the day and why sunsets are often red or orange. Cover the physics involved and mention how atmospheric conditions such as dust or pollution change the colors.

reference: A100, E1 greedy, r0 · 896 tokens · no run identical
The colors of the sky during the day and at sunset are due to a phenomenon in physics known as **Rayleigh scattering**. This process explains how sunlight interacts with the molecules and small particles in Earth's atmosphere. --- ### 🌞 Why the Sky is Blue During the Day Sunlight, or white light, is made up of different colors, each with a different wavelength. The visible spectrum ranges from short-wavelength violet and blue to long-wavelength red and orange. - **Rayleigh scattering** occurs when light interacts with particles much smaller than the wavelength of the light—such as nitrogen and oxygen molecules in the atmosphere. - The intensity of scattering is **inversely proportional to the fourth power of the wavelength**: \[ I \propto \frac{1}{\lambda^4} \] This means **shorter wavelengths (blue and violet)** are scattered much more strongly than longer wavelengths (red, orange, yellow). - As sunlight enters the atmosphere, blue and violet light are scattered in all directions by air molecules. This scattered blue light reaches our eyes from all directions, making the sky appear blue. - Although violet light is scattered even more than blue, our eyes are less sensitive to violet, and some of it is absorbed by the upper atmosphere (by ozone), so we perceive the sky as **blue**, not violet. --- ### 🌅 Why Sunsets Are Red or Orange At sunset (or sunrise), the sun is near the horizon, so sunlight must pass through a much thicker layer of the atmosphere to reach our eyes. - As the light travels through more atmosphere, **more of the shorter wavelengths (blue and green)** are scattered out of the direct path. - The longer wavelengths (red, orange, and yellow) are scattered much less and continue traveling in a straight line. - As a result, the direct sunlight that reaches us is dominated by red and orange hues. This is why the sun appears red or orange at sunrise and sunset. --- ### 🌫️ How Dust, Pollution, and Atmospheric Conditions Change the Colors Atmospheric conditions can significantly alter the colors we see: 1. **Dust or Pollution (e.g., smog, smoke, haze):** - Larger particles (like dust, smoke, or pollution) scatter light differently than gas molecules. - These particles cause **Mie scattering**, which scatters all wavelengths more equally (not just blue). - This can result in **duller, more uniform colors** or even **grayish skies**. - In hazy conditions, the blue sky may appear washed out, and sunsets may appear more yellow or gray rather than vibrant reds. 2. **High Pollution or Smoke (e.g., wildfires):** - Particles can absorb and scatter light in ways that enhance reds and oranges or even produce **intense, vivid red sunsets** due to the dominance of longer wavelengths. - In some cases, pollution can create a **"hazy red" or "orange" sky** even during the day. 3. **Clean, Clear Air:** - In pristine conditions, Rayleigh scattering is dominant, leading to a **bright blue sky** and **vivid red/orange sunsets**. 4. **High Altitude or Thin Atmosphere (e.g., mountains, space):** - With less atmosphere, less scattering occurs, so the sky appears darker or even black during the day, and sunsets are less dramatic. --- ### Summary | Phenomenon | Cause | |----------|-------| | Blue sky during the day | Rayleigh scattering of short-wavelength blue light by air molecules | | Red/orange sunsets | Long-wavelength red/orange light travels through more atmosphere and is less scattered | | Dust/pollution | Causes Mie scattering, reducing blue and making skies appear hazy or duller; can enhance reds in certain conditions | ✅ In essence: **Blue light scatters more than red light**, and the path of sunlight changes at sunrise/sunset, altering which colors reach our eyes. So, the sky is blue because of how light scatters in the atmosphere—and sunsets are red because the blue light gets scattered away, leaving the reds to dominate. Atmospheric particles can modify this effect, making colors more or less vivid depending on conditions. 🌍🌤️🌅
r0–9 · differs from token 12 · 879 tokens
The colors of the sky during the day and at sunset are primarily due to a phenomenon in physics known as **Rayleigh scattering**. This process explains how sunlight interacts with the molecules and small particles in Earth's atmosphere. --- ### 🌞 Why the Sky is Blue During the Day Sunlight, or white light, is made up of a spectrum of colors, each with a different wavelength. The visible spectrum ranges from short-wavelength violet and blue to longer-wavelength red and orange. - **Rayleigh scattering** occurs when light interacts with particles much smaller than the wavelength of the light—such as nitrogen and oxygen molecules in the atmosphere. - The intensity of scattering is **inversely proportional to the fourth power of the wavelength**: \[ I \propto \frac{1}{\lambda^4} \] This means **shorter wavelengths (blue and violet)** are scattered much more strongly than longer wavelengths (red, orange, yellow). - As sunlight enters the atmosphere, blue and violet light are scattered in all directions by air molecules. This scattered blue light reaches our eyes from all directions, making the sky appear blue. - Although violet light is scattered even more than blue, our eyes are less sensitive to violet, and some of it is absorbed by the upper atmosphere (especially by ozone), so we perceive the sky as **blue**, not violet. --- ### 🌅 Why Sunsets Are Red or Orange At sunset (or sunrise), the sun is near the horizon, so sunlight must pass through a much thicker layer of the atmosphere to reach our eyes. - As the light travels through more atmosphere, **more of the shorter wavelengths (blue and green)** are scattered out of the direct path. - The longer wavelengths (red, orange, and yellow) are scattered much less and continue to travel in a straight line through the atmosphere. - These longer wavelengths reach our eyes directly, making the sun and the surrounding sky appear **red, orange, or pink**. This is why sunsets are often vividly colored—longer wavelengths dominate the direct beam of sunlight after most of the blue light has been scattered away. --- ### 🌫️ How Dust, Pollution, and Atmospheric Conditions Change the Colors Atmospheric conditions can significantly alter the colors we see: 1. **Pollution and Dust (e.g., smog, sandstorms)**: - Larger particles (like dust, smoke, or pollution) scatter light differently than gas molecules. - These particles cause **Mie scattering**, which affects all wavelengths more equally and does not depend on wavelength as strongly as Rayleigh scattering. - As a result, the sky may appear **gray, hazy, or white**, and sunsets may appear **duller or more yellow/orange** rather than vibrant reds. - In some cases, pollution can enhance red or orange hues by scattering blue light and allowing reds to dominate, but the overall effect is often muted due to the even scattering across wavelengths. 2. **High Humidity or Clouds**: - Clouds scatter light in all directions and can create white or gray skies. - When the sun is low, clouds can reflect and diffuse sunlight, producing soft, warm hues (like orange or pink) due to the combination of scattered reds and diffused light. 3. **Clean, Clear Air**: - In pristine conditions, Rayleigh scattering is most effective, leading to a bright blue sky and vivid red sunsets. --- ### Summary | Phenomenon | Cause | |----------|-------| | Blue sky during the day | Rayleigh scattering of short blue wavelengths by air molecules | | Red/orange sunsets | Long-wavelength red/orange light travels through more atmosphere, with blue light scattered away | | Dust/pollution effects | Mie scattering reduces blue scattering, leading to hazy skies and muted or altered sunset colors | ✅ In essence: **Blue light scatters more than red light in the atmosphere, so we see blue during the day and red/orange at sunset.** Atmospheric particles like dust or pollution alter this scattering, changing the intensity and hue of the colors we observe. This beautiful interplay of light and matter is a classic example of how simple physical principles govern everyday natural phenomena. 🌍✨

storyWrite a short story about a lighthouse keeper on a remote island who finds a message in a bottle that seems to be addressed to them personally.

reference: A100, E1 greedy, r0 · 805 tokens · no run identical
The wind howled across Blackthorn Point, a jagged island clawed from the sea, its cliffs slick with salt and spray. Elias Thorne, the lighthouse keeper, stood at the tall, weathered glass of the lantern room, his breath fogging the cold pane. For twenty-three years, he’d watched the endless grey expanse, the relentless rhythm of waves crashing against the rocks below. His world was predictable: oil, wicks, the turn of the great clockwork gears, the occasional seabird or the distant cry of a gull. Routine, like the sea, was his only companion. Then, one rain-lashed morning, while sweeping the stone steps leading down to the sea wall, he found it. Tucked beneath a loose stone, half-buried in damp moss, was a small, unremarkable bottle. It was made of thick, green glass, the kind from the 1800s, its surface pitted and faded. No label. No seal. Just the bottle itself, heavy and cold in his hands. Curiosity, a rare spark in his otherwise monotonous life, made him open it. Inside, a single sheet of yellowed paper, brittle as old parchment, lay folded neatly. The ink was faded, the script delicate and hurried. *To Elias Thorne, Keeper of Blackthorn Point,* *If you are reading this, the storm has passed. The sea is calm. I am not who you think. I am not lost. I am here. I have been waiting. I know the light you keep. I know the rhythm of your watch. I know the name of the storm that took my brother. I know the name of the girl who sang to the waves when the fog rolled in. I know you remember. I know you remember her.* *You are not alone. I am not gone. I am here, in the silence between the waves. I am the echo in the wind. I am the light that flickers when the sea is still. I am the message you never sent.* *Find the cove. The one with the black rocks and the silver tide. There, beneath the old oak, you will find a stone. Carved with a single word: "Remember."* *—Someone who remembers.* Elias stared at the words, his heart pounding in his chest. *Someone who remembers.* The name of the girl? The storm that took his brother? He’d never spoken of the storm. He’d never spoken of the girl. He’d buried the memory deep, like the old oak tree in the cove, long since fallen. He’d thought the island was empty. That the sea had swallowed all that was lost. He went to the cove, the one with the black rocks and the silver tide. The wind was still, the sea calm. He found the old oak, its roots long gone, but beneath the moss-covered stone at its base, he found it — a smooth, cold stone, carved with a single word, etched in a hand that seemed to know his own. *Remember.* He sat on the wet rocks, the bottle in his hand, the words echoing in the silence. For the first time in decades, he didn’t feel alone. He didn’t feel the weight of the sea or the cold of the wind. He felt something else — a warmth, a quiet understanding. He looked up at the lighthouse, its beam cutting through the grey sky. The light was steady. The light was *alive*. And for the first time, Elias Thorne smiled. Not because he had found a secret, but because he had finally remembered — not just the past, but the presence of someone who had been there all along, watching, waiting, and remembering. The sea was still. The light burned. And somewhere, in the quiet between the waves, a message had been answered.
r0–9 · differs from token 13 · 858 tokens
The wind howled across Blackthorn Point, a jagged tooth of rock rising from the churning North Sea. Elias Thorne, the lighthouse keeper, stood at the iron railing, his face etched with the salt and wind. For twenty-three years, he’d watched the endless grey expanse, his life measured in tides and storms. The light, a steady beam cutting through the fog, was his only companion, his only purpose. He’d found the bottle half-buried in the damp sand near the base of the cliff, a small, chipped glass vessel, its surface pitted by time. It wasn’t the usual driftwood or seaweed. This was different. Clean, almost new, the glass held a faint, oily sheen. Inside, nestled in a folded piece of yellowed paper, was a single sentence, written in a looping, elegant hand: *"To Elias Thorne, Keeper of Blackthorn Point: If you read this, the sea has spoken. It remembers your name. It remembers the storm of '87. Find the stone beneath the old oak. It holds the key to the silence."* Elias froze. *'87*? The storm that had swallowed the fishing village of Seabrook, the one that had taken his sister, Clara? He’d been on duty that night, the light blazing, the fog so thick it felt like a physical wall. He’d seen the boats vanish, heard the screams, but the official report said the storm was too fierce. He’d buried Clara’s letters in the old oak tree, a promise to himself to never forget. The stone beneath the oak? He’d never seen it. The oak was ancient, gnarled, and the roots were deep in the cliffside. He didn’t believe in messages from the sea. He believed in the wind, the tides, the relentless rhythm of the waves. But this… this felt like a whisper from the past, a ghost of Clara’s voice. That night, he lit the lamp, the beam sweeping the dark water. He walked to the old oak, its trunk twisted like a serpent. He knelt, brushing away centuries of moss and salt. Beneath the roots, half-buried in damp earth, was a smooth, dark stone, cool and heavy. He picked it up. It felt familiar, like a piece of his own memory. He returned to the cottage, the bottle in his hand. He placed it on the mantel, where the wind could not reach it. The next morning, he found a second note, tucked inside the first, written in the same hand: *"The silence is not empty, Elias. It is waiting. The stone is not a key. It is a mirror. Look into it, and you will see what the sea has hidden from you."* He didn’t sleep. He sat by the window, the stone in his palm. He thought of Clara, of the storm, of the way she’d always said the sea was full of stories, stories only the wind and the tide could carry. He thought of the silence after the storm, the silence that had followed her death. That night, he placed the stone on the table beside the lamp. As the beam swept across the water, he closed his eyes and whispered, “Clara?” The stone didn’t glow. But the light from the lamp caught the surface of the sea, and for a moment, the waves didn’t look like water. They looked like ripples, like breath. And in the reflection, he saw a figure—tall, in a blue coat, standing on the shore, holding a small, folded letter. He opened his eyes. The sea was still. The wind had died. The stone was cold. He didn’t know if it was a message from the sea, or from Clara. He didn’t know if the stone was a key or a mirror. But for the first time in twenty-three years, Elias Thorne felt the silence not as emptiness, but as presence. And in that quiet, he finally understood: the sea had not forgotten. It had simply been waiting for him to listen.

mathA train leaves Plzeň at 8:15 and travels toward Prague at an average speed of 72 km/h. A second train leaves Prague at 8:45 toward Plzeň at 90 km/h. The distance between the two cities along the track is 114 km. At what time do the trains meet, and how far from Plzeň? Solve it step by step and state the final answer clearly.

reference: A100, E1 greedy, r0 · 1024 tokens · no run identical
Let's solve the problem step by step. --- ### **Given:** - Distance between Plzeň and Prague: **114 km** - Train A (from Plzeň) leaves at **8:15** at **72 km/h** - Train B (from Prague) leaves at **8:45** at **90 km/h** - We are to find: - The **time** when the two trains meet - The **distance from Plzeň** to the meeting point --- ### **Step 1: Determine how long Train A travels before Train B starts** Train A starts at 8:15, Train B at 8:45. Time difference = 8:45 − 8:15 = **30 minutes** = **0.5 hours** In that time, Train A travels: $$ \text{Distance} = \text{Speed} \times \text{Time} = 72 \, \text{km/h} \times 0.5 \, \text{h} = 36 \, \text{km} $$ So, when Train B starts at 8:45, the two trains are **36 km apart** (Train A has already covered 36 km from Plzeň). --- ### **Step 2: After 8:45, both trains are moving toward each other** Now, both trains are moving toward each other: - Train A speed: 72 km/h - Train B speed: 90 km/h - Combined speed: $$ 72 + 90 = 162 \, \text{km/h} $$ Remaining distance between them at 8:45: $$ 114 \, \text{km} - 36 \, \text{km} = 78 \, \text{km} $$ Time to meet after 8:45: $$ \text{Time} = \frac{\text{Distance}}{\text{Speed}} = \frac{78}{162} \, \text{hours} $$ Simplify the fraction: $$ \frac{78}{162} = \frac{13}{27} \, \text{hours} $$ Convert to minutes: $$ \frac{13}{27} \times 60 = \frac{780}{27} \approx 28.888... \, \text{minutes} $$ Break it down: - 28 minutes - 0.888... × 60 ≈ 53.33 seconds So, approximately **28 minutes and 53 seconds** --- ### **Step 3: Add this time to 8:45 to get the meeting time** 8:45 + 28 minutes = **9:13** Then + 53 seconds → **9:13:53** So, the trains meet at approximately **9:13 and 53 seconds** But we can keep it as a precise time. Alternatively, we can express the meeting time exactly. --- ### **Step 4: Find distance from Plzeň to meeting point** We can compute this in two ways: #### **Option 1: Distance traveled by Train A from 8:15 to meeting time** - Time from 8:15 to meeting time: - From 8:15 to 8:45 = 30 minutes = 0.5 h - From 8:45 to meeting = $ \frac{13}{27} $ h - Total time = $ 0.5 + \frac{13}{27} = \frac{1}{2} + \frac{13}{27} $ Convert to common denominator: $$ \frac{1}{2} = \frac{27}{54}, \quad \frac{13}{27} = \frac{26}{54} $$ Wait — better to use 54: $$ \frac{1}{2} = \frac{27}{54}, \quad \frac{13}{27} = \frac{26}{54} $$ No — actually: $$ \frac{1}{2} = \frac{27}{54}? \quad \text{No: } \frac{1}{2} = \frac{27}{54} \text{ is wrong. } \frac{1}{2} = \frac{27}{54}? 27/54 = 1/2 → yes, correct. $$ $$ \frac{
r0–9 · differs from token 263 · 1024 tokens
…Speed} \times \text{Time} = 72 \, \text{km/h} \times 0.5 \, \text{h} = 36 \, \text{km} $$ So, when Train B starts at 8:45, the two trains are **36 km apart** (since Train A has already covered 36 km from Plzeň). --- ### **Step 2: Determine the remaining distance between the two trains at 8:45** Total distance = 114 km Distance already covered by Train A = 36 km Remaining distance = 114 − 36 = **78 km** --- ### **Step 3: Determine the relative speed when both trains are moving** Train A: 72 km/h Train B: 90 km/h Combined speed (closing speed) = 72 + 90 = **162 km/h** --- ### **Step 4: Time to meet after 8:45** They are 78 km apart and closing at 162 km/h. $$ \text{Time} = \frac{\text{Distance}}{\text{Speed}} = \frac{78}{162} \text{ hours} $$ Simplify the fraction: $$ \frac{78}{162} = \frac{13}{27} \text{ hours} $$ Convert to minutes: $$ \frac{13}{27} \times 60 = \frac{780}{27} \approx 28.888... \text{ minutes} $$ $$ 28.888... = 28 \text{ minutes} + 0.888... \times 60 \approx 28 \text{ min } 53.3 \text{ sec} $$ So, approximately **28 minutes and 53 seconds** --- ### **Step 5: Add this time to 8:45 to get the meeting time** 8:45 + 28 minutes = 9:13 + 53 seconds = **9:13:53** So, the trains meet at approximately **9:13 and 53 seconds**. But let's keep it precise. --- ### **Step 6: Find the distance from Plzeň to the meeting point** We can compute it in two ways: #### **Option 1: Distance covered by Train A from 8:15 to meeting time** - Time from 8:15 to meeting time = 0.5 h (to 8:45) + 13/27 h = $$ \frac{1}{2} + \frac{13}{27} = \frac{27}{54} + \frac{26}{54} = \frac{53}{54} \text{ hours} $$ - Distance = 72 km/h × (53/54) h $$ = 72 \times \frac{53}{54} = \frac{72}{54} \times 53 = \frac{4}{3} \times 53 = \frac{212}{3} \approx 70.67 \text{ km} $$ #### **Option 2: Distance covered by Train B** Time from 8:45 to meeting = 13/27 h Distance = 90 × (13/27) = (1170)/27 = 43.333... km Now, total distance covered = 70.67 + 43.33 = 114 km ✅ So, distance from Plzeň = **

codeWrite a Python function `parse_iso8601(s: str)` that parses an ISO 8601 timestamp such as `2026-10-12T14:03:07.250+02:00` into a tuple (year, month, day, hour, minute, second, microsecond, utc_offset_minutes) without using the datetime module. Validate the input and raise ValueError on malformed strings. Include a few pytest test cases.

reference: A100, E1 greedy, r0 · 1024 tokens · no run identical
```python import re from typing import Tuple, ValueError def parse_iso8601(s: str) -> Tuple[int, int, int, int, int, int, int, int]: """ Parse an ISO 8601 timestamp string into a tuple (year, month, day, hour, minute, second, microsecond, utc_offset_minutes). Args: s: ISO 8601 formatted string (e.g., "2026-10-12T14:03:07.250+02:00") Returns: Tuple of (year, month, day, hour, minute, second, microsecond, utc_offset_minutes) Raises: ValueError: If the input string is malformed or does not conform to ISO 8601 format """ # Validate input if not isinstance(s, str): raise ValueError("Input must be a string") if not s or s.isspace(): raise ValueError("Input string cannot be empty or contain only whitespace") # Define the expected pattern # Format: YYYY-MM-DDTHH:MM:SS.sss[+-]HH:MM pattern = r'^(\d{4})-(\d{2})-(\d{2})T(\d{2}):(\d{2}):(\d{2})\.(\d{3})([+-])(\d{2}):(\d{2})$' match = re.match(pattern, s) if not match: # Try without microseconds (e.g., "2026-10-12T14:03:07+02:00") pattern_no_micro = r'^(\d{4})-(\d{2})-(\d{2})T(\d{2}):(\d{2}):(\d{2})([+-])(\d{2}):(\d{2})$' match_no_micro = re.match(pattern_no_micro, s) if not match_no_micro: raise ValueError(f"Invalid ISO 8601 format: {s}") # Extract values from the no-microsecond version year, month, day, hour, minute, second, utc_sign, utc_hour, utc_minute = match_no_micro.groups() # Microsecond is 0 microsecond = 0 # UTC offset in minutes offset_minutes = int(utc_hour) * 60 + int(utc_minute) if utc_sign == '+' else -(int(utc_hour) * 60 + int(utc_minute)) return ( int(year), int(month), int(day), int(hour), int(minute), int(second), microsecond, offset_minutes ) # Extract values from the full pattern year, month, day, hour, minute, second, microsecond_str, utc_sign, utc_hour, utc_minute = match.groups() # Convert to integers year, month, day, hour, minute, second = int(year), int(month), int(day), int(hour), int(minute), int(second) microsecond = int(microsecond_str) # UTC offset in minutes offset_minutes = int(utc_hour) * 60 + int(utc_minute) if utc_sign == '+' else -(int(utc_hour) * 60 + int(utc_minute)) # Validate date components if not (1 <= month <= 12): raise ValueError(f"Invalid month: {month}") if not (1 <= day <= 31): raise ValueError(f"Invalid day: {day}") # Validate time components if not (0 <= hour <= 23): raise ValueError(f"Invalid hour: {hour}") if not (0 <= minute <= 59): raise ValueError(f"Invalid minute: {minute}") if not (0 <= second <= 59): raise ValueError(f"Invalid second: {second}") if not (0 <= microsecond <= 999999): raise ValueError(f"Invalid microsecond: {microsecond}") # Validate UTC offset if not (-1440 <= offset_minutes <= 1440): raise ValueError(f"Invalid UTC offset: {offset_minutes} minutes") # Validate day of month based on month (basic check) # This is a simplified check - we don't validate leap years or month-specific days # in this function for simplicity if month in [4, 6, 9, 11] and day > 30: raise ValueError(f"Invalid day for month {month}: {day}
r0–9 · differs from token 185 · 1024 tokens
…, second, microsecond, utc_offset_minutes) Raises: ValueError: If the input string is malformed or does not conform to ISO 8601 format """ # Validate input if not isinstance(s, str): raise ValueError("Input must be a string") if not s or s.isspace(): raise ValueError("Input string cannot be empty or contain only whitespace") # Define the expected pattern # Format: YYYY-MM-DDTHH:MM:SS.sss[+-]HH:MM or YYYY-MM-DDTHH:MM:SS.sss[+-]HH # We need to match the full structure with optional fractional seconds and timezone # Pattern breakdown: # YYYY-MM-DDT HH:MM:SS.sss[+-]HH:MM or YYYY-MM-DDT HH:MM:SS.sss[+-]HH pattern = ( r'^(\d{4})-(\d{2})-(\d{2})T' r'(\d{2}):(\d{2}):(\d{2})' r'(\.\d{1,3})?' r'([+-])?(\d{2}):(\d{2})?$' ) match = re.match(pattern, s) if not match: raise ValueError("Invalid ISO 8601 format") # Extract groups year, month, day, hour, minute, second, frac_part, tz_sign, tz_hour, tz_minute = match.groups() # Handle fractional seconds microsecond = 0 if frac_part: frac_val = frac_part.strip('.') # Ensure we have at least 3 digits (if less, pad with zeros) frac_val = frac_val.lstrip('0') if len(frac_val) < 3: frac_val = frac_val.ljust(3, '0') # Convert to microseconds (multiply by 1000) microsecond = int(frac_val) * 1000 # Handle timezone offset utc_offset_minutes = 0 if tz_sign: tz_hour = int(tz_hour) if tz_hour else 0 tz_minute = int(tz_minute) if tz_minute else 0 utc_offset_minutes = (tz_hour * 60) + (tz_minute if tz_sign == '+' else -tz_minute) else: # If no timezone sign, it's invalid (should be either + or -) raise ValueError("Timezone must have a sign (+ or -)") # Validate date components try: year = int(year) month = int(month) day = int(day) hour = int(hour) minute = int(minute) second = int(second) except ValueError as e: raise ValueError(f"Invalid numeric value in timestamp: {e}") # Validate ranges if not (1 <= month <= 12): raise ValueError("Month must be between 1 and 12") if not (1 <= day <= 31): raise ValueError("Day must be between 1 and 31") if not (0 <= hour <= 23): raise ValueError("Hour must be between 0 and 23") if not (0 <= minute <= 59): raise ValueError("Minute must be between 0 and 59") if not (0 <= second <= 59): raise ValueError("Second must be between 0 and 59") # Validate microsecond (should be 0-999999) if microsecond < 0 or microsecond > 999999: raise ValueError("Microsecond must be between 0 and 999999") # Validate timezone offset (should be in range -1440 to +1440 minutes) if utc_offset_minutes < -1440 or utc_offset_minutes > 1440: raise ValueError("UTC offset must